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41014 results.

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Page 1456, results 36376 - 36400

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Not all publications have extents, not all extents are completely accurate
Habitat Suitability Index Models: Northern pintail
Willie J. Suchy, Stanley H. Anderson
1987, FWS/OBS 82/10.145
A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the northern pintail (Anas acuta). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum...
Habitat Suitability Index Models: Marsh wren
Kevin J. Gutzwiller, Stanley H. Anderson
1987, FWS/OBS 82/10.139
A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the marsh wren (Cistothorus palustris). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum...
Habitat Suitability Index Models: Muskellunge
Mark F. Cook, R. Charles Solomon
1987, FWS/OBS 82/10.148
A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the muskellunge (Esox masquinongy Mitchell). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum...
Habitat Suitability Index Models: Moose, Lake Superior region
Arthur W. Allen, Peter A. Jordan, James W. Terrell
1987, FWS/OBS 82/10.155
A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the moose (Alces alces). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum habitat)....
Habitat Suitability Index Models: Plains sharp-tailed grouse
Bart L. Prose
1987, FWS/OBS 82/10.142
A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the plains sharp-tailed grouse (Tympanuchus phasianellus jamesi). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to...
Habitat Suitability Index Models: Greater sandhill crane
Michael J. Armbruster
1987, FWS/OBS 82/10.140
A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the greater sandhill crane (Grus canadensis tabida). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to...
Habitat Suitability Index Models: Forster's tern (breeding) - Gulf and Atlantic coasts
Richard P. Martin, Phillip J. Zwank
1987, FWS/OBS 82/10.131
The nesting range of Forster's terns hosts three allopatric breeding populations. The first and most important breeding area, in terms of the number of nes t i ng pairs, includes the western guIf coas t from the Louisiana-Mississippi border to northern Tamaulipas, Mexico (American Ornithologists' Union [AOUJ 1983). In addition,...
Habitat Suitability Index Models: Hairy woodpecker
Patrick J. Sousa
1987, FWS/OBS 82/10.146
A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the hairy woodpecker (Picoides villosus). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum...
The phytoplankton component of seston in San Francisco Bay
S.M. Wienke, J. E. Cloern
1987, Netherlands Journal of Sea Research (21) 25-33
Phytoplankton biomass (as carbon) was estimated from chlorophyll a concentrations (Chla) and a mean value for the ratio of phytoplankton carbon to chlorophyll a in San Francisco Bay. The ratio was determined as the slope of a Model II regression of POC' against (Chla), where POC' is total particulate organic carbon minus sediment-associated non-phytoplankton...
North American nonmarine climates and vegetation during the Late Cretaceous
J. A. Wolfe, G.R. Upchurch Jr.
1987, Palaeogeography, Palaeoclimatology, Palaeoecology (61) 33-77
Analyses of physiognomy of Late Cretaceous leaf assemblages and of structural adaptations of Late Cretaceous dicotyledonous woods indicate that megathermal vegetation was an open-canopy, broad-leaved evergreen woodland that existed under low to moderate amounts of rainfall evenly distributed through the year, with a moderate increase at about 40–45°N. Many dicotyledons...
Spectral analysis of topography and gravity in the Basin and Range Province
Y. Ricard, C. Froidevaux, R. Simpson
1987, Tectonophysics (133) 175-187
A two-dimensional spectral analysis has been carried out for the topography and the Bouguer gravity anomaly of the Basin and Range Province in western North America. The aim was to investigate the possible presence of dominant wavelengths in the deformation pattern at the surface and at the depth of compensation....
Nucleation and triggering of earthquake slip: Effect of periodic stresses
James H. Dieterich
1987, Tectonophysics (144) 127-139
Results of stability analyses for spring and slider systems, with state variable constitutive properties, are applied to slip on embedded fault patches. Unstable slip may nucleate only if the slipping patch exceeds some minimum size. Subsequent to the onset of instability the earthquake slip may propagate well beyond the patch....
Fault failure with moderate earthquakes
M.J.S. Johnston, A. T. Linde, M. T. Gladwin, R. D. Borcherdt
1987, Tectonophysics (144) 189-206
High resolution strain and tilt recordings were made in the near-field of, and prior to, the May 1983 Coalinga earthquake (ML = 6.7, Δ = 51 km), the August 4, 1985, Kettleman Hills earthquake (ML = 5.5, Δ = 34 km), the April 1984 Morgan Hill earthquake (ML = 6.1, Δ = 55 km), the November 1984 Round Valley...
Origins of seawater intrusion in a coastal aquifer - A case study of the Pajaro Valley, California
L.D. Bond, J.D. Bredehoeft
1987, Journal of Hydrology (92) 363-388
Seawater may enter and contaminate stratified coastal aquifers through a number of different pathways. These pathways and their relative contribution are examined in the Pajaro Valley, California, a coastal area with extensive groundwater development. This study considers three pathways of possible intrusion of the primary confined aquifer: (1) onshore leakage...
Regional regression of flood characteristics employing historical information
Gary D. Tasker, J.R. Stedinger
1987, Journal of Hydrology (96) 255-264
Streamflow gauging networks provide hydrologic information for use in estimating the parameters of regional regression models. The regional regression models can be used to estimate flood statistics, such as the 100 yr peak, at ungauged sites as functions of drainage basin characteristics. A recent innovation in regional regression is the...
Analysis of saltwater upconing beneath a pumping well
T. E. Reilly, A.S. Goodman
1987, Journal of Hydrology (89) 169-204
Aquifer systems that contain freshwater and saltwater are usually stratified, with the more dense saltwater underlying the freshwater. A groundwater well discharging from the freshwater zone causes the saltwater to move upwards towards the well. This phenomenon is known as saltwater upconing. Two methods of analysis, the sharp-interface method and...
Analysis of an anisotropic coastal aquifer system using variable-density flow and solute transport simulation
W. R. Souza, C.I. Voss
1987, Journal of Hydrology (92) 17-41
The groundwater system in southern Oahu, Hawaii consists of a thick, areally extensive freshwater lens overlying a zone of transition to a thick saltwater body. This system is analyzed in cross section with a variable-density groundwater flow and solute transport model on a regional scale. The simulation is difficult, because...
The Morgan Hill, California, earthquake of April 24, 1984
Seena N. Hoose, editor(s)
1987, Bulletin 1639
The Morgan Hill earthquake, a moderate-size (M_g=6.1, ML =6.2, M=6.2) event, was felt throughout central California on April 24, 1984. The epicenter of the earthquake was located near Halls Valley southwest of Mount Hamilton, and the event is presumed to have occurred on the Calaveras fault. Damage, however, was concentrated near the south end of the Anderson Reservoir and in the town of Morgan Hill. A preliminary assessment by the California Office of Emergency Services estimated damage to private property at $7.0 million and to local-government facilities at $0.5 million, for a total of $7.5 million in damage. Acknowledgments.--! appreciate the helpful suggestions of Joseph I. Ziony and Robert D. Brown, Jr. These studies were aided by the generous cooperation of the many landowners who permitted access to their properties....
Computation of rapidly varied unsteady, free-surface flow
D.R. Basco
1987, Water-Resources Investigations Report 83-4284
Many unsteady flows in hydraulics occur with relatively large gradients in free surface profiles. The assumption of hydrostatic pressure distribution with depth is no longer valid. These are rapidly-varied unsteady flows (RVF) of classical hydraulics and also encompass short wave propagation of coastal hydraulics. The purpose of this report is...
Gravity profiles across the Uyaijah Ring structure, Kingdom of Saudi Arabia
M. E. Gettings, G. E. Andreasen
1987, Open-File Report 87-500
Three detailed gravity profiles across parts of the Uyaijah ring structure have been completed using an average station spacing of 260 M (giving a total of 217 gravity stations) and level surveys for elevation control. When combined with regional gravity-anomaly data, the profiles are adequate for construction of a structural...
Geohydrology and water quality of the Inyan Kara, Minnelusa, and Madison aquifers of the northern Black Hills, South Dakota and Wyoming, and Bear Lodge Mountains, Wyoming
D.P. Kyllonen, K. D. Peter
1987, Water-Resources Investigations Report 86-4158
The Inyan Kara, Minnelusa, and Madison aquifers are the principal sources of ground water in the northern Black Hills, South Dakota and Wyoming, and Bear Lodge Mountains, Wyoming. The aquifers are exposed in the Bear Lodge Mountains and the Black Hills and are about 3,000 to 5,000 ft below the...
Effect of reduced industrial pumpage on the migration of dissolved nitrogen in an outwash aquifer at Olean, Cattaraugus County, New York
M. P. Bergeron
1987, Water-Resources Investigations Report 85-4082
A quasi-three-dimensional digital groundwater flow model of a shallow outwash aquifer system at Olean, New York, was developed to study the effects of several pumping alternatives on groundwater flow and stream seepage. Nitrogen compounds have contaminated the aquifer in an industrial park in North Olean. Pumping from seven industrial production...