{"pageNumber":"1867","pageRowStart":"46650","pageSize":"25","recordCount":184982,"records":[{"id":70041792,"text":"70041792 - 2010 - Introduction to special section on phenomenology, underlying processes, and hazard implications of aseismic slip and nonvolcanic tremor","interactions":[],"lastModifiedDate":"2019-07-17T16:30:24","indexId":"70041792","displayToPublicDate":"2012-12-14T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Introduction to special section on phenomenology, underlying processes, and hazard implications of aseismic slip and nonvolcanic tremor","docAbstract":"This paper introduces the special section on the \"phenomenology, underlying processes, and hazard implications of aseismic slip and nonvolcanic tremor\" by highlighting key results of the studies published in it. Many of the results indicate that seismic and aseismic manifestations of slow slip reflect transient shear displacements on the plate interface, with the outstanding exception of northern Cascadia where tremor sources have been located on and above the plate interface (differing models of the plate interface there also need to be reconciled). Slow slip phenomena appear to result from propagating deformation that may develop with persistent gaps and segment boundaries. Results add to evidence that when tectonic deformation is relaxed via slow slip, most relaxation occurs aseismically but with seismic signals providing higher-resolution proxies for the aseismic slip. Instead of two distinct slip modes as suggested previously, lines between \"fast\" and \"slow\" slip more appropriately may be described as blurry zones. Results reported also show that slow slip sources do not coincide with a specific temperature or metamorphic reaction. Their associations with zones of high conductivity and low shear to compressional wave velocity ratios corroborate source models involving pore fluid pressure buildup and release. These models and spatial anticorrelations between earthquake and tremor activity also corroborate a linkage between slow slip and frictional properties transitional between steady state and stick-slip. Finally, this special section highlights the benefits of global and multidisciplinary studies, which demonstrate that slow phenomena are not confined to beneath the locked zone but exist in many settings.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","publisherLocation":"Washington, D.C.","doi":"10.1029/2010JB008052","usgsCitation":"Gomberg, J., 2010, Introduction to special section on phenomenology, underlying processes, and hazard implications of aseismic slip and nonvolcanic tremor: Journal of Geophysical Research, v. 115, 6 p.; B00A00, https://doi.org/10.1029/2010JB008052.","productDescription":"6 p.; B00A00","numberOfPages":"6","ipdsId":"IP-025538","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":475479,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2010jb008052","text":"Publisher Index Page"},{"id":264107,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":264105,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2010JB008052"}],"country":"United States","volume":"115","noUsgsAuthors":false,"publicationDate":"2010-12-18","publicationStatus":"PW","scienceBaseUri":"50d20c51e4b08b071e771b86","contributors":{"authors":[{"text":"Gomberg, Joan","contributorId":77919,"corporation":false,"usgs":true,"family":"Gomberg","given":"Joan","affiliations":[],"preferred":false,"id":470218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042288,"text":"70042288 - 2010 - Aftershocks are well aligned with the background stress field, contradicting the hypothesis of highly-heterogeneous crustal stress","interactions":[],"lastModifiedDate":"2013-03-14T12:38:43","indexId":"70042288","displayToPublicDate":"2012-12-13T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Aftershocks are well aligned with the background stress field, contradicting the hypothesis of highly-heterogeneous crustal stress","docAbstract":"It has been proposed that the crustal stress field contains small-length-scale heterogeneity of much larger amplitude than the uniform background stress. This model predicts that earthquake focal mechanisms should reflect the loading stress rather than the uniform background stress. So, if the heterogeneous stress hypothesis is correct, focal mechanisms before and after a large earthquake should align with the tectonic loading and the earthquake-induced static stress perturbation, respectively. However, I show that the off-fault triggered aftershocks of the 1992 M7.3 Landers, California, earthquake align with the same stress field as the pre-Landers mechanisms. The aftershocks occurred on faults that were well oriented for failure in the pre-Landers stress field and then loaded by the Landers-induced static stress change. Aftershocks in regions experiencing a 0.05 to 5 MPa coseismic differential stress change align with the modeled Landers-induced static stress change, implying that they were triggered by the stress perturbation. Contrary to the heterogeneous stress hypothesis, these triggered aftershocks are also well aligned with the pre-Landers stress field obtained from inverting the pre-Landers focal mechanisms. Therefore, the inverted pre-Landers stress must represent the persistent background stress field. Earthquake focal mechanisms provide an unbiased sample of the spatially coherent background stress field, which is large relative to any small-scale stress heterogeneity. The counterexample provided by the Landers earthquake is strong evidence that the heterogeneous stress model is not widely applicable.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","publisherLocation":"Hoboken, NJ","doi":"10.1029/2010JB007586","usgsCitation":"Hardebeck, J.L., 2010, Aftershocks are well aligned with the background stress field, contradicting the hypothesis of highly-heterogeneous crustal stress: Journal of Geophysical Research B: Solid Earth, v. 115, no. B12, B12308: 10 p., https://doi.org/10.1029/2010JB007586.","productDescription":"B12308: 10 p.","ipdsId":"IP-020681","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":265032,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265031,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2010JB007586"}],"country":"United States","state":"California","city":"Landers","otherGeospatial":"Joshua Tree;Big Bear;San Andreas Fault","volume":"115","issue":"B12","noUsgsAuthors":false,"publicationDate":"2010-12-03","publicationStatus":"PW","scienceBaseUri":"50e5cfdee4b0a4aa5bb0ae6c","contributors":{"authors":[{"text":"Hardebeck, Jeanne L. 0000-0002-6737-7780 jhardebeck@usgs.gov","orcid":"https://orcid.org/0000-0002-6737-7780","contributorId":841,"corporation":false,"usgs":true,"family":"Hardebeck","given":"Jeanne","email":"jhardebeck@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"preferred":true,"id":471215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70041690,"text":"70041690 - 2010 - Effects of soil aggregates on debris-flow mobilization: Results from ring-shear experiments","interactions":[],"lastModifiedDate":"2012-12-11T11:07:00","indexId":"70041690","displayToPublicDate":"2012-12-11T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1517,"text":"Engineering Geology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of soil aggregates on debris-flow mobilization: Results from ring-shear experiments","docAbstract":"Rates and styles of landslide motion are sensitive to pore-water pressure changes caused by changes in soil porosity accompanying shear deformation. Soil may either contract or dilate upon shearing, depending upon whether its initial porosity is greater or less, respectively, than a critical-state porosity attained after sufficiently high strain. We observed complications in this behavior, however, during rate-controlled (0.02 m s<sup>−1</sup>) ring-shear experiments conducted on naturally aggregated dense loamy sand at low confining stresses (10.6 and 40 kPa). The aggregated soil first dilated and then contracted to porosities less than initial values, whereas the same soil with its aggregates destroyed monotonically dilated. We infer that aggregates persisted initially during shear and caused dilation before their eventual breakdown enabled net contraction. An implication of this contraction, demonstrated in experiments in which initial soil porosity was varied, is that the value of porosity distinguishing initially contractive from dilative behavior can be significantly larger than the critical-state porosity, which develops only after disaggregation ceases at high strains. In addition, post-dilative contraction may produce excess pore pressures, thereby reducing frictional strength and facilitating debris-flow mobilization. We infer that results of triaxial tests, which generally produce strains at least a factor of ∼ 4 smaller than those we observed at the inception of post-dilative contraction, do not allow soil contraction to be ruled out as a mechanism for debris-flow mobilization in dense soils containing aggregates.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Engineering Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.enggeo.2010.04.006","usgsCitation":"Iverson, N., Mann, J.E., and Iverson, R.M., 2010, Effects of soil aggregates on debris-flow mobilization: Results from ring-shear experiments: Engineering Geology, v. 114, no. 1-2, p. 84-92, https://doi.org/10.1016/j.enggeo.2010.04.006.","productDescription":"9 p.","startPage":"84","endPage":"92","ipdsId":"IP-020481","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":475480,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://lib.dr.iastate.edu/ge_at_pubs/268","text":"External Repository"},{"id":263923,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":263922,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.enggeo.2010.04.006"}],"volume":"114","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50c85608e4b03bc63bd6799a","contributors":{"authors":[{"text":"Iverson, Neal R.","contributorId":91380,"corporation":false,"usgs":true,"family":"Iverson","given":"Neal R.","affiliations":[],"preferred":false,"id":470095,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mann, Janet E.","contributorId":39664,"corporation":false,"usgs":true,"family":"Mann","given":"Janet","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":470094,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":470093,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70041334,"text":"70041334 - 2010 - Infrasonic harmonic tremor and degassing bursts from Halema'uma'u Crater, Kilauea Volcano, Hawaii","interactions":[],"lastModifiedDate":"2012-12-14T13:42:37","indexId":"70041334","displayToPublicDate":"2012-12-10T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Infrasonic harmonic tremor and degassing bursts from Halema'uma'u Crater, Kilauea Volcano, Hawaii","docAbstract":"The formation, evolution, collapse, and subsequent resurrection of a vent within Halema'uma'u Crater, Kilauea Volcano, produced energetic and varied degassing signals recorded by a nearby infrasound array between 2008 and early 2009. After 25 years of quiescence, a vent-clearing explosive burst on 19 March 2008 produced a clear, complex acoustic signal. Near-continuous harmonic infrasonic tremor followed this burst until 4 December 2008, when a period of decreased degassing occurred. The tremor spectra suggest volume oscillation and reverberation of a shallow gas-filled cavity beneath the vent. The dominant tremor peak can be sustained through Helmholtz oscillations of the cavity, while the secondary tremor peak and overtones are interpreted assuming acoustic resonance. The dominant tremor frequency matches the oscillation frequency of the gas emanating from the vent observed by video. Tremor spectra and power are also correlated with cavity geometry and dynamics, with the cavity depth estimated at ~219 m and volume ~3 x 10<sup>6</sup> m<sup>3</sup> in November 2008. Over 21 varied degassing bursts were observed with extended burst durations and frequency content consistent with a transient release of gas exciting the cavity into resonance. Correlation of infrasound with seismicity suggests an open system connecting the atmosphere to the seismic excitation process at depth. Numerous degassing bursts produced very long period (0.03-0.1 Hz) infrasound, the first recorded at Kilauea, indicative of long-duration atmospheric accelerations. Kilauea infrasound appears controlled by the exsolution of gas from the magma, and the interaction of this gas with the conduits and cavities confining it.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","publisherLocation":"Washington, D.C.","doi":"10.1029/2010JB007642","usgsCitation":"Fee, D., Garces, M., Patrick, M., Chouet, B., Dawson, P., and Swanson, D., 2010, Infrasonic harmonic tremor and degassing bursts from Halema'uma'u Crater, Kilauea Volcano, Hawaii: Journal of Geophysical Research, v. 115, 15 p.; B11316, https://doi.org/10.1029/2010JB007642.","productDescription":"15 p.; B11316","numberOfPages":"15","ipdsId":"IP-023579","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":336,"text":"Hawaiian Volcano Observatory","active":false,"usgs":true}],"links":[{"id":264051,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":264050,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2010JB007642"}],"country":"United States","state":"Hawai'i","otherGeospatial":"Kilauea Volcano","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155.3,19.3 ], [ -155.3,19.5 ], [ -155.0,19.5 ], [ -155.0,19.3 ], [ -155.3,19.3 ] ] ] } } ] }","volume":"115","noUsgsAuthors":false,"publicationDate":"2010-11-30","publicationStatus":"PW","scienceBaseUri":"50cc58f4e4b00ab7c548c6b4","contributors":{"authors":[{"text":"Fee, David","contributorId":77761,"corporation":false,"usgs":true,"family":"Fee","given":"David","affiliations":[],"preferred":false,"id":469551,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garces, Milton","contributorId":101166,"corporation":false,"usgs":true,"family":"Garces","given":"Milton","email":"","affiliations":[],"preferred":false,"id":469552,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patrick, Matt","contributorId":69033,"corporation":false,"usgs":true,"family":"Patrick","given":"Matt","email":"","affiliations":[],"preferred":false,"id":469550,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chouet, Bernard","contributorId":65485,"corporation":false,"usgs":true,"family":"Chouet","given":"Bernard","affiliations":[],"preferred":false,"id":469549,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dawson, Phil","contributorId":18647,"corporation":false,"usgs":true,"family":"Dawson","given":"Phil","email":"","affiliations":[],"preferred":false,"id":469548,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Swanson, Donald A. 0000-0002-1680-3591 donswan@usgs.gov","orcid":"https://orcid.org/0000-0002-1680-3591","contributorId":3137,"corporation":false,"usgs":true,"family":"Swanson","given":"Donald A.","email":"donswan@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":469547,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70041794,"text":"70041794 - 2010 - Inelastic off-fault response and three-dimensional dynamics of earthquake rupture on a strike-slip fault","interactions":[],"lastModifiedDate":"2013-03-14T12:34:29","indexId":"70041794","displayToPublicDate":"2012-12-10T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Inelastic off-fault response and three-dimensional dynamics of earthquake rupture on a strike-slip fault","docAbstract":"Large dynamic stress off the fault incurs an inelastic response and energy loss, which contributes to the fracture energy, limiting the rupture and slip velocity. Using an explicit finite element method, we model three-dimensional dynamic ruptures on a vertical strike-slip fault in a homogeneous half-space. The material is subjected to a pressure-dependent Drucker-Prager yield criterion. Initial stresses in the medium increase linearly with depth. Our simulations show that the inelastic response is confined narrowly to the fault at depth. There the inelastic strain is induced by large dynamic stresses associated with the rupture front that overcome the effect of the high confining pressure. The inelastic zone increases in size as it nears the surface. For material with low cohesion (~5 MPa) the inelastic zone broadens dramatically near the surface, forming a \"flowerlike\" structure. The near-surface inelastic strain occurs in both the extensional and the compressional regimes of the fault, induced by seismic waves ahead of the rupture front under a low confining pressure. When cohesion is large (~10 MPa), the inelastic strain is significantly reduced near the surface and confined mostly to depth. Cohesion, however, affects the inelastic zone at depth less significantly. The induced shear microcracks show diverse orientations near the surface, owing to the low confining pressure, but exhibit mostly horizontal slip at depth. The inferred rupture-induced anisotropy at depth has the fast wave direction along the direction of the maximum compressive stress.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","publisherLocation":"Washington, D.C.","doi":"10.1029/2009JB006382","usgsCitation":"Andrews, D., and Ma, S., 2010, Inelastic off-fault response and three-dimensional dynamics of earthquake rupture on a strike-slip fault: Journal of Geophysical Research B: Solid Earth, v. 115, no. B4, https://doi.org/10.1029/2009JB006382.","productDescription":"16 p.","startPage":"B04304","numberOfPages":"16","ipdsId":"IP-012923","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":475481,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2009jb006382","text":"Publisher Index Page"},{"id":264056,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269316,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2009JB006382"}],"country":"United States","volume":"115","issue":"B4","noUsgsAuthors":false,"publicationDate":"2010-04-08","publicationStatus":"PW","scienceBaseUri":"50cc58f0e4b00ab7c548c6b0","contributors":{"authors":[{"text":"Andrews, D.J.","contributorId":7416,"corporation":false,"usgs":true,"family":"Andrews","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":470219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ma, Shuo","contributorId":67373,"corporation":false,"usgs":true,"family":"Ma","given":"Shuo","affiliations":[],"preferred":false,"id":470220,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70041916,"text":"70041916 - 2010 - Fault zone structure from topography: signatures of en echelon fault slip at Mustang Ridge on the San Andreas Fault, Monterey County, California","interactions":[],"lastModifiedDate":"2012-12-31T12:26:42","indexId":"70041916","displayToPublicDate":"2012-12-10T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"Fault zone structure from topography: signatures of en echelon fault slip at Mustang Ridge on the San Andreas Fault, Monterey County, California","docAbstract":"We used high-resolution topography to quantify the spatial distribution of scarps, linear valleys, topographic sinks, and oversteepened stream channels formed along an extensional step over on the San Andreas Fault (SAF) at Mustang Ridge, California. This location provides detail of both creeping fault landform development and complex fault zone kinematics. Here, the SAF creeps 10–14 mm/yr slower than at locations ∼20 km along the fault in either direction. This spatial change in creep rate is coincident with a series of en echelon oblique-normal faults that strike obliquely to the SAF and may accommodate the missing deformation. This study presents a suite of analyses that are helpful for proper mapping of faults in locations where high-resolution topographic data are available. Furthermore, our analyses indicate that two large subsidiary faults near the center of the step over zone appear to carry significant distributed deformation based on their large apparent vertical offsets, the presence of associated sag ponds and fluvial knickpoints, and the observation that they are rotating a segment of the main SAF. Several subsidiary faults in the southeastern portion of Mustang Ridge are likely less active; they have few associated sag ponds and have older scarp morphologic ages and subdued channel knickpoints. Several faults in the northwestern part of Mustang Ridge, though relatively small, are likely also actively accommodating active fault slip based on their young morphologic ages and the presence of associated sag ponds.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Tectonics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union (AGU)","publisherLocation":"Washington, D.C.","doi":"10.1029/2010TC002673","usgsCitation":"DeLong, S.B., Hilley, G.E., Rymer, M.J., and Prentice, C., 2010, Fault zone structure from topography: signatures of en echelon fault slip at Mustang Ridge on the San Andreas Fault, Monterey County, California: Tectonics, v. 29, TC5003: 16 p., https://doi.org/10.1029/2010TC002673.","productDescription":"TC5003: 16 p.","ipdsId":"IP-018444","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":264969,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":264968,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2010TC002673"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.0,36.0 ], [ -121.0,36.5 ], [ -120.5,36.5 ], [ -120.5,36.0 ], [ -121.0,36.0 ] ] ] } } ] }","volume":"29","noUsgsAuthors":false,"publicationDate":"2010-09-02","publicationStatus":"PW","scienceBaseUri":"50e5d127e4b0a4aa5bb0b177","contributors":{"authors":[{"text":"DeLong, Stephen B. 0000-0002-0945-2172 sdelong@usgs.gov","orcid":"https://orcid.org/0000-0002-0945-2172","contributorId":5240,"corporation":false,"usgs":true,"family":"DeLong","given":"Stephen","email":"sdelong@usgs.gov","middleInitial":"B.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":470377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hilley, George E.","contributorId":85484,"corporation":false,"usgs":true,"family":"Hilley","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":470378,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rymer, Michael J. mrymer@usgs.gov","contributorId":1522,"corporation":false,"usgs":true,"family":"Rymer","given":"Michael","email":"mrymer@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":470376,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prentice, Carol","contributorId":103549,"corporation":false,"usgs":true,"family":"Prentice","given":"Carol","affiliations":[],"preferred":false,"id":470379,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70042201,"text":"70042201 - 2010 - Genetic diversity of lake whitefish in lakes Michigan and Huron: sampling, standardization, and research priorities","interactions":[],"lastModifiedDate":"2013-01-16T20:39:01","indexId":"70042201","displayToPublicDate":"2012-12-10T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Genetic diversity of lake whitefish in lakes Michigan and Huron: sampling, standardization, and research priorities","docAbstract":"We combined data from two laboratories to increase the spatial extent of a genetic data set for lake whitefish <i>Coregonus clupeaformis</i> from lakes Huron and Michigan and saw that genetic diversity was greatest between lakes, but that there was also structuring within lakes. Low diversity among stocks may be a reflection of relatively recent colonization of the Great Lakes, but other factors such as recent population fluctuation and localized stresses such as lamprey predation or heavy exploitation may also have a homogenizing effect. Our data suggested that there is asymmetrical movement of lake whitefish between Lake Huron and Lake Michigan; more genotypes associated with Lake Michigan were observed in Lake Huron. Adding additional collections to the calibrated set will allow further examination of diversity in other Great Lakes, answer questions regarding movement among lakes, and estimate contributions of stocks to commercial yields. As the picture of genetic diversity and population structure of lake whitefish in the Great Lakes region emerges, we need to develop methods to combine data types to help identify important areas for biodiversity and thus conservation. Adding genetic data to existing models will increase the precision of predictions of the impacts of new stresses and changes in existing pressures on an ecologically and commercially important species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Great Lakes Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"International Association for Great Lakes Research","publisherLocation":"Ann Arbor, MI","doi":"10.1016/j.jglr.2010.01.004","usgsCitation":"Stott, W., VanDeHey, J.A., and Sloss, B.L., 2010, Genetic diversity of lake whitefish in lakes Michigan and Huron: sampling, standardization, and research priorities: Journal of Great Lakes Research, v. 36, no. Supplement 1, p. 59-65, https://doi.org/10.1016/j.jglr.2010.01.004.","productDescription":"7 p.","startPage":"59","endPage":"65","ipdsId":"IP-013249","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":264995,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jglr.2010.01.004"},{"id":264996,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States;Canada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.9119,41.6089 ], [ -87.9119,46.0544 ], [ -81.2795,46.0544 ], [ -81.2795,41.6089 ], [ -87.9119,41.6089 ] ] ] } } ] }","volume":"36","issue":"Supplement 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e5d12ee4b0a4aa5bb0b19f","contributors":{"authors":[{"text":"Stott, Wendylee","contributorId":8058,"corporation":false,"usgs":true,"family":"Stott","given":"Wendylee","affiliations":[],"preferred":false,"id":470963,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"VanDeHey, Justin A.","contributorId":50800,"corporation":false,"usgs":true,"family":"VanDeHey","given":"Justin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":470964,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sloss, Brian L. bsloss@usgs.gov","contributorId":702,"corporation":false,"usgs":true,"family":"Sloss","given":"Brian","email":"bsloss@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":470962,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70042188,"text":"70042188 - 2010 - Genetic structure and diversity among brook trout from Isle Royale, Lake Nipigon, and three Minnesota tributaries of Lake Superior","interactions":[],"lastModifiedDate":"2016-01-29T09:08:31","indexId":"70042188","displayToPublicDate":"2012-12-10T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Genetic structure and diversity among brook trout from Isle Royale, Lake Nipigon, and three Minnesota tributaries of Lake Superior","docAbstract":"<p>Brook trout <i>Salvelinus fontinalis</i> from Isle Royale, Michigan, three Minnesota tributaries of Lake Superior, and Lake Nipigon in Ontario were analyzed for genetic variation at 12 microsatellite DNA loci. Analysis of molecular variance, genetic distance measures, and cluster analysis were used to examine the diversity, gene flow, and relatedness among the samples. The diversity estimates for the samples from Isle Royale were similar to those for the samples collected from Minnesota tributaries of Lake Superior, and all estimates were lower than those reported in other studies of brook trout from eastern North America. Genetic differences were detected among the brook trout at Isle Royale, Lake Nipigon, and the Minnesota tributaries of Lake Superior. Further, the population in Tobin Harbor at the eastern end of Isle Royale was distinct from the populations from tributaries at the southwestern end of the island. The Minnesota tributary population formed a group that was genetically distinct from those from Isle Royale and Lake Nipigon. The Isle Royale population should be managed to preserve the genetic and phenotypic variation that distinguishes it from the other brook trout populations analyzed to date.</p>","language":"English","publisher":"Taylor & Francis","publisherLocation":"London, UK","doi":"10.1577/M08-213.1","usgsCitation":"Stott, W., Quinlan, H., Gorman, O.T., and King, T.L., 2010, Genetic structure and diversity among brook trout from Isle Royale, Lake Nipigon, and three Minnesota tributaries of Lake Superior: North American Journal of Fisheries Management, v. 30, no. 2, p. 400-411, https://doi.org/10.1577/M08-213.1.","productDescription":"12 p.","startPage":"400","endPage":"411","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-009201","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":264989,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United 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,{"id":70041667,"text":"70041667 - 2010 - Interdisciplinary studies of eruption at Chaitén volcano, Chile","interactions":[],"lastModifiedDate":"2018-02-21T14:00:00","indexId":"70041667","displayToPublicDate":"2012-12-03T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Interdisciplinary studies of eruption at Chaitén volcano, Chile","docAbstract":"High-silica rhyolite magma fuels Earth's largest and most explosive eruptions. Recurrence intervals for such highly explosive eruptions are in the 100- to 100,000-year time range, and there have been few direct observations of such eruptions and their immediate impacts. Consequently, there was keen interest within the volcanology community when the first large eruption of high-silica rhyolite since that of Alaska's Novarupta volcano in 1912 began on 1 May 2008 at Chaitén volcano, southern Chile, a 3-kilometer-diameter caldera volcano with a prehistoric record of rhyolite eruptions [<i>Naranjo and Stern, 2004semi; Servicio Nacional de Geología y Minería (SERNAGEOMIN), 2008semi; Carn et al., 2009; Castro and Dingwell, 2009; Lara, 2009; Muñoz et al., 2009</i>]. Vigorous explosions occurred through 8 May 2008, after which explosive activity waned and a new lava dome was extruded.","language":"English","publisher":"American Geophysical Union (AGU)","doi":"10.1029/2010EO420001","usgsCitation":"Pallister, J.S., Major, J.J., Pierson, T.C., Holitt, R.P., Lowenstern, J.B., Eichelberger, J.C., Luis, L., Moreno, H., Muñoz, J., Castro, J.M., Iroumé, A., Andreoli, A., Jones, J., Swanson, F., and Crisafulli, C., 2010, Interdisciplinary studies of eruption at Chaitén volcano, Chile: Eos, Transactions, American Geophysical Union, v. 91, no. 42, https://doi.org/10.1029/2010EO420001.","startPage":"381","numberOfPages":"1","ipdsId":"IP-020523","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":475482,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2010eo420001","text":"Publisher Index Page"},{"id":264082,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":264081,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2010EO420001"}],"country":"Chile","volume":"91","issue":"42","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","scienceBaseUri":"50d04d14e4b0d83991d156b3","contributors":{"authors":[{"text":"Pallister, John S. 0000-0002-2041-2147 jpallist@usgs.gov","orcid":"https://orcid.org/0000-0002-2041-2147","contributorId":2024,"corporation":false,"usgs":true,"family":"Pallister","given":"John","email":"jpallist@usgs.gov","middleInitial":"S.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":470078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Major, Jon J. 0000-0003-2449-4466 jjmajor@usgs.gov","orcid":"https://orcid.org/0000-0003-2449-4466","contributorId":439,"corporation":false,"usgs":true,"family":"Major","given":"Jon","email":"jjmajor@usgs.gov","middleInitial":"J.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":470077,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pierson, Thomas C. 0000-0001-9002-4273 tpierson@usgs.gov","orcid":"https://orcid.org/0000-0001-9002-4273","contributorId":2498,"corporation":false,"usgs":true,"family":"Pierson","given":"Thomas","email":"tpierson@usgs.gov","middleInitial":"C.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":470079,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Holitt, Richard P.","contributorId":49679,"corporation":false,"usgs":true,"family":"Holitt","given":"Richard","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":470089,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lowenstern, Jacob B. 0000-0003-0464-7779 jlwnstrn@usgs.gov","orcid":"https://orcid.org/0000-0003-0464-7779","contributorId":2755,"corporation":false,"usgs":true,"family":"Lowenstern","given":"Jacob","email":"jlwnstrn@usgs.gov","middleInitial":"B.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":470080,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Eichelberger, John C.","contributorId":64971,"corporation":false,"usgs":true,"family":"Eichelberger","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":470090,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Luis, Lara","contributorId":21044,"corporation":false,"usgs":true,"family":"Luis","given":"Lara","email":"","affiliations":[],"preferred":false,"id":470084,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Moreno, Hugo","contributorId":20232,"corporation":false,"usgs":true,"family":"Moreno","given":"Hugo","email":"","affiliations":[],"preferred":false,"id":470083,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Muñoz, Jorge","contributorId":23412,"corporation":false,"usgs":true,"family":"Muñoz","given":"Jorge","affiliations":[],"preferred":false,"id":470085,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Castro, Jonathan M.","contributorId":45198,"corporation":false,"usgs":true,"family":"Castro","given":"Jonathan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":470088,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Iroumé, Andrés","contributorId":40492,"corporation":false,"usgs":true,"family":"Iroumé","given":"Andrés","affiliations":[],"preferred":false,"id":470087,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Andreoli, Andrea","contributorId":17502,"corporation":false,"usgs":true,"family":"Andreoli","given":"Andrea","email":"","affiliations":[],"preferred":false,"id":470082,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Jones, Julia","contributorId":6740,"corporation":false,"usgs":true,"family":"Jones","given":"Julia","affiliations":[],"preferred":false,"id":470081,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Swanson, Fred","contributorId":26596,"corporation":false,"usgs":true,"family":"Swanson","given":"Fred","email":"","affiliations":[],"preferred":false,"id":470086,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Crisafulli, Charlie","contributorId":92140,"corporation":false,"usgs":true,"family":"Crisafulli","given":"Charlie","affiliations":[],"preferred":false,"id":470091,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}}
,{"id":70041979,"text":"70041979 - 2010 - Diet shift of double-crested cormorants in eastern Lake Ontario associated with the expansion of the invasive round goby","interactions":[],"lastModifiedDate":"2012-12-25T17:44:21","indexId":"70041979","displayToPublicDate":"2012-12-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Diet shift of double-crested cormorants in eastern Lake Ontario associated with the expansion of the invasive round goby","docAbstract":"The proliferation of the invasive round goby (<i>Apollonia melanostoma</i>) in the Great Lakes has caused shifts in the trophic ecology in some areas. We examined the diet of double-crested cormorants (<i>Phalacrocorax auritas</i>) prior to, and immediately after, round goby population expansion at two colonies, Pigeon and Snake Islands, in eastern Lake Ontario from 1999 to 2007. Cormorant diet was determined from the examination of 10,167 pellets collected over the nine-year period. By the second year round gobies were found in the diet (2002 at Snake Island and 2003 at Pigeon Island) they were the main species consumed by cormorants at each colony. The dominance of round goby in cormorant diets had a significant effect on both daily fish consumption and seasonal trends in fish consumption compared to the pre-goby years. Seasonal differences that were observed during the pre-goby years were lost once gobies became the main diet component of cormorants. The rapid switch to a benthic prey such as round goby, from a largely limnetic fish diet demonstrates the adaptive foraging ability of cormorants. Round goby may act as a buffer for yellow perch and smallmouth bass, two sport fish impacted by cormorant predation in eastern Lake Ontario.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Great Lakes Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"International Association for Great Lakes Research","publisherLocation":"Ann Arbor, MI","doi":"10.1016/j.jglr.2010.02.013","usgsCitation":"Johnson, J.H., Ross, R.M., McCullough, R.D., and Mathers, A., 2010, Diet shift of double-crested cormorants in eastern Lake Ontario associated with the expansion of the invasive round goby: Journal of Great Lakes Research, v. 36, no. 2, p. 242-247, https://doi.org/10.1016/j.jglr.2010.02.013.","productDescription":"6 p.","startPage":"242","endPage":"247","temporalStart":"1999-01-01","temporalEnd":"2007-12-31","ipdsId":"IP-016794","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":264780,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":264779,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jglr.2010.02.013"}],"country":"United States","otherGeospatial":"Lake Ontario","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.0,43.17 ], [ -80.0,44.36 ], [ -76.0,44.36 ], [ -76.0,43.17 ], [ -80.0,43.17 ] ] ] } } ] }","volume":"36","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e5d10fe4b0a4aa5bb0b105","contributors":{"authors":[{"text":"Johnson, James H. 0000-0002-5619-3871 jhjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-5619-3871","contributorId":389,"corporation":false,"usgs":true,"family":"Johnson","given":"James","email":"jhjohnson@usgs.gov","middleInitial":"H.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":470525,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, Robert M.","contributorId":62562,"corporation":false,"usgs":true,"family":"Ross","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":470527,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCullough, Russell D.","contributorId":98154,"corporation":false,"usgs":true,"family":"McCullough","given":"Russell","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":470528,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mathers, Alastair","contributorId":36786,"corporation":false,"usgs":true,"family":"Mathers","given":"Alastair","email":"","affiliations":[],"preferred":false,"id":470526,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70042092,"text":"70042092 - 2010 - Mechanisms for chemostatic behavior in catchments: implications for CO<sub>2</sub> consumption by mineral weathering","interactions":[],"lastModifiedDate":"2017-01-18T13:43:43","indexId":"70042092","displayToPublicDate":"2012-12-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Mechanisms for chemostatic behavior in catchments: implications for CO<sub>2</sub> consumption by mineral weathering","docAbstract":"Concentrations of weathering products in streams often show relatively little variation compared to changes in discharge, both at event and annual scales. In this study, several hypothesized mechanisms for this “chemostatic behavior” were evaluated, and the potential for those mechanisms to influence relations between climate, weathering fluxes, and CO<sub>2</sub> consumption via mineral weathering was assessed. Data from Loch Vale, an alpine catchment in the Colorado Rocky Mountains, indicates that cation exchange and seasonal precipitation and dissolution of amorphous or poorly crystalline aluminosilicates are important processes that help regulate solute concentrations in the stream; however, those processes have no direct effect on CO<sub>2</sub> consumption in catchments. Hydrograph separation analyses indicate that old water stored in the subsurface over the winter accounts for about one-quarter of annual streamflow, and almost one-half of annual fluxes of Na and SiO<sub>2</sub> in the stream; thus, flushing of old water by new water (snowmelt) is an important component of chemostatic behavior. Hydrologic flushing of subsurface materials further induces chemostatic behavior by reducing mineral saturation indices and increasing reactive mineral surface area, which stimulate mineral weathering rates. CO<sub>2</sub> consumption by carbonic acid mediated mineral weathering was quantified using mass-balance calculations; results indicated that silicate mineral weathering was responsible for approximately two-thirds of annual CO<sub>2</sub> consumption, and carbonate weathering was responsible for the remaining one-third. CO<sub>2</sub> consumption was strongly dependent on annual precipitation and temperature; these relations were captured in a simple statistical model that accounted for 71% of the annual variation in CO<sub>2</sub> consumption via mineral weathering in Loch Vale.","language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.chemgeo.2009.09.014","usgsCitation":"Clow, D.W., and Mast, M.A., 2010, Mechanisms for chemostatic behavior in catchments: implications for CO<sub>2</sub> consumption by mineral weathering: Chemical Geology, v. 269, no. 1-2, p. 40-51, https://doi.org/10.1016/j.chemgeo.2009.09.014.","productDescription":"12 p.","startPage":"40","endPage":"51","ipdsId":"IP-017755","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"links":[{"id":264971,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":264970,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2009.09.014"}],"country":"United States","state":"Colorado","otherGeospatial":"Loch Vale","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,37.0 ], [ -109.0,41.0 ], [ -102.0,41.0 ], [ -102.0,37.0 ], [ -109.0,37.0 ] ] ] } } ] }","volume":"269","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e5d168e4b0a4aa5bb0b274","contributors":{"authors":[{"text":"Clow, David W. 0000-0001-6183-4824 dwclow@usgs.gov","orcid":"https://orcid.org/0000-0001-6183-4824","contributorId":1671,"corporation":false,"usgs":true,"family":"Clow","given":"David","email":"dwclow@usgs.gov","middleInitial":"W.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":470759,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mast, M. Alisa 0000-0001-6253-8162 mamast@usgs.gov","orcid":"https://orcid.org/0000-0001-6253-8162","contributorId":827,"corporation":false,"usgs":true,"family":"Mast","given":"M.","email":"mamast@usgs.gov","middleInitial":"Alisa","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":470758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70041975,"text":"70041975 - 2010 - Migratory salmonid redd habitat characteristics in the Salmon River, New York","interactions":[],"lastModifiedDate":"2012-12-31T15:01:02","indexId":"70041975","displayToPublicDate":"2012-12-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Migratory salmonid redd habitat characteristics in the Salmon River, New York","docAbstract":"Non-native migratory salmonids ascend tributaries to spawn in all the Great Lakes. In Lake Ontario, these species include Chinook salmon (<i>Oncorhynchus tshawytscha</i>), coho salmon (<i>O. kisutch</i>), steelhead (<i>O. mykiss</i>), and brown trout (<i>Salmo trutta</i>). Although successful natural reproduction has been documented for many of these species, little research has been conducted on their spawning habitat. We examined the spawning habitat of these four species in the Salmon River, New York. Differences in fish size among the species were significantly correlated with spawning site selection. In the Salmon River, the larger species spawned in deeper areas with larger size substrate and made the largest redds. Discriminant function analysis correctly classified redds by species 64–100% of the time. The size of substrate materials below Lighthouse Hill Dam is within the preferred ranges for spawning for these four species indicating that river armoring has not negatively impacted salmonid production. Intra-specific and inter-specific competition for spawning sites may influence redd site selection for smaller salmonids and could be an impediment for Atlantic salmon (<i>S. salar</i>) restoration.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Great Lakes Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"International Association for Great Lakes Research","publisherLocation":"Ann Arbor, MI","doi":"10.1016/j.jglr.2010.02.012","usgsCitation":"Johnson, J.H., Nack, C.C., and McKenna, J., 2010, Migratory salmonid redd habitat characteristics in the Salmon River, New York: Journal of Great Lakes Research, v. 36, no. 2, p. 387-392, https://doi.org/10.1016/j.jglr.2010.02.012.","productDescription":"6 p.","startPage":"387","endPage":"392","ipdsId":"IP-013747","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":264990,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jglr.2010.02.012"},{"id":264992,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","city":"Altmar","otherGeospatial":"Salmon River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.166667,43.5 ], [ -76.166667,43.583333 ], [ -75.916667,43.583333 ], [ -75.916667,43.5 ], [ -76.166667,43.5 ] ] ] } } ] }","volume":"36","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e5d16fe4b0a4aa5bb0b290","contributors":{"authors":[{"text":"Johnson, James H. 0000-0002-5619-3871 jhjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-5619-3871","contributorId":389,"corporation":false,"usgs":true,"family":"Johnson","given":"James","email":"jhjohnson@usgs.gov","middleInitial":"H.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":470518,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nack, Christopher C.","contributorId":66137,"corporation":false,"usgs":true,"family":"Nack","given":"Christopher","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":470520,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenna, James E. Jr.","contributorId":56992,"corporation":false,"usgs":true,"family":"McKenna","given":"James E.","suffix":"Jr.","affiliations":[],"preferred":false,"id":470519,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70042029,"text":"70042029 - 2010 - Lakewide estimates of alewife biomass and Chinook salmon abundance and consumption in Lake Ontario, 1989–2005: implications for prey fish sustainability","interactions":[],"lastModifiedDate":"2012-12-28T11:12:05","indexId":"70042029","displayToPublicDate":"2012-12-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Lakewide estimates of alewife biomass and Chinook salmon abundance and consumption in Lake Ontario, 1989–2005: implications for prey fish sustainability","docAbstract":"Stocking levels of Chinook salmon <i>Oncorhynchus tshawytscha</i> for Lake Ontario have been highly controversial since the early 1990s, largely because of uncertainties about lakewide abundance and rates of prey consumption. Previous estimates have focused on years before 1995; since then, however, the Lake Ontario ecosystem has undergone substantial changes, and there is new evidence of extensive natural recruitment. Presented here are new abundance estimates of Chinook salmon and alewives <i>Alosa pseudoharengus</i> in Lake Ontario and a reevaluation of the potential risk of alewife population collapse. We found that Lake Ontario has been supporting, on average (1989–2005), 1.83 × 10<sup>6</sup> (range, 1.08 × 10<sup>6</sup> to 3.24 × 10<sup>6</sup>) Chinook salmon of ages 1–4, amounting to a mean annual biomass of 11.33 × 10<sup>3</sup> metric tons (range, 5.83 × 10<sup>3</sup> to 23.04 × 10<sup>3</sup> metric tons). During the same period (1989–2005), the lake supported an alewife biomass of 173.66 × 103 metric tons (range, 62.37 × 10<sup>3</sup> to 345.49 × 10<sup>3</sup> metric tons); Chinook salmon of ages 1–4 consumed, on average, 22% (range, 11–44%) of the alewife biomass annually. Because our estimates probably underestimate total consumption and because Chinook salmon are only one of several salmonine species that depend on alewives, predation pressure on the Lake Ontario alewife population may be high enough to raise concerns about long-term stability of this predator–prey system.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis Group","publisherLocation":"London, UK","doi":"10.1577/T08-216.1","usgsCitation":"Murry, B.A., Connerton, M., O’Gorman, R., Stewart, D.J., and Ringlerd, N.H., 2010, Lakewide estimates of alewife biomass and Chinook salmon abundance and consumption in Lake Ontario, 1989–2005: implications for prey fish sustainability: Transactions of the American Fisheries Society, v. 139, no. 1, p. 223-240, https://doi.org/10.1577/T08-216.1.","productDescription":"18 p.","startPage":"223","endPage":"240","ipdsId":"IP-016135","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":264875,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T08-216.1"},{"id":264877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Lake Ontario","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.0,43.17 ], [ -80.0,44.36 ], [ -76.0,44.36 ], [ -76.0,43.17 ], [ -80.0,43.17 ] ] ] } } ] }","volume":"139","issue":"1","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"50df5923e4b0dfbe79e6b828","contributors":{"authors":[{"text":"Murry, Brent A.","contributorId":16294,"corporation":false,"usgs":true,"family":"Murry","given":"Brent","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":470632,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Connerton, Michael J.","contributorId":21435,"corporation":false,"usgs":true,"family":"Connerton","given":"Michael J.","affiliations":[],"preferred":false,"id":470633,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Gorman, Robert rogorman@usgs.gov","contributorId":3451,"corporation":false,"usgs":true,"family":"O’Gorman","given":"Robert","email":"rogorman@usgs.gov","affiliations":[],"preferred":true,"id":470631,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stewart, Donald J.","contributorId":33660,"corporation":false,"usgs":true,"family":"Stewart","given":"Donald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":470634,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ringlerd, Neil H.","contributorId":52860,"corporation":false,"usgs":true,"family":"Ringlerd","given":"Neil","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":470635,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70042172,"text":"70042172 - 2010 - Long-term trends in habitat use of offshore demersal fishes in western Lake Huron suggest large-scale ecosystem change","interactions":[],"lastModifiedDate":"2012-12-31T12:21:07","indexId":"70042172","displayToPublicDate":"2012-12-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Long-term trends in habitat use of offshore demersal fishes in western Lake Huron suggest large-scale ecosystem change","docAbstract":"We estimated mean depths of capture for offshore demersal fish species, grouped into three habitat-based guilds (shallow benthic, pelagic, and deep benthic), using fall bottom trawl data (27–73 m) in the western main basin of Lake Huron from 1976 to 2007. The mean depth of capture of the shallow and deep benthic guilds initially exhibited a trend toward capture in shallower water, switched to a trend toward capture in deeper water in 1991, and changed back to a trend toward capture in shallower water in 2001–2002. Species in the pelagic guild showed a similar pattern, but the initial change point occurred in 1981 for this guild. Individual species in these guilds showed variable patterns of depth distribution, but a feature common to all guilds and all pelagic and deep benthic species was a change to a trend toward capturing fish in shallower water that occurred nearly simultaneously (1999–2002). These common trends suggest that large-scale factors are affecting the habitat use of offshore demersal fish species in Lake Huron. The depth distributions of the three guilds have converged in recent years, indicating that the locations of suitable habitat for offshore demersal fishes may be changing. Our results indicate that the benthic ecology of the western main basin of Lake Huron is undergoing profound changes across a large spatial scale that are affecting the habitat use of offshore demersal fishes. We suggest that these changes are related to recent invasions of exotic species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","doi":"10.1577/T09-090.1","usgsCitation":"Riley, S., and Adams, J.V., 2010, Long-term trends in habitat use of offshore demersal fishes in western Lake Huron suggest large-scale ecosystem change: Transactions of the American Fisheries Society, v. 139, no. 5, p. 1322-1334, https://doi.org/10.1577/T09-090.1.","productDescription":"13 p.","startPage":"1322","endPage":"1334","ipdsId":"IP-013678","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":264967,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":264966,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T09-090.1"}],"country":"Canada;United States","otherGeospatial":"Lake Huron","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.95,43.0 ], [ -83.95,46.0 ], [ -81.15,46.0 ], [ -81.15,43.0 ], [ -83.95,43.0 ] ] ] } } ] }","volume":"139","issue":"5","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"50e5d15ee4b0a4aa5bb0b252","contributors":{"authors":[{"text":"Riley, Stephen C.","contributorId":84183,"corporation":false,"usgs":true,"family":"Riley","given":"Stephen C.","affiliations":[],"preferred":false,"id":470895,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, Jean V. 0000-0002-9101-068X jvadams@usgs.gov","orcid":"https://orcid.org/0000-0002-9101-068X","contributorId":3140,"corporation":false,"usgs":true,"family":"Adams","given":"Jean","email":"jvadams@usgs.gov","middleInitial":"V.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":470894,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70041901,"text":"70041901 - 2010 - Georeferencing the Large-Scale Aerial Photographs of a Great Lakes Coastal Wetland:  A Modified Photogrammetric Method","interactions":[],"lastModifiedDate":"2022-09-02T15:15:25.359476","indexId":"70041901","displayToPublicDate":"2012-12-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Georeferencing the Large-Scale Aerial Photographs of a Great Lakes Coastal Wetland:  A Modified Photogrammetric Method","docAbstract":"The geocontrol template method was developed to georeference multiple, overlapping analog aerial photographs without reliance upon conventionally obtained horizontal ground control. The method was tested as part of a long-term wetland habitat restoration project at a Lake Erie coastal wetland complex in the U.S. Fish and Wildlife Service Ottawa National Wildlife Refuge. As in most coastal wetlands, annually identifiable ground-control features required to georeference photo-interpreted data are difficult to find. The geocontrol template method relies on the following four components: (a) an uncontrolled aerial photo mosaic of the study area, (b) global positioning system (GPS) derived horizontal coordinates of each photo’s principal point, (c) a geocontrol template created by the transfer of fiducial markings and calculated principal points to clear acetate from individual photographs arranged in a mosaic, and (d) the root-mean-square-error testing of the system to ensure an acceptable level of planimetric accuracy. Once created for a study area, the geocontrol template can be registered in geographic information system (GIS) software to facilitate interpretation of multiple images without individual image registration. The geocontrol template enables precise georeferencing of single images within larger blocks of photographs using a repeatable and consistent method.","language":"English","publisher":"Springer","doi":"10.1007/s13157-010-0027-9","usgsCitation":"Kowalski, K., and Grapentine, J.L., 2010, Georeferencing the Large-Scale Aerial Photographs of a Great Lakes Coastal Wetland:  A Modified Photogrammetric Method: Wetlands, v. 30, no. 2, p. 369-374, https://doi.org/10.1007/s13157-010-0027-9.","productDescription":"6 p.","startPage":"369","endPage":"374","ipdsId":"IP-013374","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":267604,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Ohio","otherGeospatial":"Lake Erie, Ottawa National Wildlife Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.2602310180664,\n              41.605431236301456\n            ],\n            [\n              -83.26074600219727,\n              41.60478944688097\n            ],\n            [\n              -83.11878204345703,\n              41.604019291149854\n            ],\n            [\n              -83.11895370483398,\n              41.61492897332632\n            ],\n            [\n              -83.12633514404297,\n              41.617752355216076\n            ],\n            [\n              -83.13577651977539,\n              41.61646901513335\n            ],\n            [\n              -83.19551467895508,\n              41.63238062721709\n            ],\n            [\n              -83.23740005493164,\n              41.651879827111344\n            ],\n            [\n              -83.26074600219727,\n              41.64097639649512\n            ],\n            [\n              -83.2602310180664,\n              41.605431236301456\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-02-25","publicationStatus":"PW","scienceBaseUri":"5120b893e4b0e93254cd7547","contributors":{"authors":[{"text":"Kowalski, Kurt P. 0000-0002-8424-4701 kkowalski@usgs.gov","orcid":"https://orcid.org/0000-0002-8424-4701","contributorId":3768,"corporation":false,"usgs":true,"family":"Kowalski","given":"Kurt P.","email":"kkowalski@usgs.gov","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":470344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grapentine, Joel L.","contributorId":53674,"corporation":false,"usgs":true,"family":"Grapentine","given":"Joel","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":470345,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70041890,"text":"70041890 - 2010 - Linking non-culturable (qPCR) and culturable enterococci densities with hydrometeorological conditions","interactions":[],"lastModifiedDate":"2012-12-28T12:23:14","indexId":"70041890","displayToPublicDate":"2012-12-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Linking non-culturable (qPCR) and culturable enterococci densities with hydrometeorological conditions","docAbstract":"Quantitative polymerase chain reaction (qPCR) measurement of enterococci has been proposed as a rapid technique for assessment of beach water quality, but the response of qPCR results to environmental conditions has not been fully explored. Culture-based <i>E. coli</i> and enterococci have been used in empirical predictive models to characterize their responses to environmental conditions and to increase monitoring frequency and efficiency. This approach has been attempted with qPCR results only in few studies. During the summer of 2006, water samples were collected from two southern Lake Michigan beaches and the nearby river outfall (Burns Ditch) and were analyzed for enterococci by culture-based and non-culture-based (i.e., qPCR) methods, as well as culture-based <i>E. coli</i>. Culturable enterococci densities (log CFU/100 ml) for the beaches were significantly correlated with enterococci qPCR cell equivalents (CE) (<i>R</i> = 0.650, <i>P</i> < 0.0001, <i>N</i> = 32). Enterococci CE and CFU densities were highest in Burns Ditch relative to the beach sites; however, only CFUs were significantly higher (<i>P</i> < 0.0001). Culturable enterococci densities at Burns Ditch and the beaches were significantly correlated (<i>R</i> = 0.565, <i>P</i> < 0.0001, <i>N</i> = 32). Culturable E. coli and enterococci densities were significantly correlated (<i>R</i> = 0.682, <i>P</i> < 0.0001, <i>N</i> = 32). Regression analyses suggested that enterococci CFU could be predicted by lake turbidity, Burns Ditch discharge, and wind direction (adjusted <i>R<sup>2</sup></i> = 0.608); enterococci CE was best predicted by Burns Ditch discharge and log-transformed lake turbidity × wave height (adjusted <i>R<sup>2</sup></i> = 0.40). In summary, our results show that analytically, the qPCR method compares well to the non-culture-based method for measuring enterococci densities in beach water and that both these approaches can be predicted by hydrometeorological conditions. Selected predictors and model results highlight the differences between the environmental responses of the two method endpoints and the potentially high variance in qPCR results","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Science of the Total Environment","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.scitotenv.2010.04.051","usgsCitation":"Byappanahalli, M., Whitman, R.L., Shively, D.A., and Nevers, M.B., 2010, Linking non-culturable (qPCR) and culturable enterococci densities with hydrometeorological conditions: Science of the Total Environment, v. 408, no. 16, p. 3096-3101, https://doi.org/10.1016/j.scitotenv.2010.04.051.","productDescription":"6 p.","startPage":"3096","endPage":"3101","temporalStart":"2006-06-01","temporalEnd":"2006-09-21","ipdsId":"IP-011437","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":264885,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":264884,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.scitotenv.2010.04.051"}],"country":"United States","otherGeospatial":"Lake Michigan","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.9,41.3 ], [ -87.9,44.54 ], [ -84.95,44.54 ], [ -84.95,41.3 ], [ -87.9,41.3 ] ] ] } } ] }","volume":"408","issue":"16","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50df8f37e4b0dfbe79e6d85c","contributors":{"authors":[{"text":"Byappanahalli, Muruleedhara N.","contributorId":47335,"corporation":false,"usgs":true,"family":"Byappanahalli","given":"Muruleedhara N.","affiliations":[],"preferred":false,"id":470321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitman, Richard L. rwhitman@usgs.gov","contributorId":542,"corporation":false,"usgs":true,"family":"Whitman","given":"Richard","email":"rwhitman@usgs.gov","middleInitial":"L.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":470319,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shively, Dawn A. dshively@usgs.gov","contributorId":2051,"corporation":false,"usgs":true,"family":"Shively","given":"Dawn","email":"dshively@usgs.gov","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":470320,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nevers, Meredith B.","contributorId":91803,"corporation":false,"usgs":true,"family":"Nevers","given":"Meredith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":470322,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70042019,"text":"70042019 - 2010 - Lake trout population dynamics in the Northern Refuge of Lake Michigan: Implications for future rehabilitation","interactions":[],"lastModifiedDate":"2019-11-27T09:36:07","indexId":"70042019","displayToPublicDate":"2012-12-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Lake trout population dynamics in the Northern Refuge of Lake Michigan: Implications for future rehabilitation","docAbstract":"The Northern Refuge was established in 1985 as part of the lake trout <i>Salvelinus namaycush</i> rehabilitation effort for Lake Michigan. To evaluate progress toward lake trout rehabilitation in the Northern Refuge, we conducted annual (1991–2008) gill-net surveys in the fall to assess the adult population and beam trawl surveys in the spring to assess naturally reproduced age-0 lake trout. Our criteria for evaluating progress included the density of “wild” age-0 fish within the Northern Refuge, the proportion of wild fish within the adult population, density of spawners, adult survival, growth, and wounding rate by sea lampreys <i>Petromyzon marinus</i>. No wild age-0 lake trout were caught in the Northern Refuge during 1991–2008. Overall, wild lake trout did not recruit to the adult population to any detectable degree. The mean density of spawning lake trout decreased from 45 fish·305 m of gill net<sup>−1</sup>·d<sup>−1</sup> during 1991–1999 to only 4 fish·305 m<sup>−1</sup>·d<sup>−1</sup> during 2000–2008. Although the sea lamprey wounding rate more than doubled between these two time periods, catch curve analysis revealed that mortality of adult lake trout actually decreased between the two periods. Therefore, the 90% decrease in abundance of spawning lake trout between the two periods could not be attributed to increased sea lamprey predation but instead was probably due in part to the reduced lake trout stocking rate during 1995–2005. The paucity of natural reproduction in the Northern Refuge during 1991–2008 most likely resulted from alewife <i>Alosa pseudoharengus</i> interference with lake trout reproduction and from the relatively low lake trout spawner density during 2000–2008. Our results suggest that the annual stocking rate of lake trout yearlings should be increased to at least 250,000 fish/reef to achieve greater densities of spawners.","language":"English","publisher":"Taylor & Francis ","doi":"10.1577/M09-108.1","usgsCitation":"Madenjiana, C.P., and Desorcie, T.J., 2010, Lake trout population dynamics in the Northern Refuge of Lake Michigan: Implications for future rehabilitation: North American Journal of Fisheries Management, v. 30, no. 3, p. 629-641, https://doi.org/10.1577/M09-108.1.","productDescription":"13 p.","startPage":"629","endPage":"641","ipdsId":"IP-015186","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":264866,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Lake Michigan","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0,41.6 ], [ -88.0,46.0 ], [ -84.9,46.0 ], [ -84.9,41.6 ], [ -88.0,41.6 ] ] ] } } ] }","volume":"30","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-06-01","publicationStatus":"PW","scienceBaseUri":"50df5897e4b0dfbe79e6b7d0","contributors":{"authors":[{"text":"Madenjiana, Charles P.","contributorId":53262,"corporation":false,"usgs":true,"family":"Madenjiana","given":"Charles","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":470617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Desorcie, Timothy J. 0000-0002-9965-1668","orcid":"https://orcid.org/0000-0002-9965-1668","contributorId":23480,"corporation":false,"usgs":true,"family":"Desorcie","given":"Timothy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":470616,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70041922,"text":"70041922 - 2010 - Method for calculating self-noise spectra and operating ranges for seismographic inertial sensors and recorders","interactions":[],"lastModifiedDate":"2012-12-31T13:49:35","indexId":"70041922","displayToPublicDate":"2012-12-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Method for calculating self-noise spectra and operating ranges for seismographic inertial sensors and recorders","docAbstract":"Understanding the performance of sensors and recorders is prerequisite to making appropriate use of them in seismology and earthquake engineering. This paper explores a critical aspect of instrument performance, the “self” noise level of the device and the amplitude range it can usefully record. Self noise limits the smallest signals, while instrument clipping level creates the upper limit (above which it either cannot produce signals or becomes unacceptably nonlinear). Where these levels fall, and the “operating range” between them, determines much of the instrument's viability and the applications for which it is appropriate. The representation of seismic-instrument self-noise levels and their effective operating ranges (cf., dynamic range) for seismological inertial sensors, recorders (data acquisition units, or DAUs), and integrated systems of sensors and recorders (data acquisition systems, or DASs) forces one to address an unnatural comparison between transient finite-bandwidth signals, such as earthquake records, and the instrument's self noise, an effectively stationary signal of infinite duration. In addition to being transient, earthquakes and other records of interest are characterized by a peak amplitude and generally a narrow, peaked spectral shape. Unfortunately, any power spectrum computed for such transient signals is ill defined, since the maximum of that spectrum depends strongly upon signal and record durations. In contrast, the noise floor of an instrument is approximately stationary and properly described by a power spectral density (PSD) or its root (rPSD). Put another way, earthquake records have units of amplitude (<i>e.g.</i>, m/s<sup>2</sup>) while PSDs have units of amplitude-squared per hertz (<i>e.g.</i>, (m/s<sup>2</sup>)<sup>2</sup>/Hz) and the rPSD has units of amplitude per root of hertz (<i>e.g.</i>, (m/s<sup>2</sup>)/Hz<sup>1/2</sup>). Thus, this incompatability is a conflict between earthquake (amplitude) and PSD (spectral density) units that requires one to make various assumptions before they can be compared. For purposes of instrument operational performance, we provide a means of evaluating signal and noise and the range between them in a manner representative of time-domain instrument performance. We call these “operating range diagrams” (ORDs), plots of instrument self noise and clipping level; the “operating range” is the range between these values. For frequency-domain performance we elect to show self noise as an rPSD that may be compared to another instrument's noise or to ambient Earth noise (<i>e.g.</i>, Peterson 1993); however, to limit the number of arbitrary choices required to merge transient and stationary signals we do not compare the rPSD to transient signals in the frequency domain. Our solution for a time-domain comparison is not new but rather builds upon the consensus of the first and second Guidelines for Seismometer Testing workshops (Hutt <i>et al.</i> 2009) and long established practice in acoustics. We propose this method as a standard for characterizing seismic instruments, and it has been endorsed by the second workshop (Hutt <i>et al.</i> 2009, 2010) and the Advanced National Seismic System (ANSS) Working Group (2008) and recent ANSS procurement specifications.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Seismological Research Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Seismological Society of America","publisherLocation":"El Cerrito, CA","doi":"10.1785/gssrl.81.4.640","usgsCitation":"Evans, J.R., Followill, F., Hutt, C.R., Kromer, R., Nigbor, R., Ringler, A., Steim, J., and Wielandt, E., 2010, Method for calculating self-noise spectra and operating ranges for seismographic inertial sensors and recorders: Seismological Research Letters, v. 81, no. 4, p. 640-646, https://doi.org/10.1785/gssrl.81.4.640.","productDescription":"7 p.","startPage":"640","endPage":"646","ipdsId":"IP-015382","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":264981,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/gssrl.81.4.640"},{"id":264982,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"81","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-01","publicationStatus":"PW","scienceBaseUri":"50e5d16de4b0a4aa5bb0b283","contributors":{"authors":[{"text":"Evans, John R. jrevans@usgs.gov","contributorId":529,"corporation":false,"usgs":true,"family":"Evans","given":"John","email":"jrevans@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":470385,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Followill, F.","contributorId":93357,"corporation":false,"usgs":true,"family":"Followill","given":"F.","affiliations":[],"preferred":false,"id":470391,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hutt, Charles R. 0000-0001-9033-9195 bhutt@usgs.gov","orcid":"https://orcid.org/0000-0001-9033-9195","contributorId":1622,"corporation":false,"usgs":true,"family":"Hutt","given":"Charles","email":"bhutt@usgs.gov","middleInitial":"R.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":470386,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kromer, R.P.","contributorId":21838,"corporation":false,"usgs":true,"family":"Kromer","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":470388,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nigbor, R.L.","contributorId":30699,"corporation":false,"usgs":true,"family":"Nigbor","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":470389,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ringler, A. 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,{"id":70040381,"text":"70040381 - 2010 - Population trends of forest birds at Hakalau Forest National Wildlife Refuge, Hawai'i","interactions":[],"lastModifiedDate":"2012-10-17T17:16:17","indexId":"70040381","displayToPublicDate":"2012-10-17T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3551,"text":"The Condor","active":true,"publicationSubtype":{"id":10}},"title":"Population trends of forest birds at Hakalau Forest National Wildlife Refuge, Hawai'i","docAbstract":"The Hakalau Forest National Wildlife Refuge was established to protect native Hawaiian forest birds, particularly endangered species. Management for forest restoration on the refuge has consisted mainly of removing feral ungulates, controlling invasive alien plants, and reforesting former pastures. 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The closed forest was surveyed in only the most recent 9 years, and trajectories of native species there were mixed. Overall, long-term population trends in Hakalau are stable or increasing, contrasting with declines in most other areas of Hawai'i over the same period. 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,{"id":70004402,"text":"70004402 - 2010 - Whooping crane titers in response to eastern equine encephalitis immunization","interactions":[],"lastModifiedDate":"2018-02-06T12:41:06","indexId":"70004402","displayToPublicDate":"2012-06-19T15:24:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Whooping crane titers in response to eastern equine encephalitis immunization","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the Eleventh North American Crane Workshop, 23-27 September 2008, Wisconsin Dells, Wisconsin, USA","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"11th North American Crane Workshop","usgsCitation":"Olsen, G.H., 2010, Whooping crane titers in response to eastern equine encephalitis immunization, <i>in</i> Proceedings of the Eleventh North American Crane Workshop, 23-27 September 2008, Wisconsin Dells, Wisconsin, USA, p. 180-182.","productDescription":"3 p.","startPage":"180","endPage":"182","numberOfPages":"3","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":258032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258022,"rank":9999,"type":{"id":1,"text":"Abstract"},"url":"https://www.savingcranes.org/cart/books/proceedings-of-the-eleventh-north-american-crane-workshop.html","linkFileType":{"id":5,"text":"html"}},{"id":258023,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.worldcat.org/title/proceedings-of-the-eleventh-north-american-crane-workshop-23-27-september-2008-wisconsin-dells-wisconsin/oclc/719514948","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd098e4b08c986b32ef48","contributors":{"editors":[{"text":"Hartup, Barry K.","contributorId":112921,"corporation":false,"usgs":true,"family":"Hartup","given":"Barry","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":508233,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Urbanek, Richard P.","contributorId":38400,"corporation":false,"usgs":true,"family":"Urbanek","given":"Richard","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":508232,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Olsen, Glenn H. 0000-0002-7188-6203 golsen@usgs.gov","orcid":"https://orcid.org/0000-0002-7188-6203","contributorId":40918,"corporation":false,"usgs":true,"family":"Olsen","given":"Glenn","email":"golsen@usgs.gov","middleInitial":"H.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":350454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70004098,"text":"70004098 - 2010 - Bobcats (<i>Lynx rufus</i>)","interactions":[],"lastModifiedDate":"2012-06-28T01:01:38","indexId":"70004098","displayToPublicDate":"2012-06-19T14:34:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Bobcats (<i>Lynx rufus</i>)","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Urban Carnivores: Ecology, Conflict, and Conservation","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"The Johns Hopkins University Press","publisherLocation":"Baltimore, MD","usgsCitation":"Riley, S.P., Boydston, E.E., Crooks, K.R., and Lyren, L.M., 2010, Bobcats (<i>Lynx rufus</i>), chap. <i>of</i> Urban Carnivores: Ecology, Conflict, and Conservation, p. 121-140.","productDescription":"20 p.","startPage":"121","endPage":"140","numberOfPages":"18","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":258028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":21784,"rank":9999,"type":{"id":1,"text":"Abstract"},"url":"https://jhupbooks.press.jhu.edu/ecom/MasterServlet/GetItemDetailsHandler?iN=9780801893896&qty=1&source=2&viewMode=3&loggedIN=false&JavaScript=y","linkFileType":{"id":5,"text":"html"}},{"id":258018,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.worldcat.org/title/urban-carnivores-ecology-conflict-and-conservation/oclc/320696593","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f1f1e4b0c8380cd4aef6","contributors":{"editors":[{"text":"Gehrt, Stanley D.","contributorId":114061,"corporation":false,"usgs":true,"family":"Gehrt","given":"Stanley","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":508222,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Riley, Seth P. D.","contributorId":113734,"corporation":false,"usgs":false,"family":"Riley","given":"Seth P. D.","affiliations":[{"id":6924,"text":"National Park Service, Upper Columbia Basin Network","active":true,"usgs":false}],"preferred":false,"id":508221,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Cypher, Brian L.","contributorId":111868,"corporation":false,"usgs":true,"family":"Cypher","given":"Brian","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":508220,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Riley, Seth P.D.","contributorId":83246,"corporation":false,"usgs":true,"family":"Riley","given":"Seth","email":"","middleInitial":"P.D.","affiliations":[],"preferred":false,"id":350421,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boydston, Erin E. 0000-0002-8452-835X eboydston@usgs.gov","orcid":"https://orcid.org/0000-0002-8452-835X","contributorId":1705,"corporation":false,"usgs":true,"family":"Boydston","given":"Erin","email":"eboydston@usgs.gov","middleInitial":"E.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":350418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crooks, Kevin R.","contributorId":51137,"corporation":false,"usgs":false,"family":"Crooks","given":"Kevin","email":"","middleInitial":"R.","affiliations":[{"id":6621,"text":"Colorado State University","active":true,"usgs":false}],"preferred":false,"id":350420,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lyren, Lisa M. llyren@usgs.gov","contributorId":2398,"corporation":false,"usgs":true,"family":"Lyren","given":"Lisa","email":"llyren@usgs.gov","middleInitial":"M.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":350419,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70004238,"text":"70004238 - 2010 - 7.2.3 Land Birds","interactions":[],"lastModifiedDate":"2012-06-28T01:01:38","indexId":"70004238","displayToPublicDate":"2012-06-19T12:56:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"7.2.3 Land Birds","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Oregon Climate Change Research Institute (2010), Oregon Climate Assessment Report","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisherLocation":"Reston, VA","usgsCitation":"Haig, S.M., 2010, 7.2.3 Land Birds, chap. <i>of</i> Oregon Climate Change Research Institute (2010), Oregon Climate Assessment Report, p. 278-282.","productDescription":"5 p.","startPage":"278","endPage":"282","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":258001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257999,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://library.state.or.us/repository/2010/201012011104133/7-9.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e26ce4b0c8380cd45b85","contributors":{"editors":[{"text":"Hixon, M.A.","contributorId":111865,"corporation":false,"usgs":true,"family":"Hixon","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":508228,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Gregory, S.V.","contributorId":21130,"corporation":false,"usgs":true,"family":"Gregory","given":"S.V.","email":"","affiliations":[],"preferred":false,"id":508226,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Robinson, W.D.","contributorId":29928,"corporation":false,"usgs":true,"family":"Robinson","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":508227,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"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":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":350441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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