{"pageNumber":"1413","pageRowStart":"35300","pageSize":"25","recordCount":46730,"records":[{"id":70016972,"text":"70016972 - 1992 - Triton's surface-atmosphere energy balance","interactions":[],"lastModifiedDate":"2024-02-15T23:24:44.090565","indexId":"70016972","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Triton's surface-atmosphere energy balance","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id7\" class=\"abstract author\"><div id=\"aep-abstract-sec-id8\"><p>We explore the energetics of Triton's surface-atmosphere system using a model that includes the turbulent transfer of sensible heat as well as insolation, reradiation, and latent heat transport. The model relies on a 1° by 1° resolution hemispheric bolometric albedo map of Triton for determining the atmospheric temperature, the N<sub>2</sub><span>&nbsp;</span>frost emissivity, and the temperatures of unfrosted portions of the surface consistent with a frost temperature of ≅38 K. For a physically plausible range of heat transfer coefficients, we find that the atmospheric temperature roughly 1 km above the surface is approximately 1 to 3 K hotter than the surface. Atmospheric temperatures of 48 K suggested by early analysis of radio occultation data cannot be obtained for plausible values of the heat transfer coefficients. Our calculations indicate that Triton's N<sub>2</sub><span>&nbsp;</span>frosts must have an emissivity well below unity in order to have a temperature of ≅38 K, consistent with previous results. We also find that convection over small hot spots does not significantly cool them off, so they may be able to act as continous sources of buoyancy for convective plumes, but have not explored whether the convection is vigorous enough to entrain particulate matter thereby forming a dust devil. Our elevated atmospheric temperatures make geyser driven plumes with initial upward velocities ≤10 m s<sup>−1</sup><span>&nbsp;</span>stagnate in the lower atmosphere. These “wimpy” plumes provide a possible explanation for Triton's “wind streaks.”</p></div></div></div></div><div id=\"preview-section-introduction\"><br></div><div id=\"preview-section-snippets\"><br></div><div id=\"preview-section-references\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(92)90144-V","issn":"00191035","usgsCitation":"Stansberry, J., Yelle, R., Lunine, J., and McEwen, A.S., 1992, Triton's surface-atmosphere energy balance: Icarus, v. 99, no. 2, p. 242-260, https://doi.org/10.1016/0019-1035(92)90144-V.","productDescription":"19 p.","startPage":"242","endPage":"260","numberOfPages":"19","costCenters":[],"links":[{"id":224713,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"99","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb87ae4b08c986b32789d","contributors":{"authors":[{"text":"Stansberry, J.A.","contributorId":80430,"corporation":false,"usgs":true,"family":"Stansberry","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":375007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yelle, R.V.","contributorId":74523,"corporation":false,"usgs":true,"family":"Yelle","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":375006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lunine, J. I.","contributorId":51899,"corporation":false,"usgs":false,"family":"Lunine","given":"J. I.","affiliations":[],"preferred":false,"id":375005,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McEwen, A. S.","contributorId":11317,"corporation":false,"usgs":true,"family":"McEwen","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":375004,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70188408,"text":"70188408 - 1992 - The 1990 conterminous U. S. AVHRR data set","interactions":[],"lastModifiedDate":"2017-06-08T12:44:48","indexId":"70188408","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"The 1990 conterminous U. S. AVHRR data set","docAbstract":"<p>The U.S. Geological Survey, using NOAA-ll Advanced Very High Resolution Radiometer (AVHRR) 1-km data, has produced a time series of 19 biweekly maximum normalized difference vegetation index (NDV!) composites of the conterminous United States for the 1990 growing season. Each biweekly composite included data from approximately 20 calibrated and georegistered daily overpasses. The output is a data set which includes all five calibrated AVHRR channels, NOV! values, three satellite/solar viewing angles, and date of observation pointer for each biweekly composite. The data set is intended for assessing seasonal variations in vegetation condition and provides a foundation for studying long-term changes in vegetation resulting from human interactions or global climate alterations.</p>","language":"English","publisher":"ASPRS","usgsCitation":"Eidenshink, J.C., 1992, The 1990 conterminous U. S. AVHRR data set: Photogrammetric Engineering and Remote Sensing, v. 58, no. 6, p. 809-813.","productDescription":"5 p.","startPage":"809","endPage":"813","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":342296,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"593ad70fe4b0764e6c602182","contributors":{"authors":[{"text":"Eidenshink, Jeffery C. eidenshink@usgs.gov","contributorId":1352,"corporation":false,"usgs":true,"family":"Eidenshink","given":"Jeffery","email":"eidenshink@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":697627,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016876,"text":"70016876 - 1992 - New look at regional flood-frequency relations for arid lands","interactions":[],"lastModifiedDate":"2013-03-16T07:49:38","indexId":"70016876","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2338,"text":"Journal of Hydraulic Engineering","active":true,"publicationSubtype":{"id":10}},"title":"New look at regional flood-frequency relations for arid lands","docAbstract":"A new method is proposed that combines records for several streamflow-gaging stations, as in the station-year approach, and produces regional flood-frequency relations using an iterative regression technique. This technique eliminates the need to extrapolate the flood-frequency relation to the flood probability of interest. The resulting multiparameter regional flood-frequency relation is based on all the available annual peak-flow data. The method was applied to a group of records from 42 gaging stations in Nevada with many years of no flow and with many poorly defined flood-frquency relations. One- and two-parameter models were developed in which much of the variance in peak discharge is explained by drainage area. The log-Pearson type III and Weibull probability distributions were used in the models. Part of the error is directly assessed using randomly selected subsamples of the annual peak discharges. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydraulic Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9429(1992)118:6(868)","usgsCitation":"Hjalmarson, H., and Thomas, B.E., 1992, New look at regional flood-frequency relations for arid lands: Journal of Hydraulic Engineering, v. 118, no. 6, p. 868-886, https://doi.org/10.1061/(ASCE)0733-9429(1992)118:6(868).","startPage":"868","endPage":"886","numberOfPages":"19","costCenters":[],"links":[{"id":269427,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1061/(ASCE)0733-9429(1992)118:6(868)"},{"id":224855,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"118","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a65e3e4b0c8380cd72c87","contributors":{"authors":[{"text":"Hjalmarson, H. W.","contributorId":95872,"corporation":false,"usgs":true,"family":"Hjalmarson","given":"H. W.","affiliations":[],"preferred":false,"id":374733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, B. E.","contributorId":90767,"corporation":false,"usgs":true,"family":"Thomas","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":374732,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70014919,"text":"70014919 - 1992 - Methanogenic degradation kinetics of phenolic compounds in aquifer-derived microcosms","interactions":[],"lastModifiedDate":"2019-03-28T07:11:28","indexId":"70014919","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1003,"text":"Biodegradation","active":true,"publicationSubtype":{"id":10}},"title":"Methanogenic degradation kinetics of phenolic compounds in aquifer-derived microcosms","docAbstract":"<p class=\"Para\">In this segment of a larger multidisciplinary study of the movement and fate of creosote derived compounds in a sand-and-gravel aquifer, we present evidence that the methanogenic degradation of the major biodegradable phenolic compounds and concomitant microbial growth in batch microcosms derived from contaminated aquifer material can be described using Monod kinetics. Substrate depletion and bacterial growth curves were fitted to the Monod equations using nonlinear regression analysis. The method of Marquardt was used for the determination of parameter values that best fit the experimental data by minimizing the residual sum of squares. The Monod kinetic constants (μ<sub><span>&nbsp;</span><i class=\"EmphasisTypeItalic \">max</i><span>&nbsp;</span></sub>,<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">K</i><sub>s</sub>,<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">Y</i>, and<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">k</i><sub>d</sub>) that describe phenol, 2-, 3-, and 4-methylphenol degradation and concomitant microbial growth were determined under conditions that were substantially different from those previously reported for microcosms cultured from sewage sludge. The<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">K</i><sub>s</sub><span>&nbsp;</span>values obtained in this study are approximately two orders of magnitude lower than values obtained for the anaerobic degradation of phenol in digesting sewage sludge, indicating that the aquifer microorganisms have developed enzyme systems that are adapted to low nutrient conditions. The values for<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">k</i><sub>d</sub>are much less than<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">μ</i><sub>max</sub>, and can be neglected in the microcosms. The extremely low<span>&nbsp;</span><i class=\"EmphasisTypeItalic \">Y</i><span>&nbsp;</span>values, approximately 3 orders of magnitude lower than for the sewage sludge derived cultures, and the very low numbers of microorganisms in the aquifer derived microcosms suggest that these organisms use some unique strategies to survive in the subsurface environment.</p>","language":"English","publisher":"Kluwer Academic Publishers","doi":"10.1007/BF00114553","issn":"09239820","usgsCitation":"Godsy, E., Goerlitz, D., and Grbic-Galic, D., 1992, Methanogenic degradation kinetics of phenolic compounds in aquifer-derived microcosms: Biodegradation, v. 2, no. 4, p. 211-221, https://doi.org/10.1007/BF00114553.","productDescription":"11 p.","startPage":"211","endPage":"221","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":223954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205431,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00114553"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5543e4b0c8380cd6d18a","contributors":{"authors":[{"text":"Godsy, E.M.","contributorId":56685,"corporation":false,"usgs":true,"family":"Godsy","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":369606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":369605,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grbic-Galic, D.","contributorId":80824,"corporation":false,"usgs":true,"family":"Grbic-Galic","given":"D.","affiliations":[],"preferred":false,"id":369607,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70016833,"text":"70016833 - 1992 - The extent of temporal smearing in surface-temperature histories derived from borehole temperature measurements","interactions":[],"lastModifiedDate":"2023-11-17T17:39:56.779664","indexId":"70016833","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1844,"text":"Global and Planetary Change","active":true,"publicationSubtype":{"id":10}},"title":"The extent of temporal smearing in surface-temperature histories derived from borehole temperature measurements","docAbstract":"<p><span>The ability of borehole temperature data to resolve past climatic events is investigated using Backus-Gilbert inversion methods. Two experimental approaches are considered: (1) the data consist of a single borehole temperature profile, and (2) the data consist of climatically-induced temperature transients measured within a borehole during a monitoring experiment. The sensitivity of the data's resolving power to the vertical distribution of the measurements, temperature measurement errors, the inclusion of a local meteorological record, and the duration of a monitoring experiment, are investigated. The results can be used to help interpret existing surface temperature histories derived from borehole temperature data and to optimize future experiments for the detection of climatic signals.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0921-8181(92)90027-8","usgsCitation":"Clow, G.D., 1992, The extent of temporal smearing in surface-temperature histories derived from borehole temperature measurements: Global and Planetary Change, v. 6, no. 2-4, p. 81-86, https://doi.org/10.1016/0921-8181(92)90027-8.","productDescription":"6 p.","startPage":"81","endPage":"86","numberOfPages":"6","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":225032,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505babf1e4b08c986b323187","contributors":{"authors":[{"text":"Clow, Gary D. 0000-0002-2262-3853 clow@usgs.gov","orcid":"https://orcid.org/0000-0002-2262-3853","contributorId":2066,"corporation":false,"usgs":true,"family":"Clow","given":"Gary","email":"clow@usgs.gov","middleInitial":"D.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":374617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016718,"text":"70016718 - 1992 - Public-domain-software solution to data-access problems for numerical modelers","interactions":[],"lastModifiedDate":"2012-03-12T17:18:50","indexId":"70016718","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Public-domain-software solution to data-access problems for numerical modelers","docAbstract":"Unidata's network Common Data Form, netCDF, provides users with an efficient set of software for scientific-data-storage, retrieval, and manipulation. The netCDF file format is machine-independent, direct-access, self-describing, and in the public domain, thereby alleviating many problems associated with accessing output from large hydrodynamic models. NetCDF has programming interfaces in both the Fortran and C computer language with an interface to C++ planned for release in the future. NetCDF also has an abstract data type that relieves users from understanding details of the binary file structure; data are written and retrieved by an intuitive, user-supplied name rather than by file position. Users are aided further by Unidata's inclusion of the Common Data Language, CDL, a printable text-equivalent of the contents of a netCDF file. Unidata provides numerous operators and utilities for processing netCDF files. In addition, a number of public-domain and proprietary netCDF utilities from other sources are available at this time or will be available later this year. The U.S. Geological Survey has produced and is producing a number of public-domain netCDF utilities.","conferenceTitle":"Proceedings of the 2nd International Conference on Estuarine and Coastal Modeling","conferenceDate":"13 November 1992 through 15 November 1992","conferenceLocation":"Tampa, FL, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872628612","usgsCitation":"Jenter, H., and Signell, R., 1992, Public-domain-software solution to data-access problems for numerical modelers, Proceedings of the 2nd International Conference on Estuarine and Coastal Modeling, Tampa, FL, USA, 13 November 1992 through 15 November 1992, p. 72-82.","startPage":"72","endPage":"82","numberOfPages":"11","costCenters":[],"links":[{"id":224892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8febe4b0c8380cd7fa25","contributors":{"authors":[{"text":"Jenter, Harry","contributorId":36299,"corporation":false,"usgs":true,"family":"Jenter","given":"Harry","email":"","affiliations":[],"preferred":false,"id":374301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Signell, Richard","contributorId":73623,"corporation":false,"usgs":true,"family":"Signell","given":"Richard","affiliations":[],"preferred":false,"id":374302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016554,"text":"70016554 - 1992 - Residence times in river basins as determined by analysis of long-term tritium records","interactions":[],"lastModifiedDate":"2025-03-06T16:57:14.450633","indexId":"70016554","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Residence times in river basins as determined by analysis of long-term tritium records","docAbstract":"<p><span>The US Geological Survey has maintained a network of stations to collect samples for the measurement of tritium concentrations in precipitation and streamflow since the early 1960s. Tritium data from outflow waters of river basins draining 4500–75000 km</span><sup>2</sup><span>&nbsp;are used to determine average residence times of water within the basins. The basins studied are the Colorado River above Cisco, Utah; the Kissimmee River above Lake Okeechobee, Florida; the Mississippi River above Anoka, Minnesota; the Neuse River above Streets Ferry Bridge near Vanceboro, North Carolina; the Potomac River above Point of Rocks, Maryland; the Sacramento River above Sacramento, California; the Susquehanna River above Harrisburg, Pennsylvania. The basins are modeled with the assumption that the outflow in the river comes from two sources—prompt (within-year) runoff from precipitation, and flow from the long-term reservoirs of the basin. Tritium concentration in the outflow water of the basin is dependent on three factors: (1) tritium concentration in runoff from the long-term reservoir, which depends on the residence time for the reservoir and historical tritium concentrations in precipitation; (2) tritium concentrations in precipitation (the within-year runoff component); (3) relative contributions of flow from the long-term and within-year components. Predicted tritium concentrations for the outflow water in the river basins were calculated for different residence times and for different relative contributions from the two reservoirs. A box model was used to calculate tritium concentrations in the long-term reservoir. Calculated values of outflow tritium concentrations for the basin were regressed against the measured data to obtain a slope as close as possible to 1. These regressions assumed an intercept of zero and were carried out for different values of residence time and reservoir contribution to maximize the fit of modeled versus actual data for all the above rivers. The final slopes of the fitted regression lines ranged from 0.95 to 1.01 (correlation coefficient &gt; 0.96) for the basins studied. Values for the residence time of waters within the basins and average relative contributions of the within-year and long-term reservoirs to outflow were obtained. Values for river basin residence times ranged from 2 years for the Kissimmee River basin to 20 years for the Potomac River basin. The residence times indicate the time scale in which the basin responds to anthropogenic inputs. The modeled tritium concentrations for the basins also furnish input data for urban and agricultural settings where these river waters are used.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(92)90117-E","issn":"00221694","usgsCitation":"Michel, R.L., 1992, Residence times in river basins as determined by analysis of long-term tritium records: Journal of Hydrology, v. 130, no. 1-4, p. 367-378, https://doi.org/10.1016/0022-1694(92)90117-E.","productDescription":"12 p.","startPage":"367","endPage":"378","numberOfPages":"12","costCenters":[],"links":[{"id":489980,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.unl.edu/usgsstaffpub/434","text":"External Repository"},{"id":222910,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"130","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa974e4b0c8380cd85de2","contributors":{"authors":[{"text":"Michel, R. L.","contributorId":86375,"corporation":false,"usgs":true,"family":"Michel","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":373877,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016829,"text":"70016829 - 1992 - Analysis of geomagnetic secular variation during 1980-1985 and 1985- 1990, and geomagnetic models proposed for the 1991 revision of the International Geomagnetic Reference Field","interactions":[],"lastModifiedDate":"2024-04-24T11:15:40.730401","indexId":"70016829","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2310,"text":"Journal of Geomagnetism & Geoelectricity","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of geomagnetic secular variation during 1980-1985 and 1985- 1990, and geomagnetic models proposed for the 1991 revision of the International Geomagnetic Reference Field","docAbstract":"<div id=\"article-overiew-abstract-wrap\"><p class=\"global-para-14\">The secular variation of the main geomagnetic field during the periods 1980-1985 and 1985-1990 was analyzed in terms of spherical harmonics up to the eighth degree and order. Data from worldwide magnetic observatories and the Navy's Project MAGNET aerial surveys were used. The resulting pair of secular-variation models was used to update the Definitive Geomagnetic Reference Field (DGRF) model for 1980, resulting in new main-field models for 1985.0 and 1990.0. These, along with the secular-variation model for 1985-1990, were proposed for the 1991 revision of the International Geomagnetic Reference Field (IGRF).</p></div><div id=\"datarepo-wrap\"><br></div><div id=\"article-overiew-references-wrap\"><br></div>","language":"English","publisher":"J-STAGE","doi":"10.5636/jgg.44.735","usgsCitation":"Peddie, N., 1992, Analysis of geomagnetic secular variation during 1980-1985 and 1985- 1990, and geomagnetic models proposed for the 1991 revision of the International Geomagnetic Reference Field: Journal of Geomagnetism & Geoelectricity, v. 44, no. 9, p. 735-743, https://doi.org/10.5636/jgg.44.735.","productDescription":"9 p.","startPage":"735","endPage":"743","numberOfPages":"9","costCenters":[],"links":[{"id":479616,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.5636/jgg.44.735","text":"Publisher Index Page"},{"id":224949,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eb15e4b0c8380cd48bec","contributors":{"authors":[{"text":"Peddie, N.W.","contributorId":75911,"corporation":false,"usgs":true,"family":"Peddie","given":"N.W.","affiliations":[],"preferred":false,"id":374607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016579,"text":"70016579 - 1992 - Two-dimensional circulation modeling of the Pamlico River estuary, North Carolina","interactions":[],"lastModifiedDate":"2016-11-30T10:08:40","indexId":"70016579","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Two-dimensional circulation modeling of the Pamlico River estuary, North Carolina","docAbstract":"A two dimensional, vertically averaged, unsteady flow model was applied to a 50- kilometer reach of the Pamlico River estuary, North Carolina. The model computational grid, which consists of about 16,000 square cells, each 200 meters on a side, was developed from more than one million depth soundings. Information from a comprehensive data-collection network, including six water-level stations, six temperature and salinity measurement stations, and one wind measurement station, was used to provide data for boundary conditions and for model calibration. Preliminary model results for this ongoing study were sensitive to the presence of a lateral water-level gradient at the downstream boundary. For the simulation period, water-level oscillations at the downstream boundary were much more important in controlling Pamlico River flows than were local winds blowing over the surface of the estuary. Average absolute differences between observed and simulated water levels at two measurement sites were less than 2 centimeters for the 8-day calibration period.","conferenceTitle":"Proceedings of the 2nd International Conference on Estuarine and Coastal Modeling","conferenceDate":"13 November 1992 through 15 November 1992","conferenceLocation":"Tampa, FL, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872628612","usgsCitation":"Giese, G.L., and Bales, J., 1992, Two-dimensional circulation modeling of the Pamlico River estuary, North Carolina, Proceedings of the 2nd International Conference on Estuarine and Coastal Modeling, Tampa, FL, USA, 13 November 1992 through 15 November 1992, p. 607-619.","startPage":"607","endPage":"619","numberOfPages":"13","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":223063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Pamlico River estuary","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb992e4b08c986b327c7e","contributors":{"authors":[{"text":"Giese, G. L.","contributorId":44898,"corporation":false,"usgs":true,"family":"Giese","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":373946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bales, Jerad","contributorId":47390,"corporation":false,"usgs":true,"family":"Bales","given":"Jerad","affiliations":[],"preferred":false,"id":373947,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016849,"text":"70016849 - 1992 - Classifying and mapping wetlands and peat resources using digital cartography","interactions":[],"lastModifiedDate":"2012-03-12T17:18:52","indexId":"70016849","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Classifying and mapping wetlands and peat resources using digital cartography","docAbstract":"Digital cartography allows the portrayal of spatial associations among diverse data types and is ideally suited for land use and resource analysis. We have developed methodology that uses digital cartography for the classification of wetlands and their associated peat resources and applied it to a 1:24 000 scale map area in New Hampshire. Classifying and mapping wetlands involves integrating the spatial distribution of wetlands types with depth variations in associated peat quality and character. A hierarchically structured classification that integrates the spatial distribution of variations in (1) vegetation, (2) soil type, (3) hydrology, (4) geologic aspects, and (5) peat characteristics has been developed and can be used to build digital cartographic files for resource and land use analysis. The first three parameters are the bases used by the National Wetlands Inventory to classify wetlands and deepwater habitats of the United States. The fourth parameter, geological aspects, includes slope, relief, depth of wetland (from surface to underlying rock or substrate), wetland stratigraphy, and the type and structure of solid and unconsolidated rock surrounding and underlying the wetland. The fifth parameter, peat characteristics, includes the subsurface variation in ash, acidity, moisture, heating value (Btu), sulfur content, and other chemical properties as shown in specimens obtained from core holes. These parameters can be shown as a series of map data overlays with tables that can be integrated for resource or land use analysis.","largerWorkTitle":"ASTM Special Technical Publication","conferenceTitle":"International Symposium on Mapping and Geographic Information Systems","conferenceDate":"21 June 1990 through 22 June 1990","conferenceLocation":"San Francisco, CA, USA","language":"English","publisher":"Publ by ASTM","publisherLocation":"Philadelphia, PA, United States","issn":"10403094","usgsCitation":"Cameron, C., and Emery, D.A., 1992, Classifying and mapping wetlands and peat resources using digital cartography, <i>in</i> ASTM Special Technical Publication, no. 1126, San Francisco, CA, USA, 21 June 1990 through 22 June 1990, p. 195-206.","startPage":"195","endPage":"206","numberOfPages":"12","costCenters":[],"links":[{"id":224512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"1126","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f631e4b0c8380cd4c5ec","contributors":{"authors":[{"text":"Cameron, Cornelia C.","contributorId":103002,"corporation":false,"usgs":true,"family":"Cameron","given":"Cornelia C.","affiliations":[],"preferred":false,"id":374654,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emery, David A.","contributorId":107437,"corporation":false,"usgs":true,"family":"Emery","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":374655,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016552,"text":"70016552 - 1992 - Rhenium-osmium isotope systematics in meteorites I: Magmatic iron meteorite groups IIAB and IIIAB","interactions":[],"lastModifiedDate":"2023-12-09T01:07:23.354457","indexId":"70016552","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Rhenium-osmium isotope systematics in meteorites I: Magmatic iron meteorite groups IIAB and IIIAB","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id5\"><p>Using resonance ionization mass spectrometry (RIMS), Re and Os abundances were determined by isotope dilution (ID) and<span>&nbsp;</span><sup>187</sup>Os/<sup>186</sup>Os ratios measured in nineteen iron meteorites: eight from group IIAB, ten from group IIIAB, and Treysa (IIIB anomalous). Abundances range from 1.4 to 4800 ppb Re, and from 13 to 65000 ppb Os, and generally agree well with previous ID and neutron activation (NAA) results. The Re and Os data suggest that abundance trends in these iron groups may be entirely explained by fractional crystallization. Addition of late-formed metal to produce Re<img src=\"https://sdfestaticassets-us-east-1.sciencedirectassets.com/shared-assets/55/entities/sbnd.gif\" alt=\"single bond\" data-mce-src=\"https://sdfestaticassets-us-east-1.sciencedirectassets.com/shared-assets/55/entities/sbnd.gif\">Os variation in the B subgroups is not essential but cannot be excluded. Whole-rock isochrons for the IIAB and IIIAB groups are statistically indistinguishable. Pooled data yield an initial<span>&nbsp;</span><sup>187</sup>Os/<sup>186</sup>Os of 0.794 ± 0.010, with a slope of (7.92 ± 0.20) × 10<sup>−2</sup><span>&nbsp;</span>corresponding to a magmatic iron meteorite age of 4.65 ± 0.11 Ga (using a decay constant of 1.64 × 10<sup>−11</sup><span>&nbsp;</span>a<sup>−1</sup>). Given the errors in the slope and half life, this age does not differ significantly from the canonical chondrite age of 4.56 Ga, but could be as young as 4.46 Ga.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(92)90022-N","issn":"0012821X","usgsCitation":"Morgan, J.W., Walker, R., and Grossman, J.N., 1992, Rhenium-osmium isotope systematics in meteorites I: Magmatic iron meteorite groups IIAB and IIIAB: Earth and Planetary Science Letters, v. 108, no. 4, p. 191-202, https://doi.org/10.1016/0012-821X(92)90022-N.","productDescription":"12 p.","startPage":"191","endPage":"202","numberOfPages":"12","costCenters":[],"links":[{"id":222859,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"108","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aad37e4b0c8380cd86e65","contributors":{"authors":[{"text":"Morgan, J. W.","contributorId":92384,"corporation":false,"usgs":true,"family":"Morgan","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":373873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, R.J.","contributorId":105859,"corporation":false,"usgs":true,"family":"Walker","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":373874,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grossman, J. N.","contributorId":41840,"corporation":false,"usgs":true,"family":"Grossman","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":373872,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70016660,"text":"70016660 - 1992 - Mount St. Helens a decade after the 1980 eruptions: magmatic models, chemical cycles, and a revised hazards assessment","interactions":[],"lastModifiedDate":"2012-03-12T17:18:50","indexId":"70016660","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1109,"text":"Bulletin of Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"Mount St. Helens a decade after the 1980 eruptions: magmatic models, chemical cycles, and a revised hazards assessment","docAbstract":"Available geophysical and geologic data provide a simplified model of the current magmatic plumbing system of Mount St. Helens (MSH). This model and new geochemical data are the basis for the revised hazards assessment presented here. The assessment is weighted by the style of eruptions and the chemistry of magmas erupted during the past 500 years, the interval for which the most detailed stratigraphic and geochemical data are available. This interval includes the Kalama (A. D. 1480-1770s?), Goat Rocks (A.D. 1800-1857), and current eruptive periods. In each of these periods, silica content decreased, then increased. The Kalama is a large amplitude chemical cycle (SiO2: 57%-67%), produced by mixing of arc dacite, which is depleted in high field-strength and incompatible elements, with enriched (OIB-like) basalt. The Goat Rocks and current cycles are of small amplitude (SiO2: 61%-64% and 62%-65%) and are related to the fluid dynamics of magma withdrawal from a zoned reservoir. The cyclic behavior is used to forecast future activity. The 1980-1986 chemical cycle, and consequently the current eruptive period, appears to be virtually complete. This inference is supported by the progressively decreasing volumes and volatile contents of magma erupted since 1980, both changes that suggest a decreasing potential for a major explosive eruption in the near future. However, recent changes in seismicity and a series of small gas-release explosions (beginning in late 1989 and accompanied by eruption of a minor fraction of relatively low-silica tephra on 6 January and 5 November 1990) suggest that the current eruptive period may continue to produce small explosions and that a small amount of magma may still be present within the conduit. The gas-release explosions occur without warning and pose a continuing hazard, especially in the crater area. An eruption as large or larger than that of 18 May 1980 (???0.5 km3 dense-rock equivalent) probably will occur only if magma rises from an inferred deep (???7 km), relative large (5-7 km3) reservoir. A conservative approach to hazard assessment is to assume that this deep magma is rich in volatiles and capable of erupting explosively to produce voluminous fall deposits and pyroclastic flows. Warning of such an eruption is expectable, however, because magma ascent would probably be accompanied by shallow seismicity that could be detected by the existing seismic-monitoring system. A future large-volume eruption (???0.1 km3) is virtually certain; the eruptive history of the past 500 years indicates the probability of a large explosive eruption is at least 1% annually. Intervals between large eruptions at Mount St. Helens have varied widely; consequently, we cannot confidently forecast whether the next large eruption will be years decades, or farther in the future. However, we can forecast the types of hazards, and the areas that will be most affected by future large-volume eruptions, as well as hazards associated with the approaching end of the current eruptive period. ?? 1992 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Volcanology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00278003","issn":"02588900","usgsCitation":"Pallister, J., Hoblitt, R., Crandell, D.R., and Mullineaux, D.R., 1992, Mount St. Helens a decade after the 1980 eruptions: magmatic models, chemical cycles, and a revised hazards assessment: Bulletin of Volcanology, v. 54, no. 2, p. 126-146, https://doi.org/10.1007/BF00278003.","startPage":"126","endPage":"146","numberOfPages":"21","costCenters":[],"links":[{"id":205552,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00278003"},{"id":224796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ea5e4b0c8380cd70ba0","contributors":{"authors":[{"text":"Pallister, J.S.","contributorId":46534,"corporation":false,"usgs":true,"family":"Pallister","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":374157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoblitt, R.","contributorId":89536,"corporation":false,"usgs":true,"family":"Hoblitt","given":"R.","affiliations":[],"preferred":false,"id":374160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crandell, D. R.","contributorId":78385,"corporation":false,"usgs":true,"family":"Crandell","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":374159,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mullineaux, D. R.","contributorId":64248,"corporation":false,"usgs":true,"family":"Mullineaux","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":374158,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1003142,"text":"1003142 - 1992 - Survey of non-charter boat recreational fishing in the U.S. Virgin Islands","interactions":[],"lastModifiedDate":"2012-02-02T00:04:49","indexId":"1003142","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1106,"text":"Bulletin of Marine Science","active":true,"publicationSubtype":{"id":10}},"title":"Survey of non-charter boat recreational fishing in the U.S. Virgin Islands","docAbstract":"A telephone survey was conducted by the U.S. Virgin Islands Division of Fish and Wildlife from July- September 1986 to evaluate the efficacy of telephone surveys as a sampling technique for obtaining reliable  fisheries data, and to collect fisheries data for the recreational non-charter boat fishery around the Virgin  Islands. Results suggest that telephone surveys by themselves may provide biased data on recreational fishing in  the Virgin Islands. Additional methods, such as mail surveys and limited creel surveys could be used to  supplement the fisheries data gathered through telephone surveys. The results of this survey indicate that  during the mid 1980s 10.8% of the residents of the Virgin Islands ( similar to  10,800) fished recreationally (i.e.,  non-charter boat anglers). These anglers made modest demands of the resources (effort: 19,200 manhours/yr;","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Marine Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Jennings, C., 1992, Survey of non-charter boat recreational fishing in the U.S. Virgin Islands: Bulletin of Marine Science, v. 50, no. 2, p. 342-351.","productDescription":"pp. 342-351","startPage":"342","endPage":"351","numberOfPages":"10","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":133992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6887d5","contributors":{"authors":[{"text":"Jennings, Cecil A.","contributorId":38504,"corporation":false,"usgs":true,"family":"Jennings","given":"Cecil A.","affiliations":[],"preferred":false,"id":312819,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5222952,"text":"5222952 - 1992 - Survival of cackling Canada geese, 1982-1988","interactions":[],"lastModifiedDate":"2024-12-04T16:52:02.945038","indexId":"5222952","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Survival of cackling Canada geese, 1982-1988","docAbstract":"<p>We estimated seasonal and annual survival rates of cackling Canada geese (<i>Branta canadensis minima</i>) for the period 1982-1989 to identify periods of high mortality and assess effects of harvest management decisions. We tested hypotheses about age- and sex specific variation in survival, seasonal variation in survival rates, and variation in survival between years in which hunting seasons were open and closed. Geese were marked with individually identifiable neckbands and observed from autumn through spring. We used these data to estimate survival rates for 3-month periods in early (EW) and late (LW) winter and a 6-month period in summer (SU). Mean annual survival rates of immature females were lower than those of adults over the entire study. Survival rates of immature males were lower than those of adults during the 2 years with sport hunting seasons. We found no evidence of sex-specific differences in seasonal or annual survival rates of immature geese. Mean survival rates of adult males and females were similar during EW and LW, but there was evidence of higher survival of females during SU. Annual survival rates of adult females were higher than those of adult males. Mean annual survival rates of adult females and immatures of both sexes were lower in the years during which sport hunting was permitted. Tests for different survival rates in years before and after an agreement with the Eskimos to cease summer hunting yielded equivocal results.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3808791","usgsCitation":"Raveling, D.G., Nichols, J., Hines, J., Zezulak, D.S., Silveira, J.G., Johnson, J.C., Aldrich, T.W., and Weldon, J.A., 1992, Survival of cackling Canada geese, 1982-1988: Journal of Wildlife Management, v. 56, no. 1, p. 63-73, https://doi.org/10.2307/3808791.","productDescription":"11 p.","startPage":"63","endPage":"73","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487076,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3808791","text":"Publisher Index Page"},{"id":197689,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska, 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 \"}}]}","volume":"56","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688191","contributors":{"authors":[{"text":"Raveling, Dennis G.","contributorId":89443,"corporation":false,"usgs":true,"family":"Raveling","given":"Dennis","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":337543,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, James D. jnichols@usgs.gov","contributorId":139082,"corporation":false,"usgs":true,"family":"Nichols","given":"James D.","email":"jnichols@usgs.gov","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":337542,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hines, James E. jhines@usgs.gov","contributorId":3506,"corporation":false,"usgs":true,"family":"Hines","given":"James E.","email":"jhines@usgs.gov","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":337545,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zezulak, David S.","contributorId":24461,"corporation":false,"usgs":true,"family":"Zezulak","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":337544,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Silveira, Joseph G.","contributorId":65955,"corporation":false,"usgs":true,"family":"Silveira","given":"Joseph","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":337546,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Johnson, James C.","contributorId":78364,"corporation":false,"usgs":true,"family":"Johnson","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":337547,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Aldrich, Thomas W.","contributorId":88311,"corporation":false,"usgs":true,"family":"Aldrich","given":"Thomas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":337549,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Weldon, John A.","contributorId":85688,"corporation":false,"usgs":true,"family":"Weldon","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":337548,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70187411,"text":"70187411 - 1992 - Landsat thematic mapper products for rangeland assessment","interactions":[],"lastModifiedDate":"2017-05-02T11:38:50","indexId":"70187411","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1753,"text":"Geocarto International","active":true,"publicationSubtype":{"id":10}},"title":"Landsat thematic mapper products for rangeland assessment","docAbstract":"<p><span>Landsat Thematic Mapper (TM) data are useful for mapping rangeland resources worldwide. Spatial resolution and spectral characteristics of the data are adequate for performing a variety of range‐related tasks, including monitoring ecological change. The unique spectral characteristics of TM data are important in the development of products for manual interpretation of images to be used in rangeland assessment. Procedures were developed for using a histogram‐based, data‐dependent stretch of multispectml data values for producing site‐specific TM image products. The process optimizes image information for a given data set without a priori knowledge of the imaged site. Manual interpretation of TM products for rangeland assessment has many applications and will be aided by a standardized procedure for compositing spectral bands.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/10106049209354349","usgsCitation":"Haas, R.H., 1992, Landsat thematic mapper products for rangeland assessment: Geocarto International, v. 7, no. 1, p. 27-33, https://doi.org/10.1080/10106049209354349.","productDescription":"7 p.","startPage":"27","endPage":"33","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":340734,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59099ab2e4b0fc4e44915822","contributors":{"authors":[{"text":"Haas, Robert H.","contributorId":93388,"corporation":false,"usgs":true,"family":"Haas","given":"Robert","email":"","middleInitial":"H.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":693917,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70187578,"text":"70187578 - 1992 - Monitoring rangeland dynamics in Senegal with advanced very high resolution radiometer data","interactions":[],"lastModifiedDate":"2017-05-09T13:41:11","indexId":"70187578","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1753,"text":"Geocarto International","active":true,"publicationSubtype":{"id":10}},"title":"Monitoring rangeland dynamics in Senegal with advanced very high resolution radiometer data","docAbstract":"<p><span>Time‐series Normalized Difference Vegetation Index (NDVI) data, computed from Advanced Very High Resolution Radiometer data, are being used by regional and national programs in the African Sahel to monitor seasonal rangeland conditions. The data are often used as indicators of grazing conditions and drought. However, distinguishing rangelands from other vegetation cover types on NDVI images is difficult. A second complication is that rangeland types and their associated productivity vary geographically by soil type. To effectively assess rangeland conditions, seasonal fluctuations (due to climatic cycles) must be isolated from long‐term production characteristics associated with vegetation type and soil differences. Rangeland NDVI dynamics, including qualitative assessments of rangeland production, and the timing and length of the growing season in Senegal were examined by using 7.4‐km global area coverage satellite data. Analyses were based on 10‐day NDVI composite image data from 1982 through 1989. The NDVI image data were stratified by rangeland and soil polygons derived from locally available resource maps. Time‐series NDVI statistics were calculated from the resource polygons that had been interpreted into high, medium, and low production rangelands. Analysts monitoring rangeland conditions can better identify seasonal anomalies such as drought by comparing production potential within homogeneous; resource polygons with the current NDVI data.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/10106049209354356","usgsCitation":"Tappan, G.G., Tyler, D.J., Wehde, M.E., and Moore, D.G., 1992, Monitoring rangeland dynamics in Senegal with advanced very high resolution radiometer data: Geocarto International, v. 7, no. 1, p. 87-98, https://doi.org/10.1080/10106049209354356.","productDescription":"12 p.","startPage":"87","endPage":"98","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":341007,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5912d53ee4b0e541a03d4559","contributors":{"authors":[{"text":"Tappan, G. Gray 0000-0002-2240-6963 tappan@usgs.gov","orcid":"https://orcid.org/0000-0002-2240-6963","contributorId":3624,"corporation":false,"usgs":true,"family":"Tappan","given":"G.","email":"tappan@usgs.gov","middleInitial":"Gray","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":694622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tyler, Dean J. 0000-0002-1542-7539 dtyler@usgs.gov","orcid":"https://orcid.org/0000-0002-1542-7539","contributorId":4268,"corporation":false,"usgs":true,"family":"Tyler","given":"Dean","email":"dtyler@usgs.gov","middleInitial":"J.","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":false,"id":694623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wehde, M. E.","contributorId":191158,"corporation":false,"usgs":false,"family":"Wehde","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":694624,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moore, Donald G.","contributorId":41146,"corporation":false,"usgs":true,"family":"Moore","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":694625,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70195911,"text":"70195911 - 1992 - An aeromagnetic survey over the northwestern Ross Ice Shelf and the McMurdo Sound area","interactions":[],"lastModifiedDate":"2019-12-21T08:52:14","indexId":"70195911","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3097,"text":"Polarforschung","active":true,"publicationSubtype":{"id":10}},"title":"An aeromagnetic survey over the northwestern Ross Ice Shelf and the McMurdo Sound area","docAbstract":"<p><span>As part of the expedition GANOVEX VI 1990/91, the Bundesanstalt für Geowissenschaften und Rohstoffe (BGR), the Alfred Wegener Institute for Polar and Marine Research (AWI), and the United States Geological Survey (USGS) carried out an airborne magnetic survey over the northwestern Ross Ice Shelf and McMurdo Sound between Ross Island, the Transantarctic Mountains, and Minna Bluff.</span></p><p><span>The area planned for the aeromagnetic survey connects directly with the GANOVEX IV survey area (BGR &amp; USGS 1987, BACHEM et al. 1989a) which terminated along an approximately cast-west line at about the latitude of Cape Bird. The GANOVEX IV survey covered the Victoria Land Basin - which is the westernmost of the three north/south striking basins in the Ross Sea - from its northern end in the Terra Nova Bay region to its known southern end at Ross Island. A possible southem extension of the Victoria Land Basin and its central graben structure (the Terror Rift as found from seismic surveys (COOPER et al. 1987) and what has been referred to as Victoria Graben in the aeromagnetic interpretation of the GANOVEX IV data (BOSUM et al. 1989) was one of the major targets for this survey.</span></p><p><span>The survey was laid out in the form of blocks. A 135 km wide transect from the Transantarctic Mountains to about 175° W formed the focal block of the survey (Fig. 1) in which all major scientific objectives could be covered. Other survey blocks were planned to the south of this. During the course of the survey it turned out that in the time available no further area could be covered. Indeed, the unfavourable weather conditions made it impossible to complete even the above described main section fully.</span></p><p><span>In detail, the lay-out of the survey area was closely following that of the GANOVEX IV survey to assure compatibility and direct continuation between the two data sets.</span></p><p><span>The line spacing was chosen again to 4.4 km with a tic-line separation of 22 km. The survey altitude of 2,000 ft (610 m) corresponds to that of the Ross Sea section of the GANOVEX IV survey to which this survey area is directly adjacent. The profile lines were aligned approximately E-W, the tie-lines N-S.</span></p><p><span>As part of the survey area is covered by the maps of the USGS Antarctica Reconnaissance Series 1:250,000 the Lambert conformal conic projection used for these maps was also used for the preparation of a flight line grid.</span></p>","language":"English","publisher":"Alfred Wegener Institut für Polar- und Meeresforschung und Deutsche Gesellschaft für Polarforschung","publisherLocation":"Bremerhaven, Germany","doi":"10.2312/polarforschung.60.2.152","usgsCitation":"Damaske, D., Meyer, U., McCafferty, A.E., Behrendt, J., and Hoppe, H., 1992, An aeromagnetic survey over the northwestern Ross Ice Shelf and the McMurdo Sound area: Polarforschung, v. 60, no. 2, p. 152-156, https://doi.org/10.2312/polarforschung.60.2.152.","productDescription":"5 p.","startPage":"152","endPage":"156","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":352307,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Ross Ice Shelf, McMurdo Sound","volume":"60","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff2826e4b0da30c1bfd772","contributors":{"authors":[{"text":"Damaske, Detlef","contributorId":77384,"corporation":false,"usgs":true,"family":"Damaske","given":"Detlef","email":"","affiliations":[],"preferred":false,"id":730476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, Uwe","contributorId":1648,"corporation":false,"usgs":false,"family":"Meyer","given":"Uwe","email":"","affiliations":[],"preferred":false,"id":730477,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCafferty, Anne E. 0000-0001-5574-9201 anne@usgs.gov","orcid":"https://orcid.org/0000-0001-5574-9201","contributorId":1120,"corporation":false,"usgs":true,"family":"McCafferty","given":"Anne","email":"anne@usgs.gov","middleInitial":"E.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":730478,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Behrendt, John","contributorId":146726,"corporation":false,"usgs":false,"family":"Behrendt","given":"John","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":730479,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hoppe, Herbert","contributorId":14503,"corporation":false,"usgs":false,"family":"Hoppe","given":"Herbert","email":"","affiliations":[],"preferred":false,"id":730480,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70201439,"text":"wdrOK911 - 1992 - Water Resources Data, Oklahoma, Water Year 1991","interactions":[],"lastModifiedDate":"2021-01-26T20:47:36.870839","indexId":"wdrOK911","displayToPublicDate":"1991-01-01T10:50:08","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OK-91-1","title":"Water Resources Data, Oklahoma, Water Year 1991","docAbstract":"<p><span>Water resources data for the 1991 water year for Oklahoma consists of records of </span><span>stage, discharge, and water quality of streams; </span><span>stage, contents, and water quality </span><span>of lakes or reservoirs; and water levels of ground-water wells. </span><span>This report </span><span>contains discharge records for 131 gaging stations; stage and contents for 30 lakes </span><span>or reservoirs; water quality for 46 gaging stations and 2 lakes. </span><span>Also included are </span><span>11 partial-record stations and 27 ground-water sites. </span><span>These data represent that </span><span>part of the National Water Data System collected by the U.S. Geological Survey and </span><span>cooperating State and Federal agencies in Oklahoma.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrOK911","collaboration":"Prepared in cooperation with the State of Oklahoma and with other agencies","usgsCitation":"Blazs, R., Walters, D., Coffey, T., White, D., Boyle, D., and Kerestes, J., 1992, Water Resources Data, Oklahoma, Water Year 1991: U.S. Geological Survey Water Data Report OK-91-1, xiv, 449 p., https://doi.org/10.3133/wdrOK911.","productDescription":"xiv, 449 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,{"id":27105,"text":"wri904108 - 1991 - Hydrogeology of the surficial aquifer system, Dade County, Florida","interactions":[],"lastModifiedDate":"2021-10-14T12:09:26.947959","indexId":"wri904108","displayToPublicDate":"2021-10-13T11:05:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"90-4108","title":"Hydrogeology of the surficial aquifer system, Dade County, Florida","docAbstract":"An investigation of the surficial aquifer system in Dade County, begun in 1983, is part of a regional study of the aquifer system in southeastern Florida. Test drilling for lithologic samples, flow measurements during drilling, aquifer testing, and analyses of earlier data permitted delineation of the hydraulic conductivity distribution (on hydrogeologic sections), the aquifers in the system, the generalized transmissivity distribution, and interpretation of the ground-water flow system. \r\n\r\nThe surficial aquifer system, in which an unconfined ground-water flow system exists, is composed of the sediments from land surface downward to the top of a regionally extensive zone of sediments of low permeability called the intermediate confining unit. The aquifer system units, which vary in composition from clay-size sediments to cavernous limestone, are hydro stratigraphically divided into the Biscayne aquifer at the top; an intervening semiconfining unit that consists principally of clayey sand; a predominantly gray limestone aquifer in the Tamiami Formation in western and west-central Dade County; and sand or clayey sand near the base of the surficial aquifer system. The base of the surficial aquifer system ranges from a depth of about 175 to 210 feet below land surface in westernmost Dade County to greater than 270 feet in northeastern Dade County. Test drilling and aquifer-test data indicate a complex hydraulic conductivity distribution. Hydraulic conductivities of the very highly permeable zone of the Biscayne aquifer commonly exceed 10,000 feet per day; in the gray limestone aquifer, they range from 210 to 780 feet per day. \r\n\r\nTransmissivities of the surficial aquifer system vary locally but have a recognizable areal trend. Estimated values generally are about 300,000 feet squared per day or greater in nearly all of central and eastern Dade County. Transmissivity is lower to the west, decreasing to less than 75,000 feet squared per day in western Dade County. High transmissivity usually is associated with thick sections of the Fort Thompson Formation within the Biscayne aquifer. The gray limestone aquifer of the Tamiami Formation has transmissivities that range from 5,800 to 39,000 feet squared per day in western Dade County. The transition from high transmissivity to relatively low transmissivity is often only a few miles wide and coincides with the decrease in thickness of the very highly permeable Fort Thompson Formation, which marks the western boundary of the Biscayne aquifer. \r\n\r\nMore effective drainage as a result of extensive canal systems and large-scale pumping from municipal well fields has greatly altered the predevelopment flow system in eastern Dade County by: (1) eliminating or greatly reducing a seasonal and coastal ground-water ridge; (2) reducing deep circulation; (3) reducing or eliminating seasonal westward movement of ground water; (4) causing accelerated stormwater runoff and short ground-water flow paths; and (5) generally lowering the water table and inducing saltwater intrusion. Under predevelopment conditions in western Dade County, water entered the gray limestone aquifer by lateral movement from Broward and Collier Counties, and by downward seepage from The Everglades and the Biscayne aquifer, and moved southward and southeastward into Dade County to coastal discharge areas. Circulation in the Biscayne aquifer inland also was primarily to the south and southeast. In eastern Dade County, the seasonal ground-water ridge that formed under predevelopment conditions supported both easterly and westerly ground-water flow away from the ridge axis. This seasonal flow created a zone of lower dissolved solids.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri904108","usgsCitation":"Fish, J., and Stewart, M., 1991, Hydrogeology of the surficial aquifer system, Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 90-4108, v, 50 p., https://doi.org/10.3133/wri904108.","productDescription":"v, 50 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":2216,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4108/wri904108.pdf","text":"Report","size":"3.01 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 90-4108"},{"id":389208,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4108/wri904108_plates.pdf","text":"Plates 1-11","size":"11.5 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":159040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4108/coverthb.jpg"}],"country":"United States","state":"Florida","county":"Dade County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.79345703124999,\n              25.28443774698303\n            ],\n            [\n              -79.73876953124997,\n              25.28443774698303\n            ],\n            [\n              -79.72778320312499,\n              26.401710528707707\n            ],\n            [\n              -80.2001953125,\n              26.362342068998764\n            ],\n            [\n              -80.74951171874999,\n              26.43122806450644\n            ],\n            [\n              -80.79345703124999,\n              25.28443774698303\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa69d","contributors":{"authors":[{"text":"Fish, J.E.","contributorId":101658,"corporation":false,"usgs":true,"family":"Fish","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":197560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, M.T.","contributorId":6487,"corporation":false,"usgs":true,"family":"Stewart","given":"M.T.","email":"","affiliations":[],"preferred":false,"id":197559,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":54657,"text":"wdrMDDE911 - 1991 - Water resources data Maryland and Delaware, water year 1991, Volume 1. Surface-water data","interactions":[],"lastModifiedDate":"2021-01-22T19:39:39.320594","indexId":"wdrMDDE911","displayToPublicDate":"2021-01-22T14:50:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-91-1","displayTitle":"Water Resources Data Maryland and Delaware, Water Year 1991, Volume 1. Surface-Water Data","title":"Water resources data Maryland and Delaware, water year 1991, Volume 1. Surface-water data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE911","usgsCitation":"James, R., Hornlein, J., Simmons, R., and Strain, B., 1991, Water resources data Maryland and Delaware, water year 1991, Volume 1. 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,{"id":70179794,"text":"70179794 - 1991 - Water use data for public water suppliers and self supplied industry in Utah: 1988, 1989","interactions":[],"lastModifiedDate":"2017-01-19T09:21:42","indexId":"70179794","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5267,"text":"Utah Division of Water Rights Water-Use Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"8","title":"Water use data for public water suppliers and self supplied industry in Utah: 1988, 1989","docAbstract":"<p><span>This report is a summary of data collected under the Utah Water Use Program, a cooperative program between the Utah Division of Water Rights and the United States Geological Survey (USGS).</span></p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water 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,{"id":70179970,"text":"70179970 - 1991 - Ground-water conditions in Utah, spring of 1991","interactions":[],"lastModifiedDate":"2017-01-20T15:17:06","indexId":"70179970","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"31","title":"Ground-water conditions in Utah, spring of 1991","docAbstract":"<p>This is the twenty-eighth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, published cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.</p><p>This report, like the others in the series, contains information on well construction, ground-water withdrawal from wells, water-level changes, related changes in precipitation and streamflow, and chemical quality of water. Supplementary data, such as maps showing water-level contours, are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>This report includes individual discussions of selected major areas of ground-water development in the State for the calendar year 1990. Water-level fluctuations and selected related data, however, are described from the spring of 1986 to the spring of 1991. Much of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah, Division of Water Resources and Division of Water Rights","usgsCitation":"Herbert, L.R., Gates, J., Sory, J., Kariya, K.A., Eads, J.P., Smith, G.J., Thomas, B., Brooks, L.E., Garrett, R., Overman, W., Swenson, R., Emett, D.C., and Drumiler, M., 1991, Ground-water conditions in Utah, spring of 1991: Cooperative Investigations Report 31, vii, 92 p.","productDescription":"vii, 92 p.","numberOfPages":"100","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333622,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333621,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-174"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5883303be4b0d0023163781e","contributors":{"authors":[{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":659355,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sory, J.D.","contributorId":178510,"corporation":false,"usgs":false,"family":"Sory","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":659356,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kariya, Kim A.","contributorId":177522,"corporation":false,"usgs":false,"family":"Kariya","given":"Kim","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":659357,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Eads, James P.","contributorId":178506,"corporation":false,"usgs":false,"family":"Eads","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":659358,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smith, G. J.","contributorId":80767,"corporation":false,"usgs":true,"family":"Smith","given":"G.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":659359,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Thomas, B.K.","contributorId":177516,"corporation":false,"usgs":false,"family":"Thomas","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":659360,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Brooks, Lynette E. 0000-0002-9074-0939 lebrooks@usgs.gov","orcid":"https://orcid.org/0000-0002-9074-0939","contributorId":2718,"corporation":false,"usgs":true,"family":"Brooks","given":"Lynette","email":"lebrooks@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":659361,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Garrett, R. B.","contributorId":35810,"corporation":false,"usgs":true,"family":"Garrett","given":"R. B.","affiliations":[],"preferred":false,"id":659362,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Overman, W.R.","contributorId":178509,"corporation":false,"usgs":false,"family":"Overman","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":659363,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Swenson, R.L.","contributorId":178508,"corporation":false,"usgs":false,"family":"Swenson","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":659364,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Emett, D. C.","contributorId":21213,"corporation":false,"usgs":true,"family":"Emett","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":659365,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Drumiler, M.M.","contributorId":178512,"corporation":false,"usgs":false,"family":"Drumiler","given":"M.M.","affiliations":[],"preferred":false,"id":659366,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70179028,"text":"70179028 - 1991 - Ground-water resources and simulated effects of withdrawals in the Bountiful area, Utah","interactions":[],"lastModifiedDate":"2016-12-13T14:57:35","indexId":"70179028","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"95","title":"Ground-water resources and simulated effects of withdrawals in the Bountiful area, Utah","docAbstract":"<p>Ground-water resources in the Bountiful area, Utah, were studied to document changes in ground-water conditions and to simulate the effects of increased ground-water withdrawals and changes in recharge. The aquifer system is in basin-fill deposits and is primarily a confined system with unconfined parts along the mountain front.</p><p>Recharge to the aquifer system was estimated to range from about 22,000 to 32,000 acre-feet per year during 1947-85.&nbsp; Discharge was estimated to range from 26,000 to 30,000 acre-feet per year during 1947-85.</p><p>Long-term trends of ground-water levels indicate a steady decline at most observation wells from 1952 to 1962. Importation of surface water for irrigation in 1962 resulted in decreased ground-water withdrawals, causing water levels to rise. Water levels fluctuated from 1962 to 1985, depending on changes in withdrawals and precipitation.</p><p>A computer model of the aquifer system was constructed and calibrated using water-level data from 1946 and changes in ground-water withdrawals from 1947-86. Simulations of aquifer responses to projected withdrawals were based on a 50-percent increase in the 1981-85 rate of municipal and industrial withdrawals for 20 years using both average and less-than-average recharge rates. The simulations indicated water-level declines between 5 and 50 feet; a decrease in natural discharge to drains, by evapotranspiration, and to Great Salt Lake; and a decrease of ground water in storage after 20 years between 25,000 acre-feet using the average recharge rate, and 70,000 acre-feet using the less-than-average recharge rate.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Clark, D.W., 1991, Ground-water resources and simulated effects of withdrawals in the Bountiful area, Utah: Technical Publication 95, vi, 56 p.","productDescription":"vi, 56 p.","numberOfPages":"64","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332063,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-380"},{"id":332064,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/y920/y9200003.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Bountiful Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.12646484375,\n              40.68896903762434\n            ],\n            [\n              -112.12646484375,\n              41.0130657870063\n            ],\n            [\n              -111.6595458984375,\n              41.0130657870063\n            ],\n            [\n              -111.6595458984375,\n              40.68896903762434\n            ],\n            [\n              -112.12646484375,\n              40.68896903762434\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"585116bde4b08138bf1abd64","contributors":{"compilers":[{"text":"Clark, David W.","contributorId":77146,"corporation":false,"usgs":true,"family":"Clark","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":655822,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"authors":[{"text":"Clark, David W.","contributorId":77146,"corporation":false,"usgs":true,"family":"Clark","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":655821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54795,"text":"wdrNJ902 - 1991 - Water Resources Data, New Jersey, Water Year 1990. Volume 2. Ground-Water Data","interactions":[],"lastModifiedDate":"2012-07-17T01:01:41","indexId":"wdrNJ902","displayToPublicDate":"2012-01-01T15:22:58","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NJ-90-2","title":"Water Resources Data, New Jersey, Water Year 1990. Volume 2. Ground-Water Data","docAbstract":"Water Resources data for the 1990 water year for New Jersey consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. This volume of the report contains ground water levels for 218 observation wells and water-quality data for 176 wells. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in New Jersey.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"West Trenton, NJ","doi":"10.3133/wdrNJ902","collaboration":"Prepared in cooperation with the New Jersey Department of Environmental Protection and with other agencies.","usgsCitation":"Bauersfeld, W., Jones, W., and Pustay, E., 1991, Water Resources Data, New Jersey, Water Year 1990. Volume 2. Ground-Water Data: U.S. Geological Survey Water Data Report NJ-90-2, viii, 178 p., https://doi.org/10.3133/wdrNJ902.","productDescription":"viii, 178 p.","numberOfPages":"192","costCenters":[{"id":469,"text":"New Jersey Water Resources Division","active":false,"usgs":true}],"links":[{"id":260408,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1990/nj-90-2/report.pdf"},{"id":260409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1990/nj-90-2/report-thumb.jpg"}],"country":"United States","state":"New Jersey","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.58333333333333,38.916666666666664 ], [ -75.58333333333333,41.35055555555556 ], [ -73.88416666666667,41.35055555555556 ], [ -73.88416666666667,38.916666666666664 ], [ -75.58333333333333,38.916666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc673e4b08c986b32bf81","contributors":{"authors":[{"text":"Bauersfeld, W.R.","contributorId":72451,"corporation":false,"usgs":true,"family":"Bauersfeld","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":251584,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, W.D.","contributorId":68384,"corporation":false,"usgs":true,"family":"Jones","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":251583,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pustay, E.A.","contributorId":62604,"corporation":false,"usgs":true,"family":"Pustay","given":"E.A.","affiliations":[],"preferred":false,"id":251582,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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