3 edition of Flood peaks and discharge summaries in the Delaware River basin found in the catalog.
Flood peaks and discharge summaries in the Delaware River basin
Arthur A Vickers
|Statement||by Arthur A. Vickers, Harry A. Farsett, and J. Wayne Green ; prepared in cooperation with the U.S. Army Corps of Engineers, Philadelphia District ; United States Department of the Interior, Geological Survey|
|Series||Open-file report -- 81-912, Open-file report (Geological Survey (U.S.)) -- 81-912|
|Contributions||Farsett, Harry A, Green, J. Wayne, United States. Army. Corps of Engineers. Philadelphia District, Geological Survey (U.S.)|
|The Physical Object|
|Pagination||1 v. :|
Federal Highway Administration: Computation of backwater and discharge at width constrictions of heavily vegetated flood plains / ([Bay St. Louis, Miss.]: U.S. Geological Survey, ), also by Verne R. Schneider and Geological Survey (U.S.) (page images at HathiTrust). Delmarva Peninsula -- the Nanticoke River watershed and the Coastal Bays watershed. The Nanticoke watershed covers an area approximately square miles in size, encompassing parts of Dorchester, Wicomico, and Caroline Counties. Major tributaries of the Nanticoke River drainage basin are Marshyhope, Rewastico, Quantico, and Wetipquin Creeks.
The Lackawanna drains into the Susquehanna River as do multiple heavily mined small watersheds, while the Schuylkill drains into the Delaware River. Anthracite coal was discovered in this region in the s and first shipped down the Susquehanna River in , reaching peak production in Much of the mining was done through deep-mining Cited by: 2. The Lower Tidal Schuylkill down to the confluence with the Delaware River ( miles) 3. The Delaware River from the confluence up to the Philadelphia City Boundary ( miles) The pontoon vessel was operated during the summer/fall and spring /summer season. In total during the fiscal , the pontoon vessel removed a total of
2. The Lower Tidal Schuylkill down to the confluence with the Delaware River ( miles) 3. The Delaware River from the confluence up to the Philadelphia City Boundary ( miles) During fiscal year , the pontoon vessel was operated 5 times. 3 trips during the summer/fall removed a total of cubic yards of mixed trash from the non. example, the weighted (Qw) and regression (Qr) yr flood discharge at station are 9, cfs, respectively, and the regression estimate (Qu) at the ungaged location is 9, cfs. The adjusted yr flood discharge at the ungaged location on the Northwest Branch of the Anacostia River is computed to be 9, cfsFile Size: 7MB.
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Get this from a library. Flood peaks and discharge summaries in the Delaware River basin. [Arthur A Vickers; Harry A Farsett; J Wayne Green; United States. Army. Corps of Engineers. Philadelphia District.; Geological Survey (U.S.)]. sw Availability of Techniques and Methods 4-B5, Guidelines for Determining Flood Flow Frequency, Bulletin 17C; sw Peak Flow File: Status and plans for resolving cleanup effort and an opportunity to preview a new report: The U.S.
Geological Survey Peak-Flow File Data Verification Project, ; sw Identification, Correction, and Revision of Discharges Measured with SxS Pro. The storm extended from Fort Ross on the coast to the Feather River basin.
LaPorte, in the Feather River basin, had 1, mm ( in) of rain in 20 days, an event with a return period of 12, years. The flood episodes of and in California resulted in an overhaul.
voir system, the Kansas River Basin is the largest basin under flood control in the Mississippi River Basin. Eighteen reservoirs, which have a total flood-control capacity of 7, acre-feet, provide flood protec tion within the basin and along the Missouri River downstream.
From April 1 to August 1,the resFile Size: 4MB. Harold A. Thomas Jr., and M. Fiering Mathematical synthesis of streamflow sequences for the analysis of river basins by simulation Harvard Univ. Press David K. Todd, and K. Ateshian Estimation of flood peaks in the Sierra Nevada mountains, California Univ.
of Calif Report SeriesNo. 1 United States Army Corps Of Engineers. Our results indicated that with the CMC method, the downstream flood risk caused by the Min River flood was, and % for the1, and 2% design floods of the Jinsha River.
Full text of "Flood flow frequency for ungaged watersheds: a literature evaluation" See other formats. A dimensionless index is introduced, referred to as the flood number (N F), which indicates a basin's flood control capability.
Peak discharge data for all 40 sub-basins of the studied watershed. The Online Books Page. Browsing subject area. analyses from selected sites with discharge data in the Hudson River basin,by year.
[Site locations are shown in fig. 10, names are given in table 7. Dash indicates no data available] Year Number of Samples Site 13 Site 27a Site 27b Site 28 Site 32 Site 45 12 25 1 12 10 12 12 26 - 12 11 14 12 25 - 12 12 13 12 The Brazos River basin is one of the most diverse river basins in the state, spanning six ecoregions; rainfall conditions that vary from a mean average of six inches per year in headwater areas to more than 50 inches per year near its mouth (HDR ).
The Brazos River flows for 1, milesFile Size: 45MB. Colorado River Basin, due to its longevity and its early adoption (in ) by the Reclamation-led consortium. BCSD was developed in the early s to produce regional climate data that are consistent with the observed historical weather and climate, and the long-term, large-scale climate change signal predicted by GCMs.
Sillimanite, a white to tan to green aluminum silicate, (Al 2 SiO 5) occurs in high temperature, aluminum-rich metamorphic Delaware, it is found in the Hoopes Reservoir and Brandywine Springs areas.
Inthe Delaware General Assembly, acting on a proposal by the Delaware Mineralogical Society, established sillimanite as the Delaware State Mineral. Full text of "Water quality status report: Kootenay (Kootenai) River Basin, British Columbia, Montana, and Idaho" See other formats S Knudsont Ken Water quality M26wask status report WATER QUALITY STATUS REPORT Kootenay (Kootenai) River Basin British Columbia, Montana and Idaho Prepared ton The Kootenai River Network Prepared by: Ken Knudson Ecological Resource.
Please read our short guide how to send a book to Kindle. flood penalty environmental instructor programming simulation additional file select weap constraints http click weather student iowa optimal assessment river basin evaluation regulation demand This book is the successor to the Water Quality Criteria Report of the National Technical Advisory Committee to the Secretary of the Interior in Yale University Mr.
RALPH FORCES, Delaware River Basin Commission Dr. LESLIE M. REID, Texas A & M University Dr. MICHAEL B. SONNEN, Water Resources Engineers, Inc.
ROBERT O. SYLVESTER. The computation of floodways on rivers in coastal floodplains should be based on the year flood discharge and elevations of the rivers only and should terminate at the boundary of the V, VE, or V zone or where the mean high tide exceeds the year flood elevation from a riverine-only flood, whichever occurs further upstream.
Surf ace-Water-Quality Assessment of ^i^Mfc-UiJfci **' Yakima ___ River ___Basin, Washington Distribution of Pesticides and Other Organic Compounds in Water, Sediment, and Aquatic Biota, U.S.
Department of the InteriorAuthor: Joseph F. Rinella, Stuart W. McKenzie, J. Kent Crawford, William T. Foreman, Gregory J. Fuhrer, Jenn. Welcome to the Connecticut Department of Energy and Environmental Protection's website. The staff at DEEP is dedicated to conserving, improving, and protecting our natural resources and the environment, and increasing the availability of cheaper, cleaner, and more reliable energy.
Ecologically-important medium and high flow peaks (lost from the system through river regulation) can be achievedby combining environmental water with consumptive Basin: A source book of ecological knowledge’, CSIRO Land and Water, Technical Report 30/00, recruitment in rivers with modified discharge depends on the interacting effects.
Topic 1 Hydrology and fluvial geomorphology The drainage basin system Discharge relationships within drainage basins River channel processes and landforms The human impact Topic 2.The USRW is located in the Northeast U.S.
and in the context of New Jersey, It is situated in the southern portion of the State completely within Salem County ().The USRW consists of an approximately 36 km 2, out of which 68% consists of agricultural land, 12% wetlands, 11% forest, 8% urban, and remainders are water and barren land (USDA-NASS, ).Author: Subhasis Giri, Richard G.
Lathrop, Christopher C. Obropta.CASE STUDY: MCOttiNG HEAVY METALS TRANSPORT IN THE FLINT RIVER Introduction Description of Flint River Study Site Flint River August Survey August Survey Data Summary August Survey Node) Calibration " August Survey Sensitivity Analysis Flint River December Survey