Streamgage designs often include a full-width artificial hydraulic control (e.g., concrete weir) to aid in the computation of streamflow. While important to water resource managers, these weirs also tend to act as full or partial barriers to fish migration, effectively hindering the health and survival of these populations. In this study, we conducted experiments to quantify the effect of head drop and submergence of a common streamgage weir on the passage performance of an important migratory fish species, the American Shad. Three treatment conditions were selected based on the tailwater surface elevation (ElTW): unsubmerged (ElTW = 1.05 m; head drop = 0.46 m), equal to the weir crest (ElTW = 1.20 m; head drop = 0.31 m), and submerged (ElTW = 1.36 m; head drop = 0.15 m). Fish movements were recorded via passive integrated transponder telemetry techniques. Results revealed that the backwatered Columbus-type weir was not a complete barrier at any of the three treatments, but passage was shown to be significantly impaired when the weir was unsubmerged. Passage efficiency for the unsubmerged, equal, and submerged treatments was 20.2 ± 6.2, 49.2 ± 7.2, and 64.2 ± 7.4%. Backwatering a weir, rather than removal or other major alterations that would affect weir calibration, may be an acceptable retrofit to increase fish passage.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/24705357.2021.1945500","usgsCitation":"Mulligan, K., Haro, A., and Noreika, J., 2024, Effect of backwatering a streamgage weir on the passage performance of adult American Shad (Alosa sapidissima): Journal of Ecohydraulics, v. 9, no. 2, p. 145-157, https://doi.org/10.1080/24705357.2021.1945500.","productDescription":"13 p.","startPage":"145","endPage":"157","ipdsId":"IP-121476","costCenters":[{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"links":[{"id":387121,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"2","noUsgsAuthors":false,"publicationDate":"2021-07-07","publicationStatus":"PW","contributors":{"authors":[{"text":"Mulligan, Kevin B. 0000-0002-3534-4239 kmulligan@usgs.gov","orcid":"https://orcid.org/0000-0002-3534-4239","contributorId":177024,"corporation":false,"usgs":true,"family":"Mulligan","given":"Kevin","email":"kmulligan@usgs.gov","middleInitial":"B.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":819109,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haro, Alexander 0000-0002-7188-9172 aharo@usgs.gov","orcid":"https://orcid.org/0000-0002-7188-9172","contributorId":139198,"corporation":false,"usgs":true,"family":"Haro","given":"Alexander","email":"aharo@usgs.gov","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":819110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Noreika, John 0000-0002-6637-5812 jnoreika@usgs.gov","orcid":"https://orcid.org/0000-0002-6637-5812","contributorId":167858,"corporation":false,"usgs":true,"family":"Noreika","given":"John","email":"jnoreika@usgs.gov","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":819111,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70220295,"text":"70220295 - 2024 - Sharing knowledge to improve ecological restoration outcomes","interactions":[],"lastModifiedDate":"2024-11-21T15:15:49.0223","indexId":"70220295","displayToPublicDate":"2021-04-23T07:03:43","publicationYear":"2024","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3271,"text":"Restoration Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Sharing knowledge to improve ecological restoration outcomes","docAbstract":"Ecological restoration efforts are likely to be more successful when project components are informed by relevant stakeholders. However, key stakeholders are often not included in restoration design and deployment. This is largely driven by a lack of practitioner knowledge of and experience with stakeholder relations. However, inclusion of stakeholders across the entire restoration process can be accomplished by practitioners with no formal social science training. Here, we describe several easy (and usually inexpensive) ways to formally cultivate relationships among restoration practitioners, researchers, and stakeholders to improve restoration outcomes. These include: how to identify and work with stakeholders; how to recognize the unique needs and contributions of stakeholder groups, and how to provide information back to stakeholders through outreach. Although how this practice occurs is dependent on restoration context, integrating these approaches more regularly into ecological restoration projects will likely result in more successful, relevant, and community-supported management outcomes.
","language":"English","publisher":"Wiley","doi":"10.1111/rec.13417","usgsCitation":"Gornish, E.S., McCormick, M.L., Begay, M., and Nsikani, M.M., 2024, Sharing knowledge to improve ecological restoration outcomes: Restoration Ecology, v. 32, no. 8, e13417, 7 p., https://doi.org/10.1111/rec.13417.","productDescription":"e13417, 7 p.","ipdsId":"IP-123710","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":385404,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"8","noUsgsAuthors":false,"publicationDate":"2021-07-28","publicationStatus":"PW","contributors":{"authors":[{"text":"Gornish, Elise S 0000-0002-2055-4874","orcid":"https://orcid.org/0000-0002-2055-4874","contributorId":240596,"corporation":false,"usgs":false,"family":"Gornish","given":"Elise","email":"","middleInitial":"S","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":815033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCormick, Molly L. 0000-0002-4361-7567 mmccormick@usgs.gov","orcid":"https://orcid.org/0000-0002-4361-7567","contributorId":196257,"corporation":false,"usgs":true,"family":"McCormick","given":"Molly","email":"mmccormick@usgs.gov","middleInitial":"L.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":815034,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Begay, Marquel","contributorId":257792,"corporation":false,"usgs":false,"family":"Begay","given":"Marquel","email":"","affiliations":[{"id":52121,"text":"University of Arizona, School of Natural Resources and the Environment, Tucson AZ 85711","active":true,"usgs":false}],"preferred":false,"id":815035,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nsikani, Mlungele M 0000-0002-5053-1649","orcid":"https://orcid.org/0000-0002-5053-1649","contributorId":257793,"corporation":false,"usgs":false,"family":"Nsikani","given":"Mlungele","email":"","middleInitial":"M","affiliations":[{"id":52122,"text":"South African National Biodiversity Institute, Kirstenbosch Research Centre, Claremont, South Africa; Centre for Invasion Biology, Department of Botany and Zoology, Stellenbosch University, Private Bag X1, Matieland 7602, South Africa","active":true,"usgs":false}],"preferred":false,"id":815036,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70261217,"text":"70261217 - 2024 - Historical and prehistorical water levels of Mormon Lake, Arizona as a measure of climate change on the southwest Colorado Plateau, USA","interactions":[],"lastModifiedDate":"2024-12-02T15:12:29.409176","indexId":"70261217","displayToPublicDate":"2021-03-01T00:00:00","publicationYear":"2024","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Historical and prehistorical water levels of Mormon Lake, Arizona as a measure of climate change on the southwest Colorado Plateau, USA","docAbstract":"Mormon Lake, elevation 2166 m with maximum historic surface area of 31.4 km2, lies in a forested endorheic basin covering 103 km2. It is the largest unaltered freshwater body on the 337,000 km2 Colorado Plateau. Prehistorical (before AD 1878) highstands were ca. 9 and 24 m relative to depocenter datum. These levels likely occurred during four multidecadal episodes of cool, wet conditions between ca. 3.55 and 0.20 ka BP. Maximum historical levels (early 1900s) were up to 7.9 m, whereas modern (post-1941) levels were frequently zero or relatively low. Historical climate records indicate reconstructed lake levels correlate directly with annual precipitation and inversely with temperature. Early highstands were associated with above average precipitation and the lowest temperatures of the 116 yr record. The lake receded after 1941; thereafter, frequent drying and low-water levels resulted from recurrent drought and steadily increasing temperatures. Consequently, a wet episode from the 1970s to the 1990s had precipitation like the early 1900s, but highstands were only ca. 3.8 m. The historical lake-level chronology is consistent with changes of hydrologic balance predicted by climate models, that is, reduced effective precipitation (precipitation minus evaporation). These changes, particularly aridification, apparently began in the 1970s or earlier. Global oceanic and atmospheric climate modulate lake levels and regional hydroclimate.
","language":"English","publisher":"Cambridge University Press","doi":"10.1017/qua.2020.92","usgsCitation":"Hereford, R., and Amoroso, L., 2024, Historical and prehistorical water levels of Mormon Lake, Arizona as a measure of climate change on the southwest Colorado Plateau, USA: Quaternary Research, v. 100, p. 32-51, https://doi.org/10.1017/qua.2020.92.","productDescription":"20 p.","startPage":"32","endPage":"51","ipdsId":"IP-113940","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":464625,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Mormon Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.48876598336788,\n 34.98966103819039\n ],\n [\n -111.48876598336788,\n 34.906130634842924\n ],\n [\n -111.42028354514014,\n 34.906130634842924\n ],\n [\n -111.42028354514014,\n 34.98966103819039\n ],\n [\n -111.48876598336788,\n 34.98966103819039\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"100","noUsgsAuthors":false,"publicationDate":"2020-12-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Hereford, Richard 0000-0002-0892-7367 rhereford@usgs.gov","orcid":"https://orcid.org/0000-0002-0892-7367","contributorId":3620,"corporation":false,"usgs":true,"family":"Hereford","given":"Richard","email":"rhereford@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":919934,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Amoroso, Lee 0000-0003-1342-7487","orcid":"https://orcid.org/0000-0003-1342-7487","contributorId":346805,"corporation":false,"usgs":false,"family":"Amoroso","given":"Lee","affiliations":[],"preferred":false,"id":919935,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70261874,"text":"70261874 - 2024 - Petrology and geochemistry of three early Holocene eruptions from Makushin volcano, Alaska","interactions":[],"lastModifiedDate":"2024-12-31T15:58:26.095859","indexId":"70261874","displayToPublicDate":"2020-10-19T00:00:00","publicationYear":"2024","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1109,"text":"Bulletin of Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"Petrology and geochemistry of three early Holocene eruptions from Makushin volcano, Alaska","docAbstract":"Makushin stratovolcano, Alaska, produced three, highly explosive, andesitic eruptions between ~ 9292 and 6215 yBP. Those eruptions are informally named the CFE (“crater-forming eruption”), Nateekin, and Driftwood Pumice, and they deposited significant tephra fallout in the present-day port of Dutch Harbor and City of Unalaska area. The focus of this study is to examine the geochemistry and petrology of those eruptions to better understand Makushin volcano hazards, andesite petrogenesis and eruption triggering by mafic recharge processes. The CFE, Nateekin, and Driftwood Pumice samples range from basaltic andesite to dacite but are predominantly andesitic (SiO2 = 55.6 to 63.5 wt%). The CFE deposits are slightly compositionally stratified, with the top CFE samples slightly more mafic (55 to 60 wt% SiO2) than the basal deposits (58 to 60 wt% SiO2). Disequilibrium mineral compositions and textures in the CFE, Nateekin, and Driftwood Pumice samples, combined with two pyroxene thermometry and An-rich plagioclase microlites (An80) found only in the top of the CFE deposits, provide evidence for repetitive mafic recharge triggering those eruptions, consistent with prior studies. We compare the Makushin geochemical data with data from select satellite vents and cones in the Makushin Volcanic Field (MVF) from prior studies, to examine possible genetic relationships. The geochemical data and Rhyolite-MELTS models run at crustal storage conditions (2 kbar, fO2 = Ni-NiO, and 1.5 and 3.5 wt% H2O) indicate that no single parental magma supplies the MVF satellite cones and Makushin volcano. Instead, two component mixing models better fit the MVF geochemical array. Our Makushin results compare well with models of predominantly andesitic volcanoes that require mafic recharge to mobilize the andesites and trigger eruptions.
","language":"English","publisher":"Springer Nature","doi":"10.1007/s00445-020-01412-5","usgsCitation":"Larsen, J., Schaefer, J., Vallance, J.W., and Neill, O., 2024, Petrology and geochemistry of three early Holocene eruptions from Makushin volcano, Alaska: Bulletin of Volcanology, v. 82, 72, 17 p., https://doi.org/10.1007/s00445-020-01412-5.","productDescription":"72, 17 p.","ipdsId":"IP-120635","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":465566,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Makushin volcano, Unalaska Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -167.01083004545683,\n 53.926684657654704\n ],\n [\n -167.01083004545683,\n 53.84297653402467\n ],\n [\n -166.85080239678533,\n 53.84297653402467\n ],\n [\n -166.85080239678533,\n 53.926684657654704\n ],\n [\n -167.01083004545683,\n 53.926684657654704\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"82","noUsgsAuthors":false,"publicationDate":"2020-10-19","publicationStatus":"PW","contributors":{"authors":[{"text":"Larsen, Jessica 0000-0003-1171-129X","orcid":"https://orcid.org/0000-0003-1171-129X","contributorId":242808,"corporation":false,"usgs":false,"family":"Larsen","given":"Jessica","email":"","affiliations":[{"id":6752,"text":"University of Alaska Fairbanks","active":true,"usgs":false}],"preferred":false,"id":922107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schaefer, Janet","contributorId":199547,"corporation":false,"usgs":false,"family":"Schaefer","given":"Janet","affiliations":[],"preferred":false,"id":922108,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vallance, James W. 0000-0002-3083-5469 jvallance@usgs.gov","orcid":"https://orcid.org/0000-0002-3083-5469","contributorId":547,"corporation":false,"usgs":true,"family":"Vallance","given":"James","email":"jvallance@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":922109,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Neill, O.K.","contributorId":347659,"corporation":false,"usgs":false,"family":"Neill","given":"O.K.","affiliations":[{"id":37387,"text":"University of Michigan","active":true,"usgs":false}],"preferred":false,"id":922110,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70254082,"text":"70254082 - 2024 - Puget small streams monitoring program annual status report, water year 2020","interactions":[],"lastModifiedDate":"2024-05-08T22:16:29.724043","indexId":"70254082","displayToPublicDate":"2020-05-06T06:55:13","publicationYear":"2024","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Puget small streams monitoring program annual status report, water year 2020","docAbstract":"This status report summarizes data collection from Summer 2020 for the Stormwater Action Monitoring (SAM) project.","language":"English","publisher":"Washington State Department of Ecology","usgsCitation":"Sheibley, R.W., 2024, Puget small streams monitoring program annual status report, water year 2020, 21 p.","productDescription":"21 p.","ipdsId":"IP-162509","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":428416,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.ezview.wa.gov/Portals/_1962/Documents/SAM/D4.1_AnnualReport_2020.pdf"},{"id":428431,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Puget Sound","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.46305724863647,\n 49.17206387174522\n ],\n [\n -124.46305724863647,\n 46.75986786483739\n ],\n [\n -121.52970763926143,\n 46.75986786483739\n ],\n [\n -121.52970763926143,\n 49.17206387174522\n ],\n [\n -124.46305724863647,\n 49.17206387174522\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sheibley, Rich W. 0000-0003-1627-8536 sheibley@usgs.gov","orcid":"https://orcid.org/0000-0003-1627-8536","contributorId":3044,"corporation":false,"usgs":true,"family":"Sheibley","given":"Rich","email":"sheibley@usgs.gov","middleInitial":"W.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":900172,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70240757,"text":"70240757 - 2024 - Efficient mammal biodiversity surveys for ecological restoration monitoring","interactions":[],"lastModifiedDate":"2024-10-23T15:47:31.059833","indexId":"70240757","displayToPublicDate":"2020-04-01T16:13:20","publicationYear":"2024","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2006,"text":"Integrated Environmental Assessment and Management","active":true,"publicationSubtype":{"id":10}},"title":"Efficient mammal biodiversity surveys for ecological restoration monitoring","docAbstract":"Efficient biodiversity surveys are critical for successful restoration monitoring and management. We studied the effect of varying sampling effort on the observed species richness of surveys of small mammals (trapping transects), bats (passive acoustic detection), and medium to large mammals (trail cameras). Field studies provided mammalian biodiversity data for 4 bottomland hardwood restoration sites in northeastern Indiana. Subsampled data were used to simulate monitoring surveys with a range of levels of effort. We then used hierarchical Bayesian nonlinear mixed models to analyze how different components of sampling effort affected observed species richness, a key monitoring outcome. We found that observed small mammal richness increased with the increased number of transects in a survey, while observed bat and medium to large mammal richness increased with the increased duration of sampling. Variation between sites was important for the observed richness of small mammals and bats but not for medium to large mammals. The key driver of richness observed in simulated surveys was related to the spatial scale at which target fauna interact with the habitat, with decreasing richness accompanied by a greater spatial scale of animal–habitat interactions. Our findings suggest taxon-specific recommendations for efficiently quantifying the mammalian diversity of managed sites.
","language":"English","publisher":"Wiley","doi":"10.1002/ieam.4324","usgsCitation":"Green, N., Wildhaber, M.L., Albers, J.L., Pettit, T.W., and Hooper, M.J., 2024, Efficient mammal biodiversity surveys for ecological restoration monitoring: Integrated Environmental Assessment and Management, v. 20, no. 6, p. 1969-1981, https://doi.org/10.1002/ieam.4324.","productDescription":"13 p.","startPage":"1969","endPage":"1981","ipdsId":"IP-110582","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":435587,"rank":1,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9RXPYRL","text":"USGS data release","linkHelpText":"Mammalian biodiversity data for four bottomland hardwood restoration sites in Northeastern Indiana USA May 2015-August 2016"},{"id":413227,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":445571,"rank":3,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/ieam.4324","text":"Publisher Index Page"}],"country":"United States","state":"Indiana","city":"Bluffton, New Haven","otherGeospatial":"Bluffton Native Habitat Waterway Project, Deetz Nature Preserve, Fish Creek complex","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -85.20456175119196,\n 40.762112614423955\n ],\n [\n -85.20456175119196,\n 40.70016025503452\n ],\n [\n -85.08914278782409,\n 40.70016025503452\n ],\n [\n -85.08914278782409,\n 40.762112614423955\n ],\n [\n -85.20456175119196,\n 40.762112614423955\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -84.97371420873174,\n 41.57466064563525\n ],\n [\n -84.97371420873174,\n 41.508602936877736\n ],\n [\n -84.83648016376709,\n 41.508602936877736\n ],\n [\n -84.83648016376709,\n 41.57466064563525\n ],\n [\n -84.97371420873174,\n 41.57466064563525\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -85.07991405934287,\n 41.11589628289104\n ],\n [\n -85.07991405934287,\n 41.048923920315474\n ],\n [\n -84.97206799999923,\n 41.048923920315474\n ],\n [\n -84.97206799999923,\n 41.11589628289104\n ],\n [\n -85.07991405934287,\n 41.11589628289104\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"20","issue":"6","noUsgsAuthors":false,"publicationDate":"2020-08-08","publicationStatus":"PW","contributors":{"authors":[{"text":"Green, Nicholas S. 0000-0002-8538-4191","orcid":"https://orcid.org/0000-0002-8538-4191","contributorId":202040,"corporation":false,"usgs":true,"family":"Green","given":"Nicholas S.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":864719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wildhaber, Mark L. 0000-0002-6538-9083 mwildhaber@usgs.gov","orcid":"https://orcid.org/0000-0002-6538-9083","contributorId":1386,"corporation":false,"usgs":true,"family":"Wildhaber","given":"Mark","email":"mwildhaber@usgs.gov","middleInitial":"L.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":864720,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Albers, Janice L. 0000-0002-6312-8269 jalbers@usgs.gov","orcid":"https://orcid.org/0000-0002-6312-8269","contributorId":3972,"corporation":false,"usgs":true,"family":"Albers","given":"Janice","email":"jalbers@usgs.gov","middleInitial":"L.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":864721,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pettit, Thomas W.","contributorId":239722,"corporation":false,"usgs":false,"family":"Pettit","given":"Thomas","email":"","middleInitial":"W.","affiliations":[{"id":47988,"text":"University of Maryland University College-Asia, Unit 5060","active":true,"usgs":false}],"preferred":false,"id":864722,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hooper, Michael J. 0000-0002-4161-8961 mhooper@usgs.gov","orcid":"https://orcid.org/0000-0002-4161-8961","contributorId":3251,"corporation":false,"usgs":true,"family":"Hooper","given":"Michael","email":"mhooper@usgs.gov","middleInitial":"J.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":864723,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70261212,"text":"70261212 - 2024 - Decrease in seismic velocity observed prior to the 2018 eruption of Kilauea volcano with ambient seismic noise interferometry","interactions":[],"lastModifiedDate":"2024-12-02T15:33:58.377781","indexId":"70261212","displayToPublicDate":"2019-04-16T00:00:00","publicationYear":"2024","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Decrease in seismic velocity observed prior to the 2018 eruption of Kilauea volcano with ambient seismic noise interferometry","docAbstract":"The 2018 Kilauea eruption was a complex event that included deformation and eruption at the summit and along the middle and lower East Rift Zones. We use ambient seismic noise interferometry to measure time-lapse changes in seismic velocity of the volcanic edifice prior to the 2018 Kilauea Lower East Rift Zone eruption. Our results show that seismic velocities increase in relation to gradual inflation between 1 March and 20 April. In the ten days prior to the May 3rd eruption, a rapid seismic velocity decrease occurs even though the summit is still undergoing inflation. We show that inter-eruptive inflation/deflation is correlated with surface deformation, while the velocity decrease prior to East Rift Zone eruption is likely due to accumulating damage induced by the pressure exerted by the magma reservoir on the surrounding edifice. The accumulating damage and subsequent decrease in bulk edifice strength likely facilitates the transport of magma from the summit reservoir to the Middle East Rift Zone.","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2018GL081609","usgsCitation":"Olivier, G., Brenguier, F., Carey, R.J., Okubo, P., and Donaldson, C., 2024, Decrease in seismic velocity observed prior to the 2018 eruption of Kilauea volcano with ambient seismic noise interferometry: Geophysical Research Letters, v. 46, no. 7, p. 3734-3744, https://doi.org/10.1029/2018GL081609.","productDescription":"11 p.","startPage":"3734","endPage":"3744","ipdsId":"IP-102999","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":467062,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2018gl081609","text":"Publisher Index Page"},{"id":464629,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea volcano","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -155.31292752524547,\n 19.45502623491619\n ],\n [\n -155.31292752524547,\n 19.39548460880674\n ],\n [\n -155.21913756133694,\n 19.39548460880674\n ],\n [\n -155.21913756133694,\n 19.45502623491619\n ],\n [\n -155.31292752524547,\n 19.45502623491619\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"46","issue":"7","noUsgsAuthors":false,"publicationDate":"2019-04-08","publicationStatus":"PW","contributors":{"authors":[{"text":"Olivier, Gerrit","contributorId":346798,"corporation":false,"usgs":false,"family":"Olivier","given":"Gerrit","email":"","affiliations":[{"id":82967,"text":"Institute of Mine Seismology","active":true,"usgs":false}],"preferred":false,"id":919916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brenguier, Florent","contributorId":346799,"corporation":false,"usgs":false,"family":"Brenguier","given":"Florent","email":"","affiliations":[{"id":82968,"text":"University of Grenoble","active":true,"usgs":false}],"preferred":false,"id":919917,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carey, Rebecca J.","contributorId":145530,"corporation":false,"usgs":false,"family":"Carey","given":"Rebecca","email":"","middleInitial":"J.","affiliations":[{"id":16141,"text":"University of Tasmania","active":true,"usgs":false}],"preferred":false,"id":919918,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Okubo, P. 0000-0002-0381-6051","orcid":"https://orcid.org/0000-0002-0381-6051","contributorId":49432,"corporation":false,"usgs":true,"family":"Okubo","given":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":919919,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Donaldson, C.","contributorId":346843,"corporation":false,"usgs":false,"family":"Donaldson","given":"C.","email":"","affiliations":[],"preferred":false,"id":919992,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70260156,"text":"70260156 - 2024 - Analysis of the Alaska Volcano Observatory’s response time to volcanic explosions-1989 to 2016","interactions":[],"lastModifiedDate":"2024-10-29T15:54:12.686457","indexId":"70260156","displayToPublicDate":"2018-06-19T10:47:40","publicationYear":"2024","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5232,"text":"Frontiers in Earth Science","onlineIssn":"2296-6463","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of the Alaska Volcano Observatory’s response time to volcanic explosions-1989 to 2016","docAbstract":"A major goal of volcano monitoring is the rapid identification of volcanic explosions and subsequent warning of associated hazards. Between 1988 and 2016 the Alaska Volcano Observatory (AVO) responded to at least 54 separate volcanic eruptions. During this period, AVO's monitoring program relied principally on seismic and satellite remote sensing data, supplemented with geodetic, gas, and visual observations to track volcanic unrest. In this study we focus on AVO's response time, or the time required for AVO to (1) identify seismic signals associated with large ash-producing volcanic explosions and (2) initiate public warnings. We restrict this analysis to volcanoes monitored by a local seismic network and explosive in character. We focus on the 1989–90 eruption of Redoubt Volcano (VEI 3), the 1992 eruption of Mount Spurr (VEI 4), the 1999 eruption of Shishaldin Volcano (VEI 3), the 2006 eruption of Augustine Volcano (VEI 3) and the 2016 eruption of Pavlof Volcano (VEI 2) as detailed records of the timing of formal warnings are preserved. These eruption sequences allow us to evaluate AVO's response time under a number of monitoring scenarios, including both expected (those with recognized precursory unrest) and surprise eruptions (those without identified precursory unrest) as well as individual and repetitive sequences of explosive events. Recorded response time ranges from ~1 to 86 min. The shorter response times (~1–13 min) were achieved during sequences of explosive events at Redoubt (1989–90), Spurr (1992) and Augustine (2006). The longer response times (31– 86 min) are recorded for unexpected or surprise explosions such as Spurr (August 18, 1992) and Pavlof (2016) and the only or first explosions in an eruptive sequence such as Shishaldin (1999) and Augustine (2006).
","language":"English","publisher":"Frontiers Media","doi":"10.3389/feart.2018.00072","usgsCitation":"Power, J., and Cameron, C.E., 2024, Analysis of the Alaska Volcano Observatory’s response time to volcanic explosions-1989 to 2016: Frontiers in Earth Science, v. 6, 72, 11 p., https://doi.org/10.3389/feart.2018.00072.","productDescription":"72, 11 p.","ipdsId":"IP-095235","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":467063,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3389/feart.2018.00072","text":"Publisher Index Page"},{"id":463349,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -141.19644639855917,\n 60.163701494427016\n ],\n [\n -141.4146933455769,\n 62.921338064731\n ],\n [\n -154.76413824908144,\n 62.73561750601888\n ],\n [\n -158.86626079490838,\n 57.73158331857164\n ],\n [\n -170.19280646841207,\n 54.16503628783249\n ],\n [\n -178,\n 52.50050801183875\n ],\n [\n -178,\n 52.429296373477115\n ],\n [\n -178,\n 50.51941329958498\n ],\n [\n -173.84383443644094,\n 50.656574087830876\n ],\n [\n -161.58328690877826,\n 53.442227709095874\n ],\n [\n -150.84605023440074,\n 57.26828297058938\n ],\n [\n -141.19644639855917,\n 60.163701494427016\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"6","noUsgsAuthors":false,"publicationDate":"2018-06-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Power, John 0000-0002-7233-4398","orcid":"https://orcid.org/0000-0002-7233-4398","contributorId":215240,"corporation":false,"usgs":true,"family":"Power","given":"John","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":917243,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cameron, Cheryl E. 0000-0001-6366-2130","orcid":"https://orcid.org/0000-0001-6366-2130","contributorId":194695,"corporation":false,"usgs":false,"family":"Cameron","given":"Cheryl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":917244,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70261302,"text":"70261302 - 2024 - Mapping the resistivity structure of Walker Ridge 313 in the Gulf of Mexico using the marine CSEM method","interactions":[],"lastModifiedDate":"2024-12-05T15:17:07.841811","indexId":"70261302","displayToPublicDate":"2017-12-01T00:00:00","publicationYear":"2024","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2682,"text":"Marine and Petroleum Geology","active":true,"publicationSubtype":{"id":10}},"title":"Mapping the resistivity structure of Walker Ridge 313 in the Gulf of Mexico using the marine CSEM method","docAbstract":"A marine controlled source electromagnetic (CSEM) campaign was carried out in the Gulf of Mexico to further develop marine electromagnetic techniques in order to aid the detection and mapping of gas hydrate deposits. Marine CSEM methods are used to obtain an electrical resistivity structure of the subsurface which can indicate the type of substance filling the pore space, such as gas hydrates which are more resistive. Results from the Walker Ridge 313 study (WR 313) are presented in this paper and compared with the Gulf of Mexico Gas Hydrate Joint Industry Project II (JIP2) logging while drilling (LWD) results and available seismic data. The hydrate, known to exist within sheeted sand deposits, is mapped as a resistive region in the two dimensional (2D) CSEM inversion models. This is consistent with the JIP2 LWD resistivity results. CSEM inversions that use seismic horizons provide more realistic results compared to the unconstrained inversions by providing sharp boundaries and architectural control on the location of the resistive and conductive regions in the CSEM model. The seismic horizons include: 1) the base of the gas hydrate stability zone (BGHSZ), 2) the top of salt, and 3) the top and bottom of a fine grained marine mud interval with near vertical hydrate filled fractures, to constrain the CSEM inversion model. The top of salt provides improved location for brines, water saturated salt, and resistive salt. Inversions of the CSEM data map the occurrence of a ‘halo’ of conductive brines above salt. The use of the BGHSZ as a constraint on the inversion helps distinguish between free gas and gas hydrate as well as gas hydrate and water saturated sediments.","language":"English","publisher":"Elsevier","doi":"10.1016/j.marpetgeo.2017.08.039","usgsCitation":"Weitemeyer, K., Constable, S., Shelander, D., and Haines, S.S., 2024, Mapping the resistivity structure of Walker Ridge 313 in the Gulf of Mexico using the marine CSEM method: Marine and Petroleum Geology, v. 88, p. 1013-1031, https://doi.org/10.1016/j.marpetgeo.2017.08.039.","productDescription":"19 p.","startPage":"1013","endPage":"1031","ipdsId":"IP-088265","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":467064,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.marpetgeo.2017.08.039","text":"Publisher Index Page"},{"id":464802,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana","city":"Houma","otherGeospatial":"Gulf of Mexico, Walker Ridge 313","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -91.65721574777587,\n 29.904859799956952\n ],\n [\n -91.65721574777587,\n 25.48122420526559\n ],\n [\n -88.62636230717828,\n 25.48122420526559\n ],\n [\n -88.62636230717828,\n 29.904859799956952\n ],\n [\n -91.65721574777587,\n 29.904859799956952\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"88","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Weitemeyer, Karen","contributorId":346936,"corporation":false,"usgs":false,"family":"Weitemeyer","given":"Karen","affiliations":[{"id":37955,"text":"University of Southampton","active":true,"usgs":false}],"preferred":false,"id":920301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Constable, Steven","contributorId":346937,"corporation":false,"usgs":false,"family":"Constable","given":"Steven","affiliations":[{"id":83021,"text":"Scripps Institute for Oceanography","active":true,"usgs":false}],"preferred":false,"id":920302,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shelander, Dianna","contributorId":346938,"corporation":false,"usgs":false,"family":"Shelander","given":"Dianna","affiliations":[{"id":27162,"text":"Schlumberger","active":true,"usgs":false}],"preferred":false,"id":920303,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Haines, Seth S. 0000-0003-2611-8165 shaines@usgs.gov","orcid":"https://orcid.org/0000-0003-2611-8165","contributorId":1344,"corporation":false,"usgs":true,"family":"Haines","given":"Seth","email":"shaines@usgs.gov","middleInitial":"S.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":920304,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70178411,"text":"70178411 - 2024 - Minerals Yearbook, volume III, Area Reports — International — Asia and the Pacific","interactions":[{"subject":{"id":70178411,"text":"70178411 - 2024 - Minerals Yearbook, volume III, Area Reports — International — Asia and the Pacific","indexId":"70178411","publicationYear":"2024","noYear":false,"displayTitle":"Minerals Yearbook, Volume III, Area Reports — International — Asia and the Pacific","title":"Minerals Yearbook, volume III, Area Reports — International — Asia and the Pacific"},"predicate":"IS_PART_OF","object":{"id":70048196,"text":"70048196 - 2024 - Minerals Yearbook, volume III, Area Reports — International","indexId":"70048196","publicationYear":"2024","noYear":false,"title":"Minerals Yearbook, volume III, Area Reports — International"},"id":1}],"isPartOf":{"id":70048196,"text":"70048196 - 2024 - Minerals Yearbook, volume III, Area Reports — International","indexId":"70048196","publicationYear":"2024","noYear":false,"title":"Minerals Yearbook, volume III, Area Reports — International"},"lastModifiedDate":"2024-01-08T20:22:20.216175","indexId":"70178411","displayToPublicDate":"2017-08-22T13:00:00","publicationYear":"2024","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":370,"text":"Minerals Yearbook","active":false,"publicationSubtype":{"id":6}},"displayTitle":"Minerals Yearbook, Volume III, Area Reports — International — Asia and the Pacific","title":"Minerals Yearbook, volume III, Area Reports — International — Asia and the Pacific","docAbstract":"The U.S. Geological Survey (USGS) Minerals Yearbook discusses the performance of the worldwide minerals and materials industries and provides background information to assist in interpreting that performance. Content of the individual Minerals Yearbook volumes follows:
The USGS continually strives to improve the value of its publications to users. Constructive comments and suggestions by readers of the Minerals Yearbook are welcomed.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70178411","collaboration":"National Minerals Information CenterDirector, National Minerals Information Center
U.S. Geological Survey
12201 Sunrise Valley Drive
988 National Center
Reston, VA 20192
Email: nmicrecordsmgt@usgs.gov
The U.S. Geological Survey (USGS) Minerals Yearbook discusses the performance of the worldwide minerals and materials industries and provides background information to assist in interpreting that performance. Content of the individual Minerals Yearbook volumes follows:
The USGS continually strives to improve the value of its publications to users. Constructive comments and suggestions by readers of the Minerals Yearbook are welcomed.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70178412","collaboration":"National Minerals Information CenterDirector, National Minerals Information Center
U.S. Geological Survey
12201 Sunrise Valley Drive
988 National Center
Reston, VA 20192
Email: nmicrecordsmgt@usgs.gov
The U.S. Geological Survey (USGS) Minerals Yearbook discusses the performance of the worldwide minerals and materials industries and provides background information to assist in interpreting that performance. Content of the individual Minerals Yearbook volumes follows:
The USGS continually strives to improve the value of its publications to users. Constructive comments and suggestions by readers of the Minerals Yearbook are welcomed.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70178419","collaboration":"National Minerals Information CenterDirector, National Minerals Information Center
U.S. Geological Survey
12201 Sunrise Valley Drive
988 National Center
Reston, VA 20192
Email: nmicrecordsmgt@usgs.gov
The U.S. Geological Survey (USGS) Minerals Yearbook discusses the performance of the worldwide minerals and materials industries and provides background information to assist in interpreting that performance. Content of the individual Minerals Yearbook volumes follows:
The USGS continually strives to improve the value of its publications to users. Constructive comments and suggestions by readers of the Minerals Yearbook are welcome.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70178240","issn":"0076–8952","collaboration":"National Minerals Information CenterDirector, National Minerals Information Center
U.S. Geological Survey
12201 Sunrise Valley Drive
988 National Center
Reston, VA 20192
(703) 648-4961
Email: nmicrecordsmgt@usgs.gov
The U.S. Geological Survey (USGS) Minerals Yearbook discusses the performance of the worldwide minerals and materials industries and provides background information to assist in interpreting that performance. Content of the individual Minerals Yearbook volumes follows:
The USGS continually strives to improve the value of its publications to users. Constructive comments and suggestions by readers of the Minerals Yearbook are welcome.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mybvI","collaboration":"National Minerals Information CenterDirector, National Minerals Information Center
U.S. Geological Survey
12201 Sunrise Valley Drive
988 National Center
Reston, VA 20192
Email: nmicrecordsmgt@usgs.gov
The U.S. Geological Survey (USGS) Minerals Yearbook discusses the performance of the worldwide minerals and materials industries and provides background information to assist in interpreting that performance. Content of the individual Minerals Yearbook volumes follows:
The USGS continually strives to improve the value of its publications to users. Constructive comments and suggestions by readers of the Minerals Yearbook are welcome.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mybvII","collaboration":"National Minerals Information CenterDirector, National Minerals Information Center
U.S. Geological Survey
12201 Sunrise Valley Drive
988 National Center
Reston, VA 20192
Email: nmicrecordsmgt@usgs.gov
The U.S. Geological Survey (USGS) Minerals Yearbook discusses the performance of the worldwide minerals and materials industries and provides background information to assist in interpreting that performance. Content of the individual Minerals Yearbook volumes follows:
The USGS continually strives to improve the value of its publications to users. Constructive comments and suggestions by readers of the Minerals Yearbook are welcome.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mybvIII","collaboration":"National Minerals Information CenterDirector, National Minerals Information Center
U.S. Geological Survey
12201 Sunrise Valley Drive
988 National Center
Reston, VA 20192
Email: nmicrecordsmgt@usgs.gov
The Federal Priority Streamgage (FPS) network of the U.S. Geological Survey (USGS), created in 1999 as the National Streamflow Information Program, receives Congressional appropriations to support the operation of a federally-funded “backbone” network of streamflow gages across the United States that are designated to meet the “Federal needs” or priorities of the country. Anticipating the evolution of Federal stakeholder water-data needs, the USGS launched a re-evaluation of the fundamental priorities for the FPS network in October 2020. In March 2022, the FPS Re-Prioritization Project used an online survey to solicit feedback from 767 stakeholders representing 22 Federal agencies who benefit from the FPS network. Additional feedback from survey respondents was obtained during online listening sessions to validate the USGS’s understanding of current Federal water-data needs. Results of the feedback show that the original five network priorities identified by the U.S. Geological Survey in 1999 are still valid but require modification to better incorporate additional needs, including Federal water operations, streamflow trends and extremes, water rights involving Federal lands, and streamflow data supporting ecosystem health. Federal stakeholder feedback also indicated that the inclusion of precipitation and water-temperature data collection, along with stream imagery, would enhance the value of the FPS network.
Results of the FPS Re-Prioritization Project and Open Season that ended in May 2024 revealed that the number of FPS locations meeting the updated eligibility criteria nearly tripled, which illustrates the value of the information provided by the FPS network. The Water Forecasting & Operations and the Water Quality network priorities contributed to the largest number of new eligible FPS sites, demonstrating the importance of the FPS network in supporting informed decisions related to the protection of life, property, the environment, and the economy of the United States.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20231032","usgsCitation":"Dillow, J.J.A., McCallum, B.E., and Angeroth, C.E., 2023, Re-prioritization of the U.S. Geological Survey Federal Priority Streamgage Network (ver. 1.1, April 2025): U.S. Geological Survey Open-File Report 2023–1032, 7 p., https://doi.org/10.3133/ofr20231032.","productDescription":"Report: iii, 7 p.; Data Release","numberOfPages":"7","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-146165","costCenters":[{"id":37786,"text":"WMA - Observing Systems Division","active":true,"usgs":true},{"id":41514,"text":"Maryland-Delaware-District of Columbia Water Science Center","active":true,"usgs":true}],"links":[{"id":484210,"rank":7,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/2023/1032/versionHist.txt","text":"Version History","size":"5 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Water Mission Area
U.S. Geological Survey
12201 Sunrise Valley Drive
Reston, Virginia 20192
Birds face strong selective pressures to complete individual nesting attempts as quickly as possible to minimize exposure of nests to predators and weather, maximize renesting potential, and maximize hatching success. As a result, the duration of developmental periods and of overall nest periods are often relatively constant within species. However, birds may sometimes be subject to acute energetic constraints that may preclude them from initiating incubation at the optimal time. We report an extraordinary case of delayed incubation by a female Burrowing Owl (Athene cunicularia) in Oregon, USA, which contrasted sharply with a large sample of nests monitored by motion-activated video cameras in western North America from 2015 to 2018. The focal female delayed incubation by 11 d following clutch completion and subsequently experienced near total hatching failure of her clutch. This observation corroborates previous experimental studies regarding the limits to egg viability and trade-offs between the timing of incubation onset and hatching success. These findings illustrate the acute trade-offs faced by nesting birds, and the cost of delayed incubation that we observed in this owl could help explain the cause of asynchronous hatching.
","language":"English","publisher":"Taylor & Francis","doi":"10.1676/22-00089","usgsCitation":"Lundblad, C., Conway, C.J., 2023, Delayed incubation leads to hatching failure of a Burrowing Owl (Athene cunicularia) nest: Wilson Journal of Ornithology, v. 135, no. 3, p. 400-405, https://doi.org/10.1676/22-00089.","productDescription":"6 p.","startPage":"400","endPage":"405","ipdsId":"IP-144129","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":500347,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Umatilla Army Depot","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.6494795743624,\n 46.43690242049303\n ],\n [\n -124.6494795743624,\n 41.96089422685421\n ],\n [\n -116.90302518029182,\n 41.96089422685421\n ],\n [\n -116.90302518029182,\n 46.43690242049303\n ],\n [\n -124.6494795743624,\n 46.43690242049303\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"135","issue":"3","noUsgsAuthors":false,"publicationDate":"2025-02-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Lundblad, Carl G.","contributorId":287176,"corporation":false,"usgs":false,"family":"Lundblad","given":"Carl G.","affiliations":[{"id":39599,"text":"ui","active":true,"usgs":false}],"preferred":false,"id":956320,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conway, Courtney J. 0000-0003-0492-2953 cconway@usgs.gov","orcid":"https://orcid.org/0000-0003-0492-2953","contributorId":2951,"corporation":false,"usgs":true,"family":"Conway","given":"Courtney","email":"cconway@usgs.gov","middleInitial":"J.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":956334,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70259557,"text":"70259557 - 2023 - Getting Started with MODFLFOW","interactions":[],"lastModifiedDate":"2024-10-15T11:38:40.244852","indexId":"70259557","displayToPublicDate":"2024-10-01T06:37:38","publicationYear":"2023","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":14,"text":"Instruction"},"title":"Getting Started with MODFLFOW","docAbstract":"Numerical modeling of groundwater flow systems was once accessible only to modeling specialists in the hydrogeological community. Software such as MODFLOW—the most frequently used groundwater modeling program in the world—and associated graphical user interfaces (GUIs) have made modeling possible for most groundwater scientists. This book provides the bridge from understanding to implementing models by introducing the basics of MODFLOW version 6 and providing readers who have a working knowledge of groundwater flow with a guide through construction of their first groundwater model.
","language":"English","publisher":"Groundwater Project","doi":"10.21083/978-1-77470-030-3","usgsCitation":"Winston, R.B., 2023, Getting Started with MODFLFOW, 243 p., https://doi.org/10.21083/978-1-77470-030-3.","productDescription":"243 p.","ipdsId":"IP-159533","costCenters":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"links":[{"id":462868,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Winston, Richard B. 0000-0002-6287-8834 rbwinst@usgs.gov","orcid":"https://orcid.org/0000-0002-6287-8834","contributorId":3567,"corporation":false,"usgs":true,"family":"Winston","given":"Richard","email":"rbwinst@usgs.gov","middleInitial":"B.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":915747,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70259931,"text":"70259931 - 2023 - The presence of silicate melt may enhance rates of cation diffusion in olivine","interactions":[],"lastModifiedDate":"2024-10-28T11:18:22.113863","indexId":"70259931","displayToPublicDate":"2024-09-27T06:17:16","publicationYear":"2023","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"The presence of silicate melt may enhance rates of cation diffusion in olivine","docAbstract":"The Arctic and its permafrost terrains are inherently dynamic, complex, and sensitive environments. Understanding the past and current changes occurring in these systems is key in predicting future variations, including the response of permafrost to climate change and to surface disturbances resulting from natural processes or anthropogenic activities. Here, we focus on advancing our understanding of the drivers controlling terrain vulnerability and resilience to thermal erosion gullying proximal to linear infrastructure in the lowlands of the Arctic Foothills (Alaska). This builds upon our previous work (Stephani et al. 2023) in the infrastructure corridor that includes the Dalton Highway and Trans Alaska Pipeline System (TAPS).
To identify locations affected by thermal erosion gullying and recognize changes in the ~80-km long corridor section that travels through the Arctic Foothills, we compared time series of high-resolution satellite imagery from 2001 to 2023. When we captured the timing of gullying onset and/or growth, we examined prevailing climatic conditions (Sagwon Station) prior to these terrain changes. We integrated our findings with our field-based data (e.g., drilling) described in Stephani et al. (2023).
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"12th International conference on permafrost proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"International Permafrost Association","usgsCitation":"Stephani, E.A., Darrow, M., and Kanevskiy, M., 2023, Vulnerability and resilience of ice-rich permafrost to thermal erosion gullying in the Arctic Foothills infrastructure corridor, Alaska, in 12th International conference on permafrost proceedings, v. 2, p. 533-534.","productDescription":"2 p.","startPage":"533","endPage":"534","ipdsId":"IP-160342","costCenters":[{"id":65299,"text":"Alaska Science Center Ecosystems","active":true,"usgs":true}],"links":[{"id":501314,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Foothills","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stephani, Eva Anne 0000-0002-7006-4742","orcid":"https://orcid.org/0000-0002-7006-4742","contributorId":332297,"corporation":false,"usgs":true,"family":"Stephani","given":"Eva","email":"","middleInitial":"Anne","affiliations":[{"id":65299,"text":"Alaska Science Center Ecosystems","active":true,"usgs":true}],"preferred":true,"id":889940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Darrow, M.M.","contributorId":63286,"corporation":false,"usgs":true,"family":"Darrow","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":957158,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kanevskiy, Mikhail","contributorId":169366,"corporation":false,"usgs":false,"family":"Kanevskiy","given":"Mikhail","email":"","affiliations":[{"id":7211,"text":"University of Alaska, Fairbanks","active":true,"usgs":false}],"preferred":false,"id":957159,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70265004,"text":"70265004 - 2023 - A review of the ecology and conservation biology of Sali (Micronesian Starling, Aplonis opaca guami) on Guam","interactions":[],"lastModifiedDate":"2025-03-27T15:10:52.983128","indexId":"70265004","displayToPublicDate":"2024-05-25T10:07:52","publicationYear":"2023","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2734,"text":"Micronesica","active":true,"publicationSubtype":{"id":10}},"displayTitle":"A review of the ecology and conservation biology of Såli (Micronesian Starling, Aplonis opaca guami) on Guam","title":"A review of the ecology and conservation biology of Sali (Micronesian Starling, Aplonis opaca guami) on Guam","docAbstract":"The accidental introduction of the Brown Treesnake (BTS, Boiga irregularis) to Guam following World War II led to the extinction, extirpation, or severe decline of most of Guam’s native avifauna. One forest bird species that managed to persist is the cavity-nesting Såli (Micronesian Starling, Aplonis opaca guami), a once-ubiquitous native omnivore whose current Guam distribution is restricted primarily to urbanized areas in the northern half of the island, with a second much smaller population on Cocos Island off southern Guam. Såli on Guam breed year-round and are habitat generalists with large home ranges. Besides arthropods and small vertebrates, they consume fruit from a wide range of native and introduced plant species and are key seed dispersers within the local ecosystem. Såli on Guam suffer extremely high post-fledging mortality due to predation by BTS and cats, leading to a population age structure strongly skewed towards adult birds. Other threats include habitat loss and degradation, extreme weather events, and sea level rise. Key management activities aimed at restoring this species include predator control, while non-native ungulate removal and vegetation management may be undertaken to support broader ecological recovery. This species account on Såli provides a review of the literature on this species, synthesizing information on habitat use, life history, and demographics to provide a biological foundation for future recovery efforts.
","language":"English","publisher":"University of Guam","usgsCitation":"Nguyen, A., Kastner, M., Wiles, G., Wagner, C., Pollock, H., Rogers, H., Duenas, L., Fricke, E., Rehm, E., McElderry, R., Siers, S.R., and Paxton, E.H., 2023, A review of the ecology and conservation biology of Sali (Micronesian Starling, Aplonis opaca guami) on Guam: Micronesica, v. 2023, no. 04, p. 1-18.","productDescription":"18 p.","startPage":"1","endPage":"18","ipdsId":"IP-138691","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":483929,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"http://micronesica.org/volumes/2023"},{"id":483945,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Guam","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 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Technology","active":true,"usgs":false}],"preferred":false,"id":932226,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Rehm, Evan M.","contributorId":352858,"corporation":false,"usgs":false,"family":"Rehm","given":"Evan M.","affiliations":[{"id":37389,"text":"U.S. Forest Service","active":true,"usgs":false}],"preferred":false,"id":932227,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"McElderry, Robert M.","contributorId":352860,"corporation":false,"usgs":false,"family":"McElderry","given":"Robert M.","affiliations":[{"id":54632,"text":"Research Corporation of the University of Guam","active":true,"usgs":false}],"preferred":false,"id":932228,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Siers, Shane R.","contributorId":152305,"corporation":false,"usgs":false,"family":"Siers","given":"Shane","email":"","middleInitial":"R.","affiliations":[{"id":6621,"text":"Colorado State University","active":true,"usgs":false}],"preferred":false,"id":932229,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Paxton, Eben H. 0000-0001-5578-7689","orcid":"https://orcid.org/0000-0001-5578-7689","contributorId":19640,"corporation":false,"usgs":true,"family":"Paxton","given":"Eben","email":"","middleInitial":"H.","affiliations":[{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true}],"preferred":true,"id":932230,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}} ,{"id":70253912,"text":"70253912 - 2023 - Forest bird populations at the Big Island National Wildlife Refuge Complex, Hawai'i","interactions":[],"lastModifiedDate":"2024-06-03T15:05:06.821876","indexId":"70253912","displayToPublicDate":"2024-04-11T09:18:57","publicationYear":"2023","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2287,"text":"Journal of Fish and Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Forest bird populations at the Big Island National Wildlife Refuge Complex, Hawai'i","docAbstract":"Endemic Hawaiian forest birds have experienced dramatic population declines. The Big Island National Wildlife Refuge Complex (Refuge Complex) was established for the conservation of endangered forest birds and their habitats. Surveys have been conducted at two units of the Refuge Complex to monitor forest bird populations and their response to management actions. We analyzed survey data from 1987 to 2019 at the Hakalau Forest Unit (HFU) and from 1995 to 2019 at the Kona Forest Unit (KFU). We analyzed three strata at HFU: open-forest, closed-forest, and afforested-pasture, and two strata at KFU: upper (>1,524 m elevation) and lower (<1,524 m). In all years, ‘i‘iwi Vestiaria coccinea, ‘apapane Himatione sanguinea, and Hawai'i ‘amakihi Chlorodrepanis virens virens were the most abundant species at HFU. Three endangered forest bird species, Hawai'i ‘ākepa Loxops coccineus, ‘alawī Loxops mana (also known as Hawai'i creeper) and ‘akiapōlā‘au Hemignathus wilsoni, had much lower densities. The most abundant species at KFU was ‘apapane, followed by Hawai'i ‘amakihi at much lower densities. We found a continuation of several trends observed in previous analyses at HFU up to 2012, with most species’ trends upward in afforested-pasture stratum, stable in the open-forest stratum, and downward in the closed-forest stratum. However, more species were showing downward trends in all three strata during the most recent decade. Results were mixed at KFU, with most species’ trends downward in the upper stratum and upward in the lower stratum. Populations of endangered species were either locally extirpated at KFU or in numbers too low to reliably estimate population abundance. The Refuge Complex is important for conservation of forest birds on Hawai'i Island. Our results show that HFU supports the majority of three endangered forest bird species. Threats to forest birds at the Refuge Complex appear to be having a negative impact. These threats include habitat loss, disease, feral ungulates, and nonnative predators. Continuing and enhancing management actions, such as forest restoration and removal of invasive species, could help mitigate these impacts and allow the Refuge Complex to remain a key site for forest bird conservation in Hawai'i.
","language":"English","publisher":"U.S. Fish and Wildlife Service","doi":"10.3996/JFWM-22-035","usgsCitation":"Kendall, S.J., Rounds, R.A., Camp, R.J., Genz, A., Cady, T., and Ball, D.L., 2023, Forest bird populations at the Big Island National Wildlife Refuge Complex, Hawai'i: Journal of Fish and Wildlife Management, v. 14, no. 2, p. 410-432, https://doi.org/10.3996/JFWM-22-035.","productDescription":"23 p.","startPage":"410","endPage":"432","ipdsId":"IP-145154","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":441323,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3996/jfwm-22-035","text":"Publisher Index Page"},{"id":428355,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Big Island National Wildlife Refuge Complex","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -155.21286438985624,\n 19.964079437115203\n ],\n [\n -155.35557208018355,\n 19.964079437115203\n ],\n [\n -155.35557208018355,\n 19.75471981087044\n ],\n [\n -155.21286438985624,\n 19.75471981087044\n ],\n [\n -155.21286438985624,\n 19.964079437115203\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -155.78367183276112,\n 19.326994002143053\n ],\n [\n -155.8768682174414,\n 19.326994002143053\n ],\n [\n -155.8768682174414,\n 19.257171984885417\n ],\n [\n -155.78367183276112,\n 19.257171984885417\n ],\n [\n -155.78367183276112,\n 19.326994002143053\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"14","issue":"2","noUsgsAuthors":false,"publicationDate":"2024-04-11","publicationStatus":"PW","contributors":{"authors":[{"text":"Kendall, Steven J.","contributorId":30911,"corporation":false,"usgs":false,"family":"Kendall","given":"Steven","email":"","middleInitial":"J.","affiliations":[{"id":6987,"text":"U.S. Fish and Wildlife Sevice","active":true,"usgs":false}],"preferred":false,"id":900081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rounds, Rachel A.","contributorId":290249,"corporation":false,"usgs":false,"family":"Rounds","given":"Rachel","email":"","middleInitial":"A.","affiliations":[{"id":62393,"text":"U.S. Fish and Wildlife Service, Pacific Islands Refuges and Monuments Office","active":true,"usgs":false}],"preferred":false,"id":900082,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Camp, Richard J. 0000-0001-7008-923X rick_camp@usgs.gov","orcid":"https://orcid.org/0000-0001-7008-923X","contributorId":189964,"corporation":false,"usgs":true,"family":"Camp","given":"Richard","email":"rick_camp@usgs.gov","middleInitial":"J.","affiliations":[{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true},{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"preferred":true,"id":900083,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Genz, Ayesha 0000-0002-2916-1436","orcid":"https://orcid.org/0000-0002-2916-1436","contributorId":196671,"corporation":false,"usgs":false,"family":"Genz","given":"Ayesha","email":"","affiliations":[],"preferred":false,"id":900084,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cady, Thomas","contributorId":336165,"corporation":false,"usgs":false,"family":"Cady","given":"Thomas","email":"","affiliations":[{"id":36188,"text":"U.S. Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":900085,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ball, Donna L.","contributorId":206227,"corporation":false,"usgs":false,"family":"Ball","given":"Donna","email":"","middleInitial":"L.","affiliations":[{"id":6654,"text":"USFWS","active":true,"usgs":false}],"preferred":false,"id":900086,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70252091,"text":"sir20235144 - 2023 - A comparison of water-quality and stormwater inflow and outflow during habitat restoration at the McEwen storm drainage pond, South Valley, Albuquerque, New Mexico, 2020–22","interactions":[],"lastModifiedDate":"2026-01-30T19:58:02.980208","indexId":"sir20235144","displayToPublicDate":"2024-03-15T07:34:31","publicationYear":"2023","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":"2023-5144","displayTitle":"A Comparison of Water-Quality and Stormwater Inflow and Outflow During Habitat Restoration at the McEwen Storm Drainage Pond, South Valley, Albuquerque, New Mexico, 2020–22","title":"A comparison of water-quality and stormwater inflow and outflow during habitat restoration at the McEwen storm drainage pond, South Valley, Albuquerque, New Mexico, 2020–22","docAbstract":"In 2020, the U.S. Geological Survey began targeted monitoring, in partnership with Bernalillo County, at three locations within the McEwen storm drainage pond to evaluate and compare the water quality of stormwater as it enters and exits the study area, which is channelized and routes urban stormwater runoff through a wetland area. Stage in McEwen pond and precipitation at a nearby precipitation gage were evaluated to observe relations between rainfall and stage, as well as how long the stage remained elevated at the site. Peak stage ranged from 0.73 to 2.4 feet, with the time to reach peak stage at McEwen pond ranging from 45 minutes to 10 hours and 45 minutes. The stage remained elevated for a median of 3 days. Monitored water-quality parameters included physical parameters, bacteria, sediment, and nutrients. Bacteria was the only parameter that frequently exceeded the New Mexico Water Quality standard. Significant differences (p less than 0.05) among sites were few, consisting of those for total nitrogen and dissolved ammonia concentrations, which decreased toward the middle of the pond and were lower in the outflow from the pond compared to concentrations at the east and west sites. The middle of McEwen pond showed an increase in the percentage of fine-grained sediment, which suggests that larger particles settled into the pond and were further filtered as water traveled through the swales. Concentrations of suspended sediment and dissolved nutrients were significantly lower in 2022 compared to previous years. Although the site is still undergoing restoration and plants are becoming established, observations over the last several years indicate that site restoration has resulted in changes to the study area through processes such as nutrient uptake and the filtering of larger sediment particles.
Director, New Mexico Water Science Center
U.S. Geological Survey
6700 Edith Blvd. NE
Albuquerque, NM 87113
Contact Us- USGS Publications Warehouse
","tableOfContents":"In response to previous reports of per- and polyfluoroalkyl substances (PFAS) contamination in French Island’s (located in the Mississippi River within the town of Campbell, Wisconsin) primary source of drinking water, 11 locations were sampled by the U.S. Geological Survey (USGS) in October 2021 to assess the potential presence of contaminant mixtures, including PFAS, in tapwater. Three locations were assessed seven times each over the course of three days. These samples were chosen to evaluate the water quality of the deeper Mount Simon bedrock aquifer and the water quality of the shallower sand and gravel (alluvial) aquifer at two locations. The other eight sample locations were spatially distributed within Campbell and were sampled once each. For each of these 11 sites, tapwater samples were analyzed for disinfection byproducts (DBP), pesticides, PFAS, pharmaceuticals, semi-volatile organic compounds (SVOC), volatile organic compounds (VOC), cations, anions, trace elements, alkalinity, microbial indicators, as well as measurements of water temperature, specific conductance, and pH. Of the 506 organic compounds analyzed in each water-quality sample, 74 (14 percent) were detected at least one time in any of the samples collected. Of the 14 percent, detected analytes included 27 pesticides (5 percent), 14 PFAS (3 percent), 6 pharmaceuticals (1 percent), 7 SVOC (1 percent), and 20 VOC (4 percent). No DBP were detected. The total number of organic compounds detected per sample ranged from 0–20 (median of 10), with the sum of concentrations ranging from not detected (nd)–2.53 micrograms per liter (μg/L; median of 0.333 μg/L). Of the inorganic constituents measured, eight were not detected above their reporting limit in any of the samples. The inorganic constituents that were not detected were antimony, arsenic, beryllium, cadmium, cobalt, molybdenum, selenium, and vanadium.
Along with the 11 sites sampled throughout Campbell, Wisconsin, beginning in October 2021, four more wells were sampled on the Upper Midwest Environmental Sciences Center (UMESC) campus for PFAS. Three of these sites withdraw water from the shallow alluvial aquifer (the same source water for tapwater site 002) and one from the Mount Simon aquifer (the same source of water for tapwater site 001). This sampling is ongoing with results from samples through December 2022 summarized in this report. Of the 33 PFAS analyzed in samples from the four UMESC locations, 15 individual PFAS were detected at least one time in any of the samples analyzed with the sum of PFAS concentrations ranging from nd–1.49 μg/L (median of 0.309 μg/L).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20231088","collaboration":"Prepared in cooperation with the Town of Campbell, Wisconsin","programNote":"Environmental Health Program","usgsCitation":"Romanok, K.M., Meppelink, S.M., Bradley, P.M., Breitmeyer, S.E., Donahue, L., Gaikowski, M.P., Hines, R.K., and Smalling, K.L., 2023, Occurrence of mixed organic and inorganic chemicals in groundwater and tapwater, town of Campbell, Wisconsin, 2021–22: U.S. Geological Survey Open-File Report 2023–1088, 29 p., https://doi.org/10.3133/ofr20231088.","productDescription":"Report: viii, 29 p.; 2 Data Releases","numberOfPages":"29","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-150739","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true},{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true},{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"links":[{"id":499196,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_115939.htm","linkFileType":{"id":5,"text":"html"}},{"id":423893,"rank":7,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9J6XKVS","text":"USGS data release","linkHelpText":"Quarterly sample results for perand polyfluoroalkyl substances (PFAS) for locations in Campbell, Wisconsin, 2021–22"},{"id":423892,"rank":6,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9EUBGUF","text":"USGS data release","linkHelpText":"Target-chemical concentrations for assessment of mixed-organic/inorganic chemical and biological exposures in private-well tapwater at Campbell, Wisconsin, 2021"},{"id":423887,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2023/1088/coverthb.jpg"},{"id":423888,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2023/1088/ofr20231088.pdf","text":"Report","size":"1.62 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2023-1088"},{"id":423889,"rank":3,"type":{"id":39,"text":"HTML Document"},"url":"https://pubs.usgs.gov/publication/ofr20231088/full","text":"Report","linkFileType":{"id":5,"text":"html"},"description":"OFR 2023-1088"},{"id":423890,"rank":4,"type":{"id":31,"text":"Publication XML"},"url":"https://pubs.usgs.gov/of/2023/1088/ofr20231088.XML"},{"id":423891,"rank":5,"type":{"id":34,"text":"Image Folder"},"url":"https://pubs.usgs.gov/of/2023/1088/images/"}],"country":"United States","state":"Wisconsin","county":"La Crosse County","city":"Campbell","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -91.29371444024203,\n 43.904997377408506\n ],\n [\n -91.29371444024203,\n 43.84807720086516\n ],\n [\n -91.23878279961701,\n 43.84807720086516\n ],\n [\n -91.23878279961701,\n 43.904997377408506\n ],\n [\n -91.29371444024203,\n 43.904997377408506\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","contact":"Director, New Jersey Water Science Center
3450 Princeton Pike, Suite 110
Lawrenceville, New Jersey 08648