Hydrologic data, 1967. by California. Dept. of Water Resources.

Cover of: Hydrologic data, 1967. | California. Dept. of Water Resources.

Published by The Department in [Sacramento, Calif.] .

Written in English

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  • Hydrology -- California -- Statistics,
  • Water-supply -- California -- San Joaquin Valley

Edition Notes

Book details

SeriesBulletin / Department of Water Resources -- no. 130-67, Bulletin (California. Dept. of Water Resources) -- no. 130-67.
ContributionsGianelli, William R., Chastain, Cledith L., McIntyre, Victor B.
The Physical Object
Paginationx, 321 p. :
Number of Pages321
ID Numbers
Open LibraryOL22966194M

Download Hydrologic data, 1967.

This publication presents selected hydrologic data for the calendar year The data include monthly precipitation and runoff summaries for watersheds, 1967. book maximum discharges and annual maximum volumes of runoff for the watersheds for time intervals of.

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Book Editor(s): Glenn E. Stout. Search for more papers by this author. First on the continental and hemispheric scale gives new significance to the tracing of water movement through the hydrologic cycle. The traditional concept of tracers as limited tools to obtain data about micro‐areas within extensive aquifers (analogous to measuring Cited by: 6.

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66 This is the flood of record due to ice jam. Hydrologic Data, (Hardback) by Edward J Labrie, Glenn R Peterson and a great selection of related books, art and collectibles available now at jointhedotszine.com Biographical Sketches of Committee Members KENNETH R. BRADBURY (Chairman) is a research hydrogeologist/professor with the Wisconsin Geological and Natural History Survey, University of Wisconsin-Extension, in Madison.

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Geological Survey publishes a series of manuals describing procedures for planning and conducting specialized work in water- resources investigations.

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Additional books from the extended shelves. Inthe U.S. Water Resources Council presented a coherent approach to flood frequency with Bulletin 15, “A Uniform Technique for Determining Flood Flow Frequencies.” The method it recommended involved fitting the log-Pearson Type III distribution to annual peak flow data by the method of jointhedotszine.com by: A hydrologic model is a simplification of a real-world system (e.g., surface water, soil water, wetland, groundwater, estuary) that aids in understanding, predicting, and managing water resources.

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International Yearbook Cartography, 7, The HEC-RAS approach consists of a combination of the surface hydrologic model and the digital terrain model data.

This combination allows thereafter. Full text of "Hydrologic data, Appendix A: Climatological data" See other formats.

25 Chapter 3 COLLECTION OF HYDROLOGIC DATA STREAMFLOW Continuous streamflow records a r e obtained a t a gaging s t a t i o n a t which t h e stream stage (water-surface o r is recorded continuously. h e i g h t above some datum) i s e i t h e r r e a d f r e q u e n t l y D i s c h a r g e i s measured, u s u a l l y by c u r r e n t m e t e r, Only t h e g e n e r a l a t v a r i o u s.

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The study of hydrologie processes or systems uses historical data collected from natural phenomena which are observed once, and only once, and probably will not be observed again under exactly the Models of the Hydrologic Cycle | SpringerLinkCited by: 5. The U.S. Geological Survey, in cooperation with Federal, State, and local agencies, maintains a long-term network of hydrologic monitoring stations in Kansas.

In water yearthis network included real-time streamgages. A water year is the month period from October 1 through September Analysis and modeling of the characteristics and regionalization of hydrologic data in which both the spatial and the temporal components are simultaneously considered has recently received increased attention.

Two problems related to the analysis of spatial-temporal data are discussed in this jointhedotszine.com by: 1. References for Ground Water Data or Model Report Submittals & Sources of Information for Required Data References & Citations A review of previously submitted ground water data and model reports was conducted, and a list of commonly used references was complied to serve as a starting place to find information required by Scale ,; 1 in.

equals approx. 8 miles. "Lambert conformal conic projection based on standard parallels 33⁰ and 45⁰." Relief shown by spot heights. "Base map drainage modified in " Base map "Compiled in Edition of " Includes text, table of hydrologic units, and inset.

Available also through the Library of Congress Web site as a raster image. AACR2. In these cases the characteristics, suitably defined, are revealed by the distortion of the tritium pulses in precipitation, which occur when water is passing through the reservoirs.

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Journal of Hydrology, 68 () Elsevier Science Publishers B.V., Amsterdam -- Printed in The Netherlands IDENTIFICATION AND PREDICTION OF NONLINEAR HYDROLOGIC SYSTEMS BY THE FILTER-SEPARATION AUTOREGRESSIVE (AR) METHOD: EXTENSION TO HOURLY HYDROLOGIC DATA MIKIO HINO*l and MASAHIKO HASEBE.2 Department of Civil Engineering, Cited by: Manuals in the Techniques of Water-Resources Investigations series, which are listed below, are available TWRI book 3, chap.

12 p. 3-A3. Book 4. Hydrologic Analysis and Interpretation Section A. Statistical Analysis 4-A1. data forms.

The hydrologist shall record daily field hydrological testing activities. The hydrologist shall record hydrologic data on appro-priate data forms as described in the appendices to Date Issued Supersedes Issue To Be Reviewed By Page No.

NOVEMBER JULY NOVEMBER ' 4 of 12 C A (R). Experimental Examination of the Rational Method. Rainfall and runoff data collected in Baltimore, Maryland, from 20 gaged urban drainage areas ranging in size up to acres have been used in a study of the Rational Method.

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Ralston Creek drains approximately three square miles of present-day eastern Iowa City, land that was farmed when studies commenced.

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