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Mean lake-wide pelagic fish density was 1532 fish/ha and mean pelagic fish biomass was 4151 g/ha in 2018, which represents 128% and 108% of the long-term mean, respectively. Mean lake-wide biomass was 24% lower in 2018 and mean lake-wide fish density was 3.3% lower in 2018 as compared to 2017. Lake-wide density and biomass of small alewife (< 100 mm) increased significantly in 2018 and was due primarily to increased abundance in the western main basin. Lake-wide density of small rainbow smelt (< 90 mm) increased in 2018 and was a result of increased abundance in the eastern main basin, Georgian Bay, and the North Channel. Biomass of large rainbow smelt (> 90 mm) increased in 2018 and was a result of increased biomass in the main basin and Georgian Bay. Density of small bloater (< 120 mm) declined in the western main basin but increased in other regions of Lake Huron. Biomass of large bloater (> 120 mm) remained at levels similar to 2017 in most regions of Lake Huron. Emerald shiner density and biomass increased in 2018 due to increased abundance in the main basin south and main basin west regions. Density and biomass of large cisco (> 200 mm) declined marginally between 2017 and 2018, but cisco biomass and density has shown an increasing trend in the North Channel and Georgian Bay since 2011.","conferenceTitle":"Lake Huron Committee Meeting","conferenceDate":"Mar 26, 2019","conferenceLocation":"Ypsilanti, MI","language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"O’Brien, T.P., Farha, S., Warner, D., Esselman, P., Phillips, K., Lenart, S., and Olds, C., 2019, Status and trends of pelagic prey fish in Lake Huron, 2018, Lake Huron Committee Meeting, Ypsilanti, MI, Mar 26, 2019, 14 p.","productDescription":"14 p.","ipdsId":"IP-106810","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":389651,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":389650,"rank":1,"type":{"id":15,"text":"Index 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,{"id":70218674,"text":"70218674 - 2019 - The US Geological Survey’s Earth Mapping Resources Initiative (Earth MRI)—Providing framework geologic, geophysical, and elevation data to the nation’s critical mineral-bearing regions","interactions":[],"lastModifiedDate":"2021-09-22T16:36:39.76293","indexId":"70218674","displayToPublicDate":"2019-12-31T11:27:11","publicationYear":"2019","noYear":false,"publicationType":{"id":25,"text":"Newsletter"},"publicationSubtype":{"id":30,"text":"Newsletter"},"seriesTitle":{"id":9355,"text":"Fast Times","active":true,"publicationSubtype":{"id":30}},"title":"The US Geological Survey’s Earth Mapping Resources Initiative (Earth MRI)—Providing framework geologic, geophysical, and elevation data to the nation’s critical mineral-bearing regions","docAbstract":"<p><span>New detailed mapping of the geologic resources of the Nation </span><span>has the potential to significantly close the gap in the essential </span><span>data needed to fuel a modern era of economic development and </span><span>technological innovation, while at the same time dramatically </span><span>enhancing our understanding of the fundamental way geology </span><span>impacts everyday life, from the domestic critical mineral resources </span><span>that are necessary for modern technology and the economy, </span><span>to domestic energy and water resources, geologic hazards, </span><span>agriculture, and other pressing needs. The U.S. Geological Survey </span><span>established the Earth Resources Mapping Initiative (Earth MRI) to </span><span>address the shortfall in geologic, geophysical, and elevation data </span><span>with sufficient detail to support evaluation of regions in the United </span><span>States that have potential to host critical mineral resources. The </span><span>new effort is a collaboration with the Association of American </span><span>State Geologists, who are providing new detailed geologic maps </span><span>and making available online archived data and information related </span><span>to critical mineral resources. The geophysical and lidar surveys </span><span>are being contracted through industry specialists to assure that </span><span>high-quality data are available to the public. This article provides </span><span>an overview of the Earth MRI effort with discussions on the initial </span><span>geophysical surveys funded for areas that have known potential </span><span>for rare earth element resources. Subsequent projects are being </span><span>designed to address areas that may host other critical mineral </span><span>resources.</span></p>","language":"English","publisher":"Association of American State Geologists","usgsCitation":"Day, W.C., Drenth, B.J., McCafferty, A.E., Shah, A.K., Ponce, D.A., Jones, J.V., and Grauch, V.J., 2019, The US Geological Survey’s Earth Mapping Resources Initiative (Earth MRI)—Providing framework geologic, geophysical, and elevation data to the nation’s critical mineral-bearing regions: Fast Times, v. 24, no. 5, p. 55-62.","productDescription":"8 p.","startPage":"55","endPage":"62","ipdsId":"IP-113023","costCenters":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science 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,{"id":70202322,"text":"70202322 - 2019 - Off-channel waterbodies in the Middle Mississippi River: A pilot investigation","interactions":[],"lastModifiedDate":"2020-05-27T16:31:57.70458","indexId":"70202322","displayToPublicDate":"2019-12-31T11:25:41","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":5958,"text":"U.S Army Corps of Engineers Completion Report","active":true,"publicationSubtype":{"id":1}},"title":"Off-channel waterbodies in the Middle Mississippi River: A pilot investigation","docAbstract":"<p>Off-channel and floodplain water bodies are important components of large river ecosystems while rare within the Middle Mississippi River. The lack of these habitats likely influences water quality, nutrient processing, and communities of organisms. In early 2016 a major flood event breached two levees south of Cape Girardeau, MO resulting in the creation of two new backwaters—Len Small and Backwater MO 35.5. Water quality, metabolic rate, and fish community data were collected from the new backwaters as well as Horseshow Lake an isolated floodplain lake. Backwater conditions were often different from the main channel with backwaters being warmer and with greater water clarity throughout the study. Nutrient concentrations were often different from the main channel and exhibited similar patterns to those observed in the Upper Mississippi River. One backwater showed high rates of primary productivity (NEP) along with the floodplain lake. Differences between backwater metabolic rates may be due in part to differences in size and connectivity to the river. Fish communities were different between waterbodies with a number of lacustrine species observed in the floodplain lake. Habitat and feeding guilds were also different between waterbodies. Diversity was also not significantly different between waterbodies.</p><p>This study represents novel findings for off-channel habitats on the Middle Mississippi River and the opportunity to explore the establishment of new habitat types. Ultimately, we view MO 35.5, Len Small, and Horseshoe Lake as important habitats within the larger riverine ecosystem. There remains much to be learned if restoration activities based on backwater creation within the MMR are to be successful but these preliminary and early stage results indicate these areas are already providing important and variable environmental conditions to riverine organisms.</p>","language":"English","publisher":"U.S. Army Corps of Engineer's Upper Mississippi River Restoration Program","usgsCitation":"Sobotka, M., and West, J., 2019, Off-channel waterbodies in the Middle Mississippi River: A pilot investigation: U.S Army Corps of Engineers Completion Report, Report: 28 p.; Data Release.","productDescription":"Report: 28 p.; Data Release","ipdsId":"IP-098199","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":375090,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":375089,"rank":2,"type":{"id":30,"text":"Data Release"},"url":"https://www.sciencebase.gov/catalog/item/5bf42c29e4b045bfcae120d3"},{"id":375088,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.umesc.usgs.gov/documents/publications/2019/sobotka_a_2019.html"}],"country":"United States","state":"Illinois, Missouri","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.4894790649414,\n              37.06230052887983\n            ],\n            [\n              -89.27146911621092,\n              37.06230052887983\n            ],\n            [\n              -89.27146911621092,\n              37.16113737391723\n            ],\n            [\n              -89.4894790649414,\n              37.16113737391723\n            ],\n            [\n              -89.4894790649414,\n              37.06230052887983\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":15,"text":"Madison PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sobotka, Molly","contributorId":213496,"corporation":false,"usgs":false,"family":"Sobotka","given":"Molly","email":"","affiliations":[{"id":16971,"text":"Missouri Department of Conservation","active":true,"usgs":false}],"preferred":false,"id":757832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"West, John","contributorId":189976,"corporation":false,"usgs":false,"family":"West","given":"John","affiliations":[],"preferred":false,"id":757833,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70208129,"text":"70208129 - 2019 - Proposed multi-period response spectra and ground motion requirements of the 2020 Recommended Provisions and ASCE 7-22","interactions":[],"lastModifiedDate":"2020-06-08T16:19:22.272776","indexId":"70208129","displayToPublicDate":"2019-12-31T11:18:09","publicationYear":"2019","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Proposed multi-period response spectra and ground motion requirements of the 2020 Recommended Provisions and ASCE 7-22","docAbstract":"This paper summarizes a comprehensive set of proposals to the Provisions Update Committee of the Building Seismic Safety Council that would incorporate multi-period response spectra (MPRS) in the 2020 edition of the NEHRP Recommended Seismic Provisions for New Buildings and Other Structures (2020 NEHRP Provisions) and related proposals to the ASCE 7-22 Seismic Subcommittee of the American Society of Civil Engineers for incorporation of MPRS in the ASCE Standard, ASCE/SEI 7-22, Minimum Design Loads and Associated Criteria for Buildings and Other Structures (ASCE 7-22).  Ultimately, the intent is that the proposed MPRS and related design requirements of ASCE 7-22 would be adopted, by reference, as part of the 2024 International Building Code.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the Structural Engineers Association of California (SEAOC) 2019 Convention","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Structural Engineers Association of California (SEAOC) 2019 Convention","conferenceDate":"August 28-31, 2019","conferenceLocation":"Squaw Creek, CA","language":"English","usgsCitation":"Kircher, C.A., Rezaeian, S., and Luco, N., 2019, Proposed multi-period response spectra and ground motion requirements of the 2020 Recommended Provisions and ASCE 7-22, <i>in</i> Proceedings of the Structural Engineers Association of California (SEAOC) 2019 Convention, Squaw Creek, CA, August 28-31, 2019.","productDescription":"10 p.","startPage":"10","ipdsId":"IP-111271","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":375414,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kircher, Charles A","contributorId":221886,"corporation":false,"usgs":false,"family":"Kircher","given":"Charles","email":"","middleInitial":"A","affiliations":[{"id":40454,"text":"Kircher & Associates, Consulting Engineers","active":true,"usgs":false}],"preferred":false,"id":780636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rezaeian, Sanaz 0000-0001-7589-7893 srezaeian@usgs.gov","orcid":"https://orcid.org/0000-0001-7589-7893","contributorId":4395,"corporation":false,"usgs":true,"family":"Rezaeian","given":"Sanaz","email":"srezaeian@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":780635,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Luco, Nico 0000-0002-5763-9847 nluco@usgs.gov","orcid":"https://orcid.org/0000-0002-5763-9847","contributorId":145730,"corporation":false,"usgs":true,"family":"Luco","given":"Nico","email":"nluco@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":780637,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70205945,"text":"70205945 - 2019 - Scientific Framework for resilience research on the Upper Mississippi River System","interactions":[],"lastModifiedDate":"2020-06-01T16:14:18.282784","indexId":"70205945","displayToPublicDate":"2019-12-31T11:14:06","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":5000,"text":"Long Term Resource Monitoring Technical Report","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"LTRM-2019R2","title":"Scientific Framework for resilience research on the Upper Mississippi River System","docAbstract":"<p>The goal of this research framework is to outline research that would continue to improve our understanding of ecological resilience of the Upper Mississippi River System (UMRS) and inform management of the system for health and resilience. 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,{"id":70204640,"text":"70204640 - 2019 - Identifying characteristics of actionable science for drought planning and adaptation: Final report to the North Central Climate Adaptation Science Center","interactions":[],"lastModifiedDate":"2020-06-08T16:09:16.903228","indexId":"70204640","displayToPublicDate":"2019-12-31T11:02:49","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":5883,"text":"Cooperator Report","active":true,"publicationSubtype":{"id":1}},"title":"Identifying characteristics of actionable science for drought planning and adaptation: Final report to the North Central Climate Adaptation Science Center","docAbstract":"<p><span>Changing climate conditions can make water management planning and drought preparedness decisions more complicated than ever before. Resource managers can no longer rely solely on historical data and trends to base their actions, and are in need of science that is relevant to their specific needs and can directly inform important planning decisions. Questions remain, however, regarding the most effective and efficient methods for extending scientific knowledge and products into management and decision-making.</span><br><br><span>This study analyzed two unique cases of water management to better understand how science can be translated into resource management actions and decision-making. &nbsp;In particular, this project sought to understand 1) the characteristics that make science actionable and useful for water resource management and drought preparedness, and 2) the ideal types of scientific knowledge or science products that facilitate the use of science in management and decision-making.</span><br><br><span>The first case study focused on beaver mimicry, an emerging nature-based solution that increases the presence of wood and woody debris in rivers and streams to mimic the actions of beavers. This technique has been rapidly adopted by natural resource managers as a way to restore riparian areas, increase groundwater infiltration, and slow surface water flow so that more water is available later in the year during hotter and dryer months. The second case study focused on an established research program, Colorado Dust on Snow, that provides water managers with scientific information explaining how the movement of dust particles from the Colorado Plateau influences hydrology and the timing and intensity of snow melt and water runoff into critical water sources. This program has support from and is being used by several water conservation districts in the state.</span><br><br><span>Understanding how scientific knowledge translates into action and decision-making in these cases is expected to strengthen our knowledge of actionable science in the context of drought and its impacts on ecosystems. The project team gathered qualitative data through stakeholder interviews and will conduct an extensive literature review. 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,{"id":70222188,"text":"70222188 - 2019 - An overview of the world’s plovers","interactions":[],"lastModifiedDate":"2021-07-22T16:00:13.753046","indexId":"70222188","displayToPublicDate":"2019-12-31T10:59:45","publicationYear":"2019","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"1","title":"An overview of the world’s plovers","docAbstract":"<p><span>Plovers of the genus Charadrius and their close allies are a diverse group, numbering 40 species, many with subspecies. They breed on all continents except Antarctica, in open, sparsely vegetated habitats of tundra and grasslands, and along shores of oceans, rivers, and inland lakes. Most are migratory, especially those breeding in arctic and temperate regions; others are partial migrants or sedentary. On migration, they are poorly studied and do not always correspond to the typical shorebird (i.e., sandpiper) pattern characterized by dense flocks concentrating at a few staging areas. Their foraging ecologies are rather uniform in that all species search visually for prey using a “run-stop-peck” maneuver. Breeding birds defend nesting and foraging territories while nonbreeding birds forage in loose flocks, which may stem from individuals minimizing interference with conspecifics while enhancing benefits of shared vigilance for predators. In breeding, they are conservative, laying two to four eggs at daily or longer intervals; replacement clutches are common, especially in species with prolonged breeding seasons. Precocial young hatch after comparatively long incubation that is correlated with development of neural centers associated with vision. Their mating systems are a mix of social monogamy and biparental care, with frequent sequential polygamy, especially in temperate and tropical taxa that breed for extended periods. Population sizes vary over several orders of magnitude; several species are highly endangered. Other species are abundant and widely distributed, although their populations may also be in decline. Regardless of their status, most plovers occupy habitats throughout the year that put them at conservation risk owing to anthropogenic factors including climate change, human disturbance, habitat loss, and predation. In this book, we draw from the expertise of an international group of researchers to outline the ecologies, behaviors, and challenges of plovers throughout the annual cycle so that decision makers can be most successful in their endeavors to conserve and manage populations.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The population ecology and conservation of Charadrius plovers","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Routledge","usgsCitation":"Colwell, M., and Haig, S.M., 2019, An overview of the world’s plovers, chap. 1 <i>of</i> The population ecology and conservation of Charadrius plovers, p. 2-15.","productDescription":"14 p.","startPage":"2","endPage":"15","ipdsId":"IP-088578","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":387390,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Colwell, Mark A","contributorId":217912,"corporation":false,"usgs":false,"family":"Colwell","given":"Mark A","affiliations":[{"id":7067,"text":"Humboldt State University","active":true,"usgs":false}],"preferred":false,"id":819750,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haig, Susan M. 0000-0002-6616-7589 susan_haig@usgs.gov","orcid":"https://orcid.org/0000-0002-6616-7589","contributorId":719,"corporation":false,"usgs":true,"family":"Haig","given":"Susan","email":"susan_haig@usgs.gov","middleInitial":"M.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":819632,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70206595,"text":"ofr20191124 - 2019 - Quantifying erosion rates by using terrestrial laser scanning at Malakoff Diggins State Historic Park, Nevada County, California, 2014–17","interactions":[],"lastModifiedDate":"2022-04-21T19:11:49.488677","indexId":"ofr20191124","displayToPublicDate":"2019-12-31T10:57:18","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-1124","displayTitle":"Quantifying Erosion Rates by Using Terrestrial Laser Scanning at Malakoff Diggins State Historic Park, Nevada County, California, 2014–17","title":"Quantifying erosion rates by using terrestrial laser scanning at Malakoff Diggins State Historic Park, Nevada County, California, 2014–17","docAbstract":"<p>The abandoned hydraulic mine pit at Malakoff Diggins near Grass Valley, California, can produce large volumes of eroded sediment transportable by storm runoff. Sediment-laden water discharged from the pit is a major source of heavy metals to Humbug Creek and the South Yuba River. To develop a comprehensive sediment budget for the Malakoff Diggins mine pit and identify sources of sediment and metals within the pit that can become entrained as suspended sediment in runoff discharged from the pit, the U.S. Geological Survey, working in cooperation with the California Department of Water Resources, the California Department of Parks and Recreation, and the Nevada Irrigation District, used terrestrial laser scanning technology to quantify eroded volumes and erosion rates of sedimentary units exposed in the pit walls. The results for eroded volumes and rates reported here are part one of a three-part study.</p><p>High-resolution terrestrial laser scanning surveys were repeated annually from 2014 through 2017, including before and after dry and wet winters, measuring centimeter-scale topographic changes to quantify the volume of sediment eroded from outcrops at Malakoff Diggins State Historic Park, located on the western slope of the northern Sierra Nevada about 17 kilometers northeast of Grass Valley, California. Terrestrial laser scanning enabled construction of three-dimensional maps of the complex outcrop surfaces, which could not be mapped non-destructively or in sufficient detail with traditional surveying techniques. Eroded volumes from discrete sedimentary units were calculated at four study sites (numbered 1, 2, 4, and 5) throughout the mine pit for the December 2014 to August 2017 period.</p><p>Eroded volumes at the four study sites during the 32-month study ranged from 288 plus or minus (±) 13 cubic meters (m<sup>3</sup>) of sediment at site 1 to 8,517±145 m<sup>3</sup> at site 4. Annual erosion rates at the four study sites ranged from 0.06±0.01 cubic meters per square meter per year (m<sup>3</sup>/m<sup>2</sup>/yr) at site 4 to 0.14±0.01 m<sup>3</sup>/m<sup>2</sup>/yr at site 2. The total eroded volume documented with terrestrial laser scanning at all four study sites from December 2014 to August 2017 was 12,934±334 m<sup>3</sup> of sediment, and the average annual erosion rate for the four study sites was 0.10±0.04 m<sup>3</sup>/m<sup>2</sup>/yr.</p><p>Horizontal erosional-change maps indicate that a variety of erosional processes were responsible for the eroded sediment volume. These included areally broad and smaller-scale processes such as persistent dry ravel, periodic sheet wash, and frost heave and more localized and larger-scale processes such as coalescing fluvial incision, rotational landslides, and translational block-fall failures.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20191124","collaboration":"In cooperation with the California Department of Water Resources, the California Department of Parks and Recreation, and the Nevada Irrigation District","usgsCitation":"Howle, J.F., Alpers, C.N., Ward, A.J., Bond, S., and Curtis, J.A., 2019, Quantifying erosion rates by using terrestrial laser scanning at Malakoff Diggins State Historic Park, Nevada County, California, 2014–17: U.S. Geological Survey Open-File Report 2019–1124, 39 p., https://doi.org/10.3133/ofr20191124.","productDescription":"Report: viii, 39 p.; 2 Data Releases","onlineOnly":"Y","ipdsId":"IP-087722","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":399420,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_109574.htm"},{"id":370127,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2019/1124/coverthb.jpg"},{"id":370129,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9H3VNSN","linkHelpText":"Terrestrial Laser Scanning Data from Malakoff Diggins State Historic Park, Nevada County, California, 2014–17"},{"id":370128,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2019/1124/ofr20191124.pdf","text":"Report","size":"12.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2019-1124"},{"id":370856,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P95RLMEI","linkHelpText":"Geochemical, Mineralogical, and Grain-Size Data for In Situ Solid Materials and Suspended Sediment at Malakoff Diggins State Historic Park, Nevada County, California"}],"country":"United States","state":"California","county":"Nevada County","otherGeospatial":"Malakoff Diggins State Historic Park","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-120.0032,39.448],[-120.0034,39.4331],[-120.0036,39.4181],[-120.0037,39.4049],[-120.0039,39.3909],[-120.0042,39.3741],[-120.0047,39.3451],[-120.005,39.3297],[-120.0047,39.3161],[-120.0124,39.3161],[-120.1867,39.3166],[-120.346,39.3165],[-120.3978,39.3166],[-120.5423,39.3155],[-120.6362,39.3151],[-120.6457,39.315],[-120.654,39.3104],[-120.6623,39.3103],[-120.6724,39.3098],[-120.6819,39.3065],[-120.6937,39.3023],[-120.7049,39.2977],[-120.709,39.2945],[-120.7161,39.2913],[-120.7262,39.2884],[-120.7309,39.2866],[-120.7356,39.2829],[-120.7456,39.2765],[-120.7526,39.2696],[-120.7572,39.265],[-120.7626,39.2636],[-120.7655,39.2599],[-120.7713,39.2558],[-120.7784,39.2539],[-120.7843,39.2484],[-120.7907,39.2429],[-120.796,39.2397],[-120.8019,39.2351],[-120.8095,39.2323],[-120.8202,39.2281],[-120.8249,39.2258],[-120.8278,39.2235],[-120.8401,39.2152],[-120.8531,39.2105],[-120.8582,39.195],[-120.8622,39.1905],[-120.8668,39.1832],[-120.884,39.1784],[-120.8875,39.177],[-120.8958,39.1756],[-120.9041,39.1759],[-120.9081,39.17],[-120.9075,39.1659],[-120.9134,39.165],[-120.9169,39.164],[-120.9234,39.1626],[-120.9263,39.1562],[-120.9286,39.1562],[-120.9363,39.1556],[-120.9368,39.1493],[-120.9479,39.1423],[-120.9508,39.1373],[-120.9672,39.1272],[-120.9747,39.1171],[-120.9829,39.1093],[-120.9882,39.111],[-120.9879,39.0947],[-120.9935,39.0788],[-120.9975,39.0724],[-120.9974,39.0674],[-120.9992,39.0656],[-121.0044,39.0614],[-121.0073,39.0569],[-121.0089,39.0519],[-121.0142,39.0468],[-121.0195,39.0449],[-121.0212,39.0404],[-121.0282,39.0376],[-121.0298,39.0312],[-121.0309,39.0249],[-121.0367,39.0193],[-121.0402,39.0148],[-121.0537,39.011],[-121.0578,39.0096],[-121.0649,39.0063],[-121.0696,39.0053],[-121.0755,39.0062],[-121.0803,39.0093],[-121.0899,39.0137],[-121.0987,39.0109],[-121.1054,39.0171],[-121.1101,39.0184],[-121.1184,39.0192],[-121.1204,39.0264],[-121.1252,39.0314],[-121.133,39.0353],[-121.1395,39.0353],[-121.1442,39.0311],[-121.1472,39.0324],[-121.1541,39.0255],[-121.1612,39.0245],[-121.1682,39.0195],[-121.1717,39.0185],[-121.1771,39.0189],[-121.1876,39.0124],[-121.1942,39.0155],[-121.2031,39.0158],[-121.2095,39.0117],[-121.2213,39.0124],[-121.2262,39.0191],[-121.2323,39.0236],[-121.2441,39.022],[-121.2513,39.0247],[-121.2644,39.0295],[-121.268,39.0308],[-121.2788,39.0365],[-121.2791,39.1938],[-121.2794,39.2287],[-121.2735,39.2324],[-121.2706,39.2356],[-121.2696,39.2416],[-121.2673,39.2439],[-121.2663,39.2534],[-121.2592,39.2548],[-121.2575,39.2589],[-121.2582,39.263],[-121.2655,39.2706],[-121.2561,39.2762],[-121.2473,39.2795],[-121.2409,39.2846],[-121.226,39.2816],[-121.2183,39.2831],[-121.2155,39.2917],[-121.2079,39.2964],[-121.2015,39.3019],[-121.1991,39.3024],[-121.2047,39.3118],[-121.203,39.3182],[-121.1978,39.3214],[-121.1979,39.3291],[-121.1902,39.3297],[-121.1849,39.3307],[-121.1821,39.338],[-121.1785,39.3389],[-121.175,39.339],[-121.1714,39.339],[-121.1678,39.3386],[-121.1654,39.3368],[-121.1636,39.3337],[-121.16,39.3328],[-121.1576,39.3347],[-121.1571,39.3378],[-121.1566,39.3428],[-121.1555,39.3478],[-121.1532,39.3497],[-121.1473,39.3498],[-121.1449,39.3493],[-121.1437,39.3507],[-121.145,39.3534],[-121.1445,39.3575],[-121.138,39.3617],[-121.1363,39.3667],[-121.1334,39.3699],[-121.127,39.375],[-121.1271,39.379],[-121.1057,39.3798],[-121.1027,39.3816],[-121.0986,39.3835],[-121.0945,39.3876],[-121.0892,39.3881],[-121.0862,39.3891],[-121.0845,39.3927],[-121.081,39.3946],[-121.0709,39.3938],[-121.0631,39.3921],[-121.0584,39.3949],[-121.053,39.3959],[-121.0483,39.3955],[-121.0465,39.3941],[-121.0458,39.3919],[-121.044,39.3901],[-121.0404,39.3897],[-121.0375,39.3906],[-121.034,39.3956],[-121.031,39.3961],[-121.0286,39.3953],[-121.0256,39.3917],[-121.0226,39.3908],[-121.0197,39.3949],[-121.0132,39.3977],[-121.0079,39.4005],[-121.0151,39.4054],[-121.0056,39.4064],[-120.9962,39.4124],[-120.9897,39.4116],[-120.9849,39.4112],[-120.9784,39.4163],[-120.9737,39.419],[-120.9588,39.4156],[-120.9517,39.4166],[-120.9464,39.4207],[-120.9415,39.4167],[-120.9297,39.4186],[-120.9255,39.421],[-120.9148,39.4215],[-120.9095,39.4261],[-120.9018,39.4235],[-120.8828,39.4291],[-120.8733,39.4288],[-120.8644,39.4321],[-120.8543,39.4349],[-120.843,39.4359],[-120.8383,39.4391],[-120.8335,39.4347],[-120.8263,39.4352],[-120.8174,39.438],[-120.8121,39.4372],[-120.8032,39.4391],[-120.7925,39.4419],[-120.7837,39.4479],[-120.7706,39.4507],[-120.7594,39.4549],[-120.7523,39.4573],[-120.7458,39.46],[-120.7428,39.4619],[-120.7411,39.4683],[-120.728,39.4697],[-120.7227,39.4743],[-120.721,39.4762],[-120.7157,39.4798],[-120.7134,39.483],[-120.714,39.488],[-120.7052,39.4967],[-120.7005,39.5008],[-120.6881,39.5087],[-120.6793,39.5142],[-120.6722,39.5179],[-120.6645,39.5216],[-120.6585,39.5221],[-120.6526,39.5231],[-120.6472,39.5227],[-120.6389,39.5227],[-120.6341,39.5232],[-120.6305,39.5196],[-120.6251,39.5192],[-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data-mce-href=\"https://www.usgs.gov/centers/ca-water/connect\" href=\"https://www.usgs.gov/centers/ca-water/connect\" target=\"_blank\" rel=\"noopener\">Director</a>, <br><a data-mce-href=\"https://ca.water.usgs.gov\" href=\"https://ca.water.usgs.gov\" target=\"_blank\" rel=\"noopener\">California Water Science Center</a><br><a data-mce-href=\"https://usgs.gov\" href=\"https://usgs.gov\" target=\"_blank\" rel=\"noopener\">U.S. Geological Survey</a><br>6000 J Street, Placer Hall<br>Sacramento, California 95819<br></p>","tableOfContents":"<p></p><ul><li>Abstract</li><li>Introduction</li><li>Methods</li><li>Total Eroded Volumes</li><li>Summary</li><li>References Cited</li><li>Glossary</li><li>Appendix Tables</li></ul><p></p>","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"publishedDate":"2019-12-31","noUsgsAuthors":false,"publicationDate":"2019-12-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Howle, James F. 0000-0003-0491-6203","orcid":"https://orcid.org/0000-0003-0491-6203","contributorId":202665,"corporation":false,"usgs":true,"family":"Howle","given":"James","email":"","middleInitial":"F.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":775087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":775088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ward, Alfred J. 0000-0002-4269-3162","orcid":"https://orcid.org/0000-0002-4269-3162","contributorId":208507,"corporation":false,"usgs":true,"family":"Ward","given":"Alfred","email":"","middleInitial":"J.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":775091,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bond, Sandra 0000-0003-0522-5287 sbond@usgs.gov","orcid":"https://orcid.org/0000-0003-0522-5287","contributorId":219172,"corporation":false,"usgs":true,"family":"Bond","given":"Sandra","email":"sbond@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":775090,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Curtis, Jennifer A. 0000-0001-7766-994X jacurtis@usgs.gov","orcid":"https://orcid.org/0000-0001-7766-994X","contributorId":927,"corporation":false,"usgs":true,"family":"Curtis","given":"Jennifer","email":"jacurtis@usgs.gov","middleInitial":"A.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":775089,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70217780,"text":"70217780 - 2019 - Status and trends in the Lake Superior fish community, 2019","interactions":[],"lastModifiedDate":"2023-03-30T16:35:37.704717","indexId":"70217780","displayToPublicDate":"2019-12-31T10:47:25","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"title":"Status and trends in the Lake Superior fish community, 2019","docAbstract":"The Lake Superior fish community was sampled in 2019 with daytime bottom trawls at 76 nearshore and 35 offshore stations distributed throughout the lake. In the nearshore zone, 25,131 fish from 24 species or morphotypes were collected. The number of species collected at nearshore stations ranged from 0 to 15, with a mean of 5.6 and median of five. Nearshore mean biomass was 5.7 kg/ha which was similar to the past twenty-year average of 5.2 kg/ha and less than the 42-year period-of-record mean of 8.5 kg/ha. Lake Whitefish, Rainbow Smelt, Longnose Sucker, Bloater, lean Lake Trout, Cisco, Burbot, and siscowet Lake Trout had the highest total collected biomass. In the offshore zone, 13,145 fish from 11 species or morphotypes were collected. The number of species collected at offshore stations ranged from two to six, with a mean 3.6 and median of four. Deepwater Sculpin, Kiyi, and siscowet Lake Trout made up 99% of the total number of individuals and biomass collected in offshore waters. Mean and median offshore biomass for all species in 2019 was 7.0 kg/ha which was greater than the past eight-year average of 6.6 kg/ha. Recruitment, as measured by age-1 densities, was near the period-of-record lakewide average for Lake Whitefish (7 fish/ha) and Rainbow Smelt (137 fish/ha) and was lower than the period-of-record lakewide average for Bloater (4 fish/ha), Kiyi (1 fish/ha), and Cisco (<1 fish/ha). Lakewide average age-1 Cisco densities have been estimated at <1 fish/ha in twelve of the last twenty years. 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,{"id":70207593,"text":"fs20193071 - 2019 - Assessment of continuous oil and gas resources in Jurassic Shales of the eastern Arabian Peninsula, 2019","interactions":[],"lastModifiedDate":"2021-04-08T21:42:16.335268","indexId":"fs20193071","displayToPublicDate":"2019-12-31T10:45:00","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-3071","displayTitle":"Assessment of Continuous Oil and Gas Resources in Jurassic Shales of the Eastern Arabian Peninsula, 2019","title":"Assessment of continuous oil and gas resources in Jurassic Shales of the eastern Arabian Peninsula, 2019","docAbstract":"<p>Using a geology-based assessment methodology, the U.S. Geological Survey estimated undiscovered, technically recoverable mean resources of&nbsp;5.6 billion barrels of oil and 109.1 trillion cubic feet of gas in the Jurassic Hanifa-Tuwaiq Total Petroleum System of the Arabian Peninsula.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20193071","usgsCitation":"Schenk, C.J., Mercier, T.J., Woodall, C.A., Tennyson, M.E., Finn, T.M., Brownfield, M.E., Marra, K.R., Le, P.A., Drake, R.M., II, and Kinney, S.A., 2019, Assessment of continuous oil and gas resources in Jurassic shales of the eastern Arabian Peninsula, 2019: U.S. Geological Survey Fact Sheet 2019–3071, 2 p., https://doi.org/10.3133/fs20193071.","productDescription":"2 p.","onlineOnly":"N","ipdsId":"IP-109358","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":380622,"rank":4,"type":{"id":34,"text":"Image Folder"},"url":"https://pubs.usgs.gov/fs/2019/3071/images/"},{"id":374940,"rank":3,"type":{"id":31,"text":"Publication 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,{"id":70207359,"text":"fs20193075 - 2019 - Assessment of continuous oil and gas resources in Jurassic Posidonia Shales of Greece and Albania, 2019","interactions":[],"lastModifiedDate":"2021-04-08T21:41:48.142852","indexId":"fs20193075","displayToPublicDate":"2019-12-31T10:45:00","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-3075","title":"Assessment of continuous oil and gas resources in Jurassic Posidonia Shales of Greece and Albania, 2019","docAbstract":"<p>Using a geology-based assessment methodology, the U.S. Geological Survey estimated undiscovered, technically recoverable mean resources of 118 million barrels&nbsp;of continuous oil and 170 billion cubic feet of continuous gas in the Jurassic Posidonia Shale Total Petroleum System of western Greece and southern Albania.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20193075","usgsCitation":"Schenk, C.J., Mercier, T.J., Tennyson, M.E., Finn, T.M., Woodall, C.A., Brownfield, M.E., Marra, K.R., Leathers-Miller, H.M., Le, P.A., and Drake, R.M., II, 2019, Assessment of continuous oil and gas resources in Jurassic Posidonia Shales of Greece and Albania, 2019: U.S. Geological Survey Fact Sheet 2019–3075, 2 p., https://doi.org/10.3133/fs20193075.","productDescription":"2 p.","onlineOnly":"N","ipdsId":"IP-111051","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":380623,"rank":4,"type":{"id":34,"text":"Image Folder"},"url":"https://pubs.usgs.gov/fs/2019/3075/images/"},{"id":374935,"rank":3,"type":{"id":31,"text":"Publication 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,{"id":70216826,"text":"70216826 - 2019 - Atlantic Salmon (Salmo salar) climate scenario planning pilot report","interactions":[],"lastModifiedDate":"2020-12-09T17:20:00.12116","indexId":"70216826","displayToPublicDate":"2019-12-31T10:42:02","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":7459,"text":"Greater Atlantic Region Pollicy Series","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"19-05","displayTitle":"Atlantic Salmon (<i>Salmo salar</i>) climate scenario planning pilot report","title":"Atlantic Salmon (Salmo salar) climate scenario planning pilot report","docAbstract":"<div class=\"page\" data-page-number=\"4\" data-loaded=\"true\"><div class=\"textLayer\">Scenario planning is a structured process that embraces uncertainty and explores plausible alternative future conditions under different assumptions to help manage risk and prioritize actions ( Schwartz 1996, Peterson <i>et al</i>. 2003). It has been used by a variety of organizations to explore and help prepare for the future, lends itself well to exploring the uncertainty surrounding changing environmental conditions, and is widely applicable to natural resource management issues. The conservation and management of protected resources for example, can be particularly challenging when the rate and magnitude of climate-related changes, and the response of species to those changes, are uncertain (NMFS 2016). The structured process of scenario planning can help resource managers navigate through potentially paralyzing uncertainties, manage risk, and evaluate/prioritize management actions associated with adapting to, and managing for, climate change (Moore <i>et al</i>. 2013).</div><div class=\"textLayer\"><br data-mce-bogus=\"1\"></div><div class=\"textLayer\">Atlantic salmon (<i>Salmo salar</i>) is a species highly vulnerable to climate change in the Northeast Atlantic (Hare <i>et al</i>. 2016a). Based on this and the above reasons, a scenario planning initiative was piloted by NOAA Fisheries to explore what the agency can do to improve U.S.Atlantic salmon population resilience to changing climate conditions in riverine, estuarine(transition), and marine environments across its current range (U.S. headwaters to Greenland). Project objectives were: 1) to better understand the challenges of managing Atlantic salmon in a changing climate; 2) to identify and discuss potential management actions and research activities that can be undertaken to increase our understanding of the drivers of Atlantic salmon productivity and resilience; 3) to increase collaborations and coordination related to the speciesrecovery; and 4) to explore how scenario planning can be used to support decisions. </div><div class=\"textLayer\"><br data-mce-bogus=\"1\"></div><div class=\"textLayer\">Outcomes from this initiative included, but were not limited to, the identification of high priority research and management actions to further collaborations and efforts to recover this species. The identified high priority actions were those that could be undertaken in the near-term(1-5 years) using current resources and in consideration of potential future conditions. Examples of identified actions by habitat (not in order of priority) included: 1) synthesize and refine range-wide life stage specific quantitative environmental thresholds for temperature, flow, etc.; 2) assess watershed habitat productivity; 3) assess forage fish and survival connection and options for marine migration monitoring; and 4) reduce dam-associated indirect estuarine mortality rate. In addition, a number of high priority climate-related actions were included in the revised Atlantic Salmon Recovery Plan (USFWS and NMFS 2019, Appendix 16) and at least two newly NOAA Fisheries funded projects are now underway (1. conduct range-wide habitat analysis and synthesize life stage specific quantitative thresholds and 2. identify locations of cold water refugia under a changing climate).</div><div class=\"textLayer\"><br data-mce-bogus=\"1\"></div><div class=\"textLayer\">This is the first use of the scenario planning process (NPS 2013) by NOAA Fisheries. This report documents an important example of applying scenario planning to marine species/environments and may serve as a useful reference for other case studies. </div></div>","language":"English","publisher":"NOAA Fisheries","usgsCitation":"Borggaard, D., Dick, D., Star, J., Alexander, M., Bernier, M., Collins, M., Damon-Randall, K., Dudley, R., Roger Griffis, R., Hayes, S., Johnson, M., Kircheis, D., Kocik, J., Letcher, B., Mantua, N., Morrison, W., Nislow, K., Saba, V., Saunders, R., Sheehan, T., and Staudinger, M.D., 2019, Atlantic Salmon (Salmo salar) climate scenario planning pilot report: Greater Atlantic Region Pollicy Series 19-05, ii, 89 p.","productDescription":"ii, 89 p.","ipdsId":"IP-112540","costCenters":[{"id":5080,"text":"Northeast Climate Adaptation Science 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,{"id":70225630,"text":"70225630 - 2019 - USGS Illinois River catch database and visualization","interactions":[],"lastModifiedDate":"2022-04-18T15:37:51.293262","indexId":"70225630","displayToPublicDate":"2019-12-31T10:23:15","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":9543,"text":"Interim Summary Report","active":true,"publicationSubtype":{"id":3}},"title":"USGS Illinois River catch database and visualization","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"2019 Interim summary report: Asian carp monitoring and response plan","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"Asian Carp Regional Coordinating Committee","usgsCitation":"Hlavacek, E., Harrison, T.J., Knights, B.C., and Brey, M.K., 2019, USGS Illinois River catch database and visualization: Interim Summary Report, 4 p.","productDescription":"4 p.","startPage":"51","endPage":"54","ipdsId":"IP-122169","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":398924,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":391077,"type":{"id":15,"text":"Index Page"},"url":"https://invasivecarp.us/PlansReports.html"}],"country":"United States","state":"illinois","otherGeospatial":"Illinois River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.648193359375,\n              38.92522904714054\n            ],\n            [\n              -88.099365234375,\n              38.92522904714054\n            ],\n            [\n              -88.099365234375,\n              41.72213058512578\n            ],\n            [\n              -90.648193359375,\n              41.72213058512578\n            ],\n            [\n              -90.648193359375,\n              38.92522904714054\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hlavacek, Enrika 0000-0002-9872-2305 ehlavacek@usgs.gov","orcid":"https://orcid.org/0000-0002-9872-2305","contributorId":149114,"corporation":false,"usgs":true,"family":"Hlavacek","given":"Enrika","email":"ehlavacek@usgs.gov","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":825998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrison, Travis J. 0000-0002-9195-738X","orcid":"https://orcid.org/0000-0002-9195-738X","contributorId":213966,"corporation":false,"usgs":true,"family":"Harrison","given":"Travis","email":"","middleInitial":"J.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":826002,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knights, Brent C. 0000-0001-8526-8468 bknights@usgs.gov","orcid":"https://orcid.org/0000-0001-8526-8468","contributorId":2906,"corporation":false,"usgs":true,"family":"Knights","given":"Brent","email":"bknights@usgs.gov","middleInitial":"C.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":826003,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brey, Marybeth K. 0000-0003-4403-9655 mbrey@usgs.gov","orcid":"https://orcid.org/0000-0003-4403-9655","contributorId":187651,"corporation":false,"usgs":true,"family":"Brey","given":"Marybeth","email":"mbrey@usgs.gov","middleInitial":"K.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":826004,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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,{"id":70217015,"text":"70217015 - 2019 - Stream corridor sources of suspended sediment and phosphorus from an agricultural tributary to the Great Lakes","interactions":[],"lastModifiedDate":"2022-01-12T15:25:18.324113","indexId":"70217015","displayToPublicDate":"2019-12-31T10:19:52","publicationYear":"2019","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Stream corridor sources of suspended sediment and phosphorus from an agricultural tributary to the Great Lakes","docAbstract":"Fine-grained sediment and phosphorous are major contaminants in the Great Lakes and their tributaries. Plum Creek, Wisconsin (92 km2), a tributary to the Lower Fox River, has a Total Maximum Daily Load \n(TMDL) requiring reductions of suspended sediment and phosphorus loading by 70% and 77%, respectively.  In 2016-18, an integrated sediment fingerprinting and stream corridor-based sediment budget study was conducted to help quantify upland and stream corridor sources of suspended sediment and phosphorus at a loads monitoring station on Plum Creek. Sediment fingerprinting results indicated that the proportion of upland and stream corridor sources of suspended sediment in Plum Creek varied by season and the amount of runoff; however, bank and gully erosion accounted for 51% and 24% of the suspended sediment annual load, with one or both sources present in all seasons. The next most common source was roadside ditches (11%), which was also present in all seasons. Cropland and woodland sources accounted for small proportions of the suspended sediment, with cropland mainly in summer and woodland in winter, spring, and summer.  Relative source proportions for sediment-bound phosphorus were similar to suspended sediment but made up less of the overall loading because on average 27% of the phosphorus load resides in the dissolved phase. Soft fine-grained streambed sediment had source signatures of mainly bank, gully, and ditches (ordered by decreasing proportion).  Results from the field-based rapid geomorphic assessment supported the sediment fingerprinting results and in general showed that the amount of bank erosion increases in a downstream direction. The high proportion of sources from banks and gullies is due, in part, to a 20-km long, deeply entrenched valley and steep eroding bluffs between the majority of cropland and the Plum Creek water monitoring station.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of SEDHYD 2019","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"SEDHYD 2019 Conference","conferenceDate":"June 24-28, 2019","conferenceLocation":"Reno, NV","language":"English","publisher":"Federal Interagency Sedimentation and Hydrologic Modeling Conference","usgsCitation":"Fitzpatrick, F., Blount, J.D., Kammel, L., Hoover, D.L., Gellis, A.C., and Eikenberry, B., 2019, Stream corridor sources of suspended sediment and phosphorus from an agricultural tributary to the Great Lakes, <i>in</i> Proceedings of SEDHYD 2019, v. 4, Reno, NV, June 24-28, 2019, 15 p.","productDescription":"15 p.","ipdsId":"IP-105547","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"links":[{"id":381651,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":381637,"type":{"id":15,"text":"Index Page"},"url":"https://www.sedhyd.org/2019/#sedhyd-2019-proceedings"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Plum Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.2100,\n              44.17500\n            ],\n            [\n              -88.090,\n              44.17500\n            ],\n            [\n              -88.090,\n              44.3100\n            ],\n            [\n              -88.2100,\n              44.3100\n            ],\n            [\n              -88.2100,\n              44.17500\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fitzpatrick, Faith A. 0000-0002-9748-7075","orcid":"https://orcid.org/0000-0002-9748-7075","contributorId":209612,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Faith A.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":807269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blount, James D. 0000-0002-0006-3947 jblount@usgs.gov","orcid":"https://orcid.org/0000-0002-0006-3947","contributorId":200231,"corporation":false,"usgs":true,"family":"Blount","given":"James","email":"jblount@usgs.gov","middleInitial":"D.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":807270,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kammel, Leah 0000-0003-4613-0858","orcid":"https://orcid.org/0000-0003-4613-0858","contributorId":211840,"corporation":false,"usgs":true,"family":"Kammel","given":"Leah","email":"","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":807271,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hoover, David L. dlhoover@usgs.gov","contributorId":245331,"corporation":false,"usgs":false,"family":"Hoover","given":"David","email":"dlhoover@usgs.gov","middleInitial":"L.","affiliations":[{"id":49151,"text":"USDA-ARS Rangeland Resources Research Unit, Crops Research Laboratory, Fort Collins, CO","active":true,"usgs":false}],"preferred":false,"id":807272,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gellis, Allen C. 0000-0002-3449-2889 agellis@usgs.gov","orcid":"https://orcid.org/0000-0002-3449-2889","contributorId":197684,"corporation":false,"usgs":true,"family":"Gellis","given":"Allen","email":"agellis@usgs.gov","middleInitial":"C.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":807273,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Eikenberry, Barbara C. Scudder 0000-0001-8058-1201 beikenberry@usgs.gov","orcid":"https://orcid.org/0000-0001-8058-1201","contributorId":172148,"corporation":false,"usgs":true,"family":"Eikenberry","given":"Barbara C. Scudder","email":"beikenberry@usgs.gov","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":807274,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70226988,"text":"70226988 - 2019 - Conceptual framework for assessing disturbance impacts on debris-flow initiation thresholds across hydroclimatic settings","interactions":[],"lastModifiedDate":"2021-12-23T16:25:36.085154","indexId":"70226988","displayToPublicDate":"2019-12-31T10:12:35","publicationYear":"2019","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Conceptual framework for assessing disturbance impacts on debris-flow initiation thresholds across hydroclimatic settings","docAbstract":"<p><span>The destructive and deadly nature of debris flows has motivated research into empirical rainfall thresholds to provide situational awareness, inform early warning systems, and reduce loss of life and property. Disturbances such as wildfire and land-cover change can influence the hydrological processes of infiltration and runoff generation; in steep terrain this typically lowers empirical thresholds for debris-flow initiation. However, disturbance impacts, and the post-disturbance recovery may differ, depending on the severity, nature, extent, and duration of the disturbance, as well as on the prevailing hydroclimatic conditions. Thus, it can be difficult to predict impacts on debris-flows hazards in regions where historically such disturbances have been less frequent or severe. Given the increasing magnitude and incidence of wildfires, among other disturbances, we seek to develop a conceptual framework for assessing their impacts on debris-flow hazards across geographic regions. We characterize the severity of disturbances in terms of changes from undisturbed hydrologic functioning, including hillslope drainage and available unsaturated storage capacity, which can have contrasting influences on debris-flow initiation mechanisms in different hydroclimatic settings. We compare the timescale of disturbance-recovery cycles relative to the return period of threshold exceeding storms to describe vulnerability to post-disturbance debris flows. Similarly, we quantify resilience by comparing the timescales of disturbance-recovery cycles with those of disturbance-recurrence intervals. We illustrate the utility of these concepts using information from U.S. Geological Survey landslide monitoring sites in burned and unburned areas across the United States. Increasing severity of disturbance may influence both recovery timescales and lower the return period for debris-flow inducing storms, thus increasing the vulnerability to disturbance-related hazards while also decreasing system resilience. The proposed conceptual framework can inform future data acquisition and model development to improve debris-flow initiation thresholds in areas experiencing increasingly frequent, severe, and even overlapping landscape disturbances.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Debris-flow hazards mitigation: Mechanics, monitoring, modeling, and assessment; proceedings of the Seventh International Conference on Debris-Flow Hazards Mitigation","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Seventh International Conference on Debris-Flow Hazards Mitigation","conferenceDate":"Jun 10-13, 2019","conferenceLocation":"Golden, CO","language":"English","publisher":"Association of Environmental and Engineering Geologists","doi":"10.25676/11124/173176","usgsCitation":"Mirus, B.B., Staley, D.M., Kean, J.W., Smith, J.B., Wooten, R., McGuire, L.A., and Ebel, B., 2019, Conceptual framework for assessing disturbance impacts on debris-flow initiation thresholds across hydroclimatic settings, <i>in</i> Debris-flow hazards mitigation: Mechanics, monitoring, modeling, and assessment; proceedings of the Seventh International Conference on Debris-Flow Hazards Mitigation, Golden, CO, Jun 10-13, 2019, 8 p., https://doi.org/10.25676/11124/173176.","productDescription":"8 p.","ipdsId":"IP-105027","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":393369,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Mirus, Benjamin B. 0000-0001-5550-014X bbmirus@usgs.gov","orcid":"https://orcid.org/0000-0001-5550-014X","contributorId":4064,"corporation":false,"usgs":true,"family":"Mirus","given":"Benjamin","email":"bbmirus@usgs.gov","middleInitial":"B.","affiliations":[{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true},{"id":5077,"text":"Northwest Regional Director's Office","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":829098,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Staley, Dennis M. 0000-0002-2239-3402 dstaley@usgs.gov","orcid":"https://orcid.org/0000-0002-2239-3402","contributorId":4134,"corporation":false,"usgs":true,"family":"Staley","given":"Dennis","email":"dstaley@usgs.gov","middleInitial":"M.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":829099,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kean, Jason W. 0000-0003-3089-0369 jwkean@usgs.gov","orcid":"https://orcid.org/0000-0003-3089-0369","contributorId":1654,"corporation":false,"usgs":true,"family":"Kean","given":"Jason","email":"jwkean@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":829100,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Joel B. 0000-0001-7219-7875 jbsmith@usgs.gov","orcid":"https://orcid.org/0000-0001-7219-7875","contributorId":4925,"corporation":false,"usgs":true,"family":"Smith","given":"Joel","email":"jbsmith@usgs.gov","middleInitial":"B.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":829101,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wooten, Rick","contributorId":217741,"corporation":false,"usgs":false,"family":"Wooten","given":"Rick","email":"","affiliations":[{"id":24614,"text":"North Carolina Geological Survey","active":true,"usgs":false}],"preferred":false,"id":829102,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McGuire, Luke A. 0000-0001-8178-7922 lmcguire@usgs.gov","orcid":"https://orcid.org/0000-0001-8178-7922","contributorId":203420,"corporation":false,"usgs":false,"family":"McGuire","given":"Luke","email":"lmcguire@usgs.gov","middleInitial":"A.","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":829103,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ebel, Brian A. 0000-0002-5413-3963","orcid":"https://orcid.org/0000-0002-5413-3963","contributorId":211845,"corporation":false,"usgs":true,"family":"Ebel","given":"Brian A.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":829104,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70219018,"text":"70219018 - 2019 - Berea Sandstone petroleum system","interactions":[],"lastModifiedDate":"2021-09-29T15:12:48.075696","indexId":"70219018","displayToPublicDate":"2019-12-31T10:07:25","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":9141,"text":"Final Report","active":true,"publicationSubtype":{"id":2}},"title":"Berea Sandstone petroleum system","docAbstract":"Since 2011, production of sweet high gravity oil from the Upper Devonian Berea\nSandstone in northeastern Kentucky has caused the region to become the leading oil producer in\nthe state. Remarkably, Berea oil is being produced at depths of 2,200 ft or less and in an area in\nwhich the prospective source rocks—the overlying Mississippian Sunbury Shale and underlying\nDevonian Shale—are interpreted to be immature for oil production. Further downdip, the Berea\nappears to produce primarily gas in the oil window. The economic viability of Berea production\nis also a function of reservoir porosity and permeability.","language":"English","publisher":"Kentucky Geological Survey","usgsCitation":"Parris, T.M., Greb, S.F., Eble, C.F., Hackley, P.C., and Harris, D., 2019, Berea Sandstone petroleum system: Final Report, 342 p.","productDescription":"342 p.","ipdsId":"IP-089159","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":389960,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":389959,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.uky.edu/KGS/#"}],"country":"United States","state":"Kentucky","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.0179443359375,\n              36.63316209558658\n            ],\n            [\n              -81.0406494140625,\n              36.63316209558658\n            ],\n            [\n              -81.0406494140625,\n              38.68122173079789\n            ],\n            [\n              -84.0179443359375,\n              38.68122173079789\n            ],\n            [\n              -84.0179443359375,\n              36.63316209558658\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Parris, T. Marty","contributorId":255516,"corporation":false,"usgs":false,"family":"Parris","given":"T.","email":"","middleInitial":"Marty","affiliations":[{"id":51568,"text":"Kentucky Geological Survey, U. of Kentucky","active":true,"usgs":false}],"preferred":false,"id":812476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greb, Stephen F.","contributorId":255517,"corporation":false,"usgs":false,"family":"Greb","given":"Stephen","email":"","middleInitial":"F.","affiliations":[{"id":51568,"text":"Kentucky Geological Survey, U. of Kentucky","active":true,"usgs":false}],"preferred":false,"id":812477,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eble, Cortland F.","contributorId":255518,"corporation":false,"usgs":false,"family":"Eble","given":"Cortland","email":"","middleInitial":"F.","affiliations":[{"id":51568,"text":"Kentucky Geological Survey, U. of Kentucky","active":true,"usgs":false}],"preferred":false,"id":812478,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hackley, Paul C. 0000-0002-5957-2551 phackley@usgs.gov","orcid":"https://orcid.org/0000-0002-5957-2551","contributorId":592,"corporation":false,"usgs":true,"family":"Hackley","given":"Paul","email":"phackley@usgs.gov","middleInitial":"C.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":812479,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Harris, David C.","contributorId":255519,"corporation":false,"usgs":false,"family":"Harris","given":"David C.","affiliations":[{"id":51568,"text":"Kentucky Geological Survey, U. of Kentucky","active":true,"usgs":false}],"preferred":false,"id":812480,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70195160,"text":"70195160 - 2019 - Soil microbial communities and global change","interactions":[],"lastModifiedDate":"2022-04-01T22:26:33.074383","indexId":"70195160","displayToPublicDate":"2019-12-31T10:04:00","publicationYear":"2019","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Soil microbial communities and global change","docAbstract":"<p><span>Soils and soil microbial communities mediate the biogeochemical processes that underly ecosystem-level changes. This chapter examines why soils and soil microbial communities are important for understanding impacts and feedbacks to global change. It discusses the technological approaches and challenges that are at the frontiers of this research area. Global change impacts on microbial communities can be categorized as press or pulse disturbances. Global increases in atmospheric temperature are among the most profound and concerning long-term changes affecting human society. The chapter focuses on the examples from Western North America, where issues such as land cover change, wildfire, and permafrost thaw are some of the most observable global change impacts. Wildfire is a natural phenomenon that lies at the basis of the process of plant succession. Recovery and regrowth of vegetation after wildfire regenerates carbon and nutrient pools, such that long-term impacts on the ecosystems may be small.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Modern soil microbiology","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Taylor & Francis Group","usgsCitation":"Waldrop, M.P., and Creamer, C., 2019, Soil microbial communities and global change, chap. <i>of</i> Modern soil microbiology, p. 331-342.","productDescription":"12 p.","startPage":"331","endPage":"342","ipdsId":"IP-084471","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":397980,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":397989,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.taylorfrancis.com/chapters/edit/10.1201/9780429059186-20/soil-microbial-communities-global-change-mark-waldrop-courtney-creamer?context=ubx&refId=a340edd4-6f21-429b-96d4-933539849372"}],"publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"van Elsas, Jan Dirk","contributorId":289592,"corporation":false,"usgs":false,"family":"van Elsas","given":"Jan","email":"","middleInitial":"Dirk","affiliations":[],"preferred":false,"id":839396,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Trevors, Jack T.","contributorId":289593,"corporation":false,"usgs":false,"family":"Trevors","given":"Jack","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":839397,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Rosado, Alexandre Soares","contributorId":289594,"corporation":false,"usgs":false,"family":"Rosado","given":"Alexandre","email":"","middleInitial":"Soares","affiliations":[],"preferred":false,"id":839398,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Nannipieri, Paolo","contributorId":289595,"corporation":false,"usgs":false,"family":"Nannipieri","given":"Paolo","email":"","affiliations":[],"preferred":false,"id":839399,"contributorType":{"id":2,"text":"Editors"},"rank":4}],"authors":[{"text":"Waldrop, Mark P. 0000-0003-1829-7140 mwaldrop@usgs.gov","orcid":"https://orcid.org/0000-0003-1829-7140","contributorId":1599,"corporation":false,"usgs":true,"family":"Waldrop","given":"Mark","email":"mwaldrop@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":727250,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Creamer, Courtney 0000-0001-8270-9387","orcid":"https://orcid.org/0000-0001-8270-9387","contributorId":201952,"corporation":false,"usgs":true,"family":"Creamer","given":"Courtney","email":"","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":727251,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211754,"text":"70211754 - 2019 - Recovery planning in a dynamic system: Integrating uncertainty into a decision support tool for an endangered songbird","interactions":[],"lastModifiedDate":"2020-08-07T14:59:38.820693","indexId":"70211754","displayToPublicDate":"2019-12-31T09:50:59","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1468,"text":"Ecology and Society","active":true,"publicationSubtype":{"id":10}},"title":"Recovery planning in a dynamic system: Integrating uncertainty into a decision support tool for an endangered songbird","docAbstract":"<div id=\"abstract_block\">Along the Santa Clara River in California, populations of the federally and state-listed Least Bell's Vireo (<i>Vireo bellii pusillus</i>) are recovering from near extirpation. Habitat protection and restoration, as well as controlling rates of brood parasitism, are thought to be the primary drivers of this recovery. Continuing successful management of this population faces multiple challenges due to the highly dynamic and unpredictable nature of the system, lack of clearly defined and measurable recovery criteria, parametric and stochastic uncertainty, and data limitations. Many of these management challenges are not unique to Least Bell's Vireo and require careful balancing of limited resources into the future. We developed a decision support tool as a user interface for exploring the underlying uncertainty in a population viability analysis under an array of different management scenarios. The tool was designed to assist with the planning and coordination between conservation partners in the region in three distinct aspects of the decision-making process: defining the problem and setting clear goals and objectives, exploring the consequences of potential alternative actions, and identifying criteria for ongoing evaluation and monitoring. The general framework for the design of this decision support tool is broadly applicable to many management and decision-making scenarios that share these common challenges.</div>","language":"English","publisher":"Ecology and Society","doi":"10.5751/ES-11169-240411","usgsCitation":"Stanton, J., Marek, J., Hall, L., Kus, B., Alvarado, A., Orr, B.K., Morrissette, E., Riege, L., and Thogmartin, W.E., 2019, Recovery planning in a dynamic system: Integrating uncertainty into a decision support tool for an endangered songbird: Ecology and Society, v. 24, no. 4, Article: 11, 19 p.; Data Release, https://doi.org/10.5751/ES-11169-240411.","productDescription":"Article: 11, 19 p.; Data Release","ipdsId":"IP-101205","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":458863,"rank":3,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5751/es-11169-240411","text":"Publisher Index Page"},{"id":437243,"rank":2,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9VNZI1W","text":"USGS data release","linkHelpText":"Least Bell's Vireo on the Santa Clara River, CA: decision support tool"},{"id":377177,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":377176,"rank":1,"type":{"id":30,"text":"Data Release"},"url":"https://www.sciencebase.gov/catalog/item/5d1f7535e4b0941bde64dbf5","text":"Data release","description":"USGS data release","linkHelpText":"Multiple Objective Vireo Explorer: Decision-making for the Least Bell's Vireo on the Santa Clara River, CA"}],"country":"United States","state":"California","otherGeospatial":"Santa Clara River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  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,{"id":70206602,"text":"sir20195134 - 2019 - Transmissivity and geophysical data for selected wells at and near the Idaho National Laboratory, Idaho, 2017–18","interactions":[],"lastModifiedDate":"2022-04-25T19:42:53.799577","indexId":"sir20195134","displayToPublicDate":"2019-12-31T09:34:26","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-5134","displayTitle":"Transmissivity and Geophysical Data for Selected Wells at and Near the Idaho National Laboratory, Idaho, 2017–18","title":"Transmissivity and geophysical data for selected wells at and near the Idaho National Laboratory, Idaho, 2017–18","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the U.S. Department of Energy, conducted aquifer tests during 2017–18 on 101 wells at and near the Idaho National Laboratory, Idaho, to define the hydraulic characteristics for individual wells. These were short-duration aquifer tests, conducted with a limited number of observations during routine sampling. Pumped intervals (water columns) for individual wells ranged from 12 to 790 feet (ft). Semi-constant discharge rates during aquifer testing ranged from 1 to 45 gallons per minute, water-level response to pumping ranged from no observed drawdown to 52.4 ft, and length of aquifer tests for individual wells ranged from 10 to 160 minutes. Individual well data were analyzed to estimate the capacity of the well to produce water (specific capacity) and to estimate values for transmissivity. Estimates of specific capacity for individual wells ranged from less than 1.0 to greater than (&gt;) 3.0 × 10<sup>3</sup> gallons per minute per foot; estimates of transmissivity for individual wells ranged from 2.0 to &gt;5.4 x 10<sup>5</sup> feet squared per day.</p><p>Geophysical log data, well construction information, and general geology for individual wells were presented and included in this report. Basic hydrogeologic features for individual wells were described, along with a composite of natural gamma, neutron, gamma-gamma dual density, and acoustic televiewer data (when available). The geophysical and geologic data were used to suggest the location and thickness of sediment layers along with fractured and dense basalt areas for individual wells. Geophysical data were used to describe the general geology where geologic descriptions and (or) driller notes were not available.<br></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20195134","collaboration":"Prepared in cooperation with the U.S. Department of Energy","usgsCitation":"Twining, B.V., and Maimer, N.V., 2019, Transmissivity and geophysical data for selected wells located at and near the Idaho National Laboratory, Idaho, 2017–18: U.S. Geological Survey Scientific Investigations Report 2019-5134, 30 p. plus appendixes, https://doi.org/10.3133/sir20195134.","productDescription":"Report: vi, 30 p.; 2 Appendixes","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-092370","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":370885,"rank":4,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/sir/2019/5134/sir20195134_appendix2.pdf","text":"Appendix 2","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2019-5134 Appendix 2","linkHelpText":"- Aquifer Test Data Collected For Individual Wells"},{"id":370884,"rank":3,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/sir/2019/5134/sir20195134_appendix1.pdf","text":"Appendix 1","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2019-5134 Appendix 1","linkHelpText":"- Geophysical Logs And Construction Information For Aquifer Test Wells"},{"id":370883,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2019/5134/sir20195134.pdf","text":"Report","size":"2.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2019-5134"},{"id":370882,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2019/5134/coverthb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho National Laboratory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.16629028320312,\n              43.402054267905655\n            ],\n            [\n              -111.87515258789062,\n              43.402054267905655\n            ],\n            [\n              -111.87515258789062,\n              43.68872888432795\n            ],\n            [\n              -112.16629028320312,\n              43.68872888432795\n            ],\n            [\n              -112.16629028320312,\n              43.402054267905655\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a data-mce-href=\"https://www.usgs.gov/centers/id-water/connect\" href=\"https://www.usgs.gov/centers/id-water/connect\" target=\"_blank\" rel=\"noopener\">Director</a>,<br><a data-mce-href=\"https://www.usgs.gov/centers/id-water\" href=\"https://www.usgs.gov/centers/id-water\" target=\"_blank\" rel=\"noopener\">Idaho Water Science Center</a><br><a data-mce-href=\"https://www.usgs.gov/\" href=\"https://www.usgs.gov/\" target=\"_blank\" rel=\"noopener\">U.S. Geological Survey</a><br>230 Collins Road<br>Boise, Idaho 83702-4520<br></p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Geophysical Data</li><li>Description of Wells</li><li>Aquifer Test Methods and Analysis</li><li>Review of Well Productivity</li><li>Geologic Controls on Estimated Transmissivity</li><li>Summary</li><li>References Cited</li><li>Appendixes</li></ul><p><br></p>","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"publishedDate":"2019-12-31","noUsgsAuthors":false,"publicationDate":"2019-12-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Twining, Brian V. 0000-0003-1321-4721 btwining@usgs.gov","orcid":"https://orcid.org/0000-0003-1321-4721","contributorId":2387,"corporation":false,"usgs":true,"family":"Twining","given":"Brian","email":"btwining@usgs.gov","middleInitial":"V.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":775115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maimer, Neil V. 0000-0003-3047-3282 nmaimer@usgs.gov","orcid":"https://orcid.org/0000-0003-3047-3282","contributorId":5659,"corporation":false,"usgs":true,"family":"Maimer","given":"Neil","email":"nmaimer@usgs.gov","middleInitial":"V.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":775116,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215564,"text":"70215564 - 2019 - Geomorphic controls on hyporheic exchange across scales - Watersheds to particles","interactions":[],"lastModifiedDate":"2020-10-23T14:30:58.631025","indexId":"70215564","displayToPublicDate":"2019-12-31T09:28:53","publicationYear":"2019","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Geomorphic controls on hyporheic exchange across scales - Watersheds to particles","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab0010\" class=\"abstract author\" lang=\"en\"><div id=\"as0010\"><p id=\"sp0060\">We examined the relationship between fluvial geomorphology and hyporheic exchange flows. We use geomorphology as a framework to understand hyporheic processes and how these processes change with location within a stream network, and over time in response to changes in stream discharge and catchment wetness. We focus primarily on hydrostatic and hydrodynamic processes—the processes where linkages to fluvial geomorphology are most direct. Hydrostatic processes result from morphologic features that create elevational head gradients whereas hydrodynamic processes result from the interaction between stream flow and channel morphologic features. We provide examples of the specific morphologic features that drive or enable hyporheic exchange and we examine how these processes interact in real stream networks to create complex subsurface flow nets through the hyporheic zone.</p></div></div></div>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Treatise on fluvial geomorphology","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Elsevier","doi":"10.1016/B978-0-12-409548-9.12135-9","usgsCitation":"Wondzell, S., Herzog, S., Gooseff, M., Ward, A.S., and Schmadel, N., 2019, Geomorphic controls on hyporheic exchange across scales - Watersheds to particles, chap. <i>of</i> Treatise on fluvial geomorphology, https://doi.org/10.1016/B978-0-12-409548-9.12135-9.","ipdsId":"IP-114197","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":379692,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wondzell, Steven","contributorId":242771,"corporation":false,"usgs":false,"family":"Wondzell","given":"Steven","affiliations":[{"id":37019,"text":"USDA Forest Service, Pacific Northwest Research Station","active":true,"usgs":false}],"preferred":false,"id":802740,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herzog, Skuyler","contributorId":242772,"corporation":false,"usgs":false,"family":"Herzog","given":"Skuyler","affiliations":[{"id":48520,"text":"O’Neill School of Public and Environmental Affairs, Indiana University, Bloomington, Indiana, USA","active":true,"usgs":false}],"preferred":false,"id":802741,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gooseff, Michael","contributorId":181942,"corporation":false,"usgs":false,"family":"Gooseff","given":"Michael","affiliations":[],"preferred":false,"id":802742,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ward, Adam S","contributorId":191363,"corporation":false,"usgs":false,"family":"Ward","given":"Adam","email":"","middleInitial":"S","affiliations":[],"preferred":false,"id":802743,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schmadel, Noah 0000-0002-2046-1694","orcid":"https://orcid.org/0000-0002-2046-1694","contributorId":219105,"corporation":false,"usgs":true,"family":"Schmadel","given":"Noah","email":"","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":802744,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70226986,"text":"70226986 - 2019 - Overcoming barriers to progress in seismic monitoring and characterization of debris flows and lahars","interactions":[],"lastModifiedDate":"2021-12-23T16:29:29.031603","indexId":"70226986","displayToPublicDate":"2019-12-31T09:06:53","publicationYear":"2019","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Overcoming barriers to progress in seismic monitoring and characterization of debris flows and lahars","docAbstract":"<p><span>Debris flows generate seismic signals that contain valuable information about events as they unfold. Though seismic waves have been used for along-channel debris-flow and lahar monitoring systems for decades, it has proven difficult to move beyond detection to more quantitative characterizations of flow parameters and event size. This is for two primary reasons: (1) our limited understanding of how the radiated wavefield relates to debris flow characteristics and dynamics, and (2) difficulties quantifying the effects of heterogeneous shallow earth structure on the observed wavefield. The latter issue, essentially our inability to sufficiently separate seismic path effects from source information, is a barrier to improving our understanding of the first issue. We review the progress that has been made toward establishing the theory, models and methods required to use seismic observations to make quantitative measurements of flows and summarize the practical, social, and scientific barriers to progress. We discuss some specific ongoing efforts to overcome some of these barriers, with a focus on how we are using large-scale seismic experiments at the U.S. Geological Survey debris-flow flume to develop methods for directly measuring path effects and to develop and validate theoretical debris flow seismicity models.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Debris-flow hazards mitigation: Mechanics, monitoring, modeling, and assessment; proceedings of the Seventh International Conference on Debris-Flow Hazards Mitigation","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Seventh International Conference on Debris-Flow Hazards Mitigation","conferenceDate":"Jun 10-13, 2019","conferenceLocation":"Golden, CO","language":"English","publisher":"Association of Environmental and Engineering Geologists","doi":"10.25676/11124/173234","usgsCitation":"Allstadt, K.E., Farin, M., Lockhart, A., McBride, S., Kean, J.W., Iverson, R.M., Logan, M., Smith, J.B., Tsai, V.C., and George, D.L., 2019, Overcoming barriers to progress in seismic monitoring and characterization of debris flows and lahars, <i>in</i> Debris-flow hazards mitigation: Mechanics, monitoring, modeling, and assessment; proceedings of the Seventh International Conference on Debris-Flow Hazards Mitigation, Golden, CO, Jun 10-13, 2019, p. 77-84, https://doi.org/10.25676/11124/173234.","productDescription":"8 p.","startPage":"77","endPage":"84","ipdsId":"IP-105030","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":393357,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Allstadt, Kate E. 0000-0003-4977-5248","orcid":"https://orcid.org/0000-0003-4977-5248","contributorId":138704,"corporation":false,"usgs":true,"family":"Allstadt","given":"Kate","email":"","middleInitial":"E.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":829085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farin, Maxime 0000-0002-0250-2499","orcid":"https://orcid.org/0000-0002-0250-2499","contributorId":221438,"corporation":false,"usgs":false,"family":"Farin","given":"Maxime","email":"","affiliations":[{"id":7218,"text":"California Institute of Technology","active":true,"usgs":false}],"preferred":false,"id":829086,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lockhart, Andrew 0000-0002-1591-3254 ablock@usgs.gov","orcid":"https://orcid.org/0000-0002-1591-3254","contributorId":204748,"corporation":false,"usgs":true,"family":"Lockhart","given":"Andrew","email":"ablock@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":829087,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McBride, Sara K. 0000-0002-8062-6542","orcid":"https://orcid.org/0000-0002-8062-6542","contributorId":206933,"corporation":false,"usgs":true,"family":"McBride","given":"Sara K.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":829088,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kean, Jason W. 0000-0003-3089-0369 jwkean@usgs.gov","orcid":"https://orcid.org/0000-0003-3089-0369","contributorId":1654,"corporation":false,"usgs":true,"family":"Kean","given":"Jason","email":"jwkean@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":829089,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Iverson, Richard M. 0000-0002-7369-3819 riverson@usgs.gov","orcid":"https://orcid.org/0000-0002-7369-3819","contributorId":536,"corporation":false,"usgs":true,"family":"Iverson","given":"Richard","email":"riverson@usgs.gov","middleInitial":"M.","affiliations":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":829090,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Logan, Matthew 0000-0002-3558-2405 mlogan@usgs.gov","orcid":"https://orcid.org/0000-0002-3558-2405","contributorId":638,"corporation":false,"usgs":true,"family":"Logan","given":"Matthew","email":"mlogan@usgs.gov","affiliations":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":829091,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Smith, Joel B. 0000-0001-7219-7875 jbsmith@usgs.gov","orcid":"https://orcid.org/0000-0001-7219-7875","contributorId":4925,"corporation":false,"usgs":true,"family":"Smith","given":"Joel","email":"jbsmith@usgs.gov","middleInitial":"B.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":829092,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Tsai, Victor C. 0000-0003-1809-6672","orcid":"https://orcid.org/0000-0003-1809-6672","contributorId":199684,"corporation":false,"usgs":false,"family":"Tsai","given":"Victor","email":"","middleInitial":"C.","affiliations":[{"id":27150,"text":"Seismological Laboratory, California Institute of Technology, Pasadena, CA, USA","active":true,"usgs":false}],"preferred":false,"id":829093,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"George, David L. 0000-0002-5726-0255 dgeorge@usgs.gov","orcid":"https://orcid.org/0000-0002-5726-0255","contributorId":3120,"corporation":false,"usgs":true,"family":"George","given":"David","email":"dgeorge@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":829094,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
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