Written in EnglishRead online
Includes bibliographical references (p. 69-70)
|Other titles||Precipitation runoff and streamflow routing models for the Willamette River Basin, Oregon|
|Statement||by Antonius Laenen and John C. Risley ; prepared in cooperation with Oregon Department of Environmental Quality|
|Series||Water-resources investigations report -- 95-4284|
|Contributions||Risley, John C, Geological Survey (U.S.), Oregon. Dept. of Environmental Quality|
|The Physical Object|
|Pagination||vii, 197 p. :|
|Number of Pages||197|
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Everyday low prices and free delivery on eligible : Antonius Laenen. This chapter describes how the constructed basin hydrologic models can be used in water-quality analysis; using descriptions of the watershed and Precipitation-Runoff and Streamflow-Routing Modeling as a Foundation for Water-Quality Simulation in the Willamette River Basin, Oregon.
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Everyday low prices and free delivery on eligible : Antonius Laenen. Precipitation-Runoff Modeling System (PRMS) BibliographyPrecipitation-runoff and streamflow-routing models for the Willamette River Basin, Oregon: U.S.
Geological Survey Water-Resources Investigations Report70 p.Estimates of Ground-Water Recharge, Base Flow, and Stream Reach Gains and Losses in the Willamette. References Cited. Anderson, C.W Rounds, S.A.,Occurrence of selected trace elements and organic compounds and their relation to land use in the Willamette River basin, Oregon, U.S.
Geological Survey WaterPrecipitation-runoff and streamflow-routing models for the Willamette River basin, Oregon: U.S. Geological. Analysis of the Augrainstorm and storm runoff to the South Platte River in the southern Denver metropolitan area, Colorado / (Lakewood, Colo.: U.S.
Dept. of the Interior, Geological Survey ; Denver, CO: For sale by Open-File Services Section, U.S. Geological Survey, MSWestern Distribution Branch, [i.e. ]), by. Klamath Basin Poster Project. 2 pages. Lecture Notes.
17 pages. Mitigating Geologic Hazards in Oregon. 64 pages. Study Guide. 2 pages. Research Paper. 18 pages. Seismic Hazards. 13 pages. Syllabus. 4 pages. Lecture Notes. 40 pages. Study Guide. 11 pages. Study Guide. 3 pages. Influence of the Missoula Floods. 31 pages. Overview of the Precipitation-runoff and streamflow-routing models for the Willamette River Basin.
Laenen, Antonius: Precipitation-runoff and streamflow-routing models for the Willamette River Basin, Oregon / (Portland, Or.: U.S. Dept. of the Interior, U.S.
Geological Survey ; Denver, Colo.: Branch of Information Services [distributor], ), also by John C. Risley and Oregon.
Department of Environmental Quality (page images at HathiTrust). Laenen A, Risley JC () Precipitation-runoff and streamflow-routing models for the Willamette River basin, Oregon.
U.S. Geological Survey Water Resources Investigations Report pp Google ScholarAuthor: Ellen Wohl. Request PDF | Climate Change and Stream Temperature in the Willamette River Basin: Implications for Fish Habitat | This study examined the effects of climate change on stream temperature in 12 sub.
In a larger simulation study, in which precipitation–runoff models were calibrated for sub-basins encompassing the ent km 2 Willamette River Basin, Chang and Jung () found groundwater to be a critical parameter in accurately Cited by: Precipitation-Runoff and Streamflow-Routing Models for the Williamette River Basin Modeling surface and ground water mixing in the hyporheic zone.
The Yakima is one of the early test-cases for this framework. Willamette River basin: While the Spokane and Yakima Basins are the two that we are primarily focusing on for the WISDM project, we are in the process of developing a framework to upscale the RHESSys model for implementation over the Willamette River basin as well.
Tague C, Grant GE () A geological framework for interpreting the low‐flow regimes of Cascade streams, Willamette River Basin, Oregon. Water Resour Res 40(4). doi: /WR Tague C, Grant GE () Groundwater dynamics mediate low‐flow response to global warming in snowdominated alpine by: 4.
Runoff from Snowmelt The following report, from the Corps of Engineers North Pacific Division,may be over a half century old, but it contains considerable information about the thermodynamics of snow and the mechanics of snowmelt.
The temperature. The Willamette is a gravel-bed river that drains ~28, square kilometers between the Coast Range and Cascade Range in northwestern Oregon before entering the Columbia River near Portland.
In the last years, natural and anthropogenic drivers have altered the sediment transport regime, drastically reducing the geomorphic complexity of the. Full text of "Selected water resources abstracts" See other formats. GIS systems, water, resources. 75 FR - Regulated Navigation Areas; Port of Portland Terminal 4, Willamette River, Portland, OR.
Federal Register, 77 FR - Safety Zone; Grain-Shipment Vessels, Columbia and Willamette Rivers. Federal Register, AA00 Safety Zone. HESS Hydrology and Earth System Sciences HESS Hydrol. Earth Syst. Sci. Copernicus Publications Göttingen, Germany /hess Quantifying uncertainty in urban flooding analysis considering hydro-climatic projection and urban development effects Jung I.-W.
2 1 Chang H. 1 Moradkhani H. 2 1 Department of Geography, Portland State. Randall, D. A., Wood, R. A., Bony, S., Colman, R., Fichefet, T., Fyfe, J., Kattsov, V., Pitman, A., Shukla, J., Srinivasan, J., Stouffer, R. J., Sumi, A., and Taylor Cited by: the Abstract Book - Hydrophiles` Water Research.
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Library of Congress Cataloging-in-Publication Data Modeling phosphorus in the environment / editors, David E. Radcliﬀe, Miguel L. Cabrera. ISBN (alk. Free essays, homework help, flashcards, research papers, book reports, term papers, history, science, politics.
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Willamette River Basin Review. The study will determine if modifying the operation and maintenance of the system of 13 Corps reservoirs In the interest of flood control, fish & wildlife conservation, municipal & industrial water supply, and development of additional recreational interests would better serve current and anticipated future water.
Groundwater and surface water interaction is an essential component of the hydrological cycle. The hydraulic connectivity and exchange of water between surface water (e.g. rivers, lakes, wetlands) and underlying aquifers provide many ecosystem.
They noted that for continuous-time, basin large-scale water quality models, collecting and manipulating the input data are more time-consuming and cumbersome due to the "method of disaggregation of the model", whose subdivisions are based on topographic boundaries.
a run-of-the-river hydroelectric reservoir on the Snake River, Oregon. Read Microsoft Word - text version. The linked model simulations were evaluated against historic data and two current models for the region. Historic river flows were adequately reproduced by the linked model.
Additionally, an investigation of the linked model's sensitivity to low river flow. Scribd is the world's largest social reading and publishing site.