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SURFACE WATER SUPFLY of the UNITED STATEP

SURFACE WATER SUPFLY of the UNITED STATEP

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<strong>SURFACE</strong> <strong>WATER</strong> SUPPLY OF SOUTH ATLANTIC SLOPE AMD EASTERN GULF OF MBnCO J8A8T"t. 1945 '<br />

SCOPE OP WORK<br />

IBils volume 19 one <strong>of</strong> a series <strong>of</strong> 14 reports presenting results <strong>of</strong> measurements <strong>of</strong>,<br />

stage and flow made on streams, lakes, and reservoirs in <strong>the</strong> United States during <strong>the</strong><br />

water year ending September 30, 1945. The 1 work was begun In 1888 In oonaectlor with<br />

special studies relating to Irrigation. Measurements <strong>of</strong> <strong>the</strong> flow <strong>of</strong> streams arfl <strong>of</strong> <strong>the</strong><br />

stage and contents <strong>of</strong> lakes and reservoirs have been made at about 10,300 gaglrg stations<br />

i<br />

In <strong>the</strong> 48 ^tates tad also at many in <strong>the</strong> Territories <strong>of</strong> Alaska and Hawaii. In July.l945y<br />

5,600 gaging stations, including those in Hawaii, were being maintained by tl» Geological<br />

Survey and cooperating organizations. Miscellaneous discharge measurements wer« made<br />

during <strong>the</strong> water year at many o<strong>the</strong>r, points.<br />

In <strong>the</strong> execution <strong>of</strong> <strong>the</strong> work many State and private organizations have cooppratedi,<br />

ei<strong>the</strong>r by furnishing data or by assisting in collecting data. Cooperation <strong>of</strong> <strong>the</strong> first<br />

kind is acknowledged In connection with <strong>the</strong> description <strong>of</strong> each station affected; cooper­<br />

ation <strong>of</strong> <strong>the</strong> second kind is acknowledged, under <strong>the</strong> heading "Cooperation," ln^ <strong>the</strong> iotror<br />

ductory matter that precedes <strong>the</strong> gaging-station records in each volume. In tlr present<br />

volume, <strong>the</strong> section on cooperation <strong>of</strong> <strong>the</strong> second kind appears on pajge 11.<br />

DEFINITION OF TERMS<br />

The units in which stream-flow data are presented in this report and o<strong>the</strong>r terms used<br />

herein are defined as follows:<br />

"Second-feet11 Is an abbreviation for 'cubic feet per second." A seconds-foot is <strong>the</strong><br />

rate <strong>of</strong> discharge <strong>of</strong> a stream whose channel Is 1 square foot in cross-sectional area and<br />

whose average velocity is 1 foot per second.<br />

/ "Second-feet per square mile" is <strong>the</strong> average number <strong>of</strong> cubic feet '<strong>of</strong> vater flowing tfer<br />

second from each square mile <strong>of</strong> area drained, on <strong>the</strong> assumption that <strong>the</strong> run<strong>of</strong>f 18 dis­<br />

tributed uniformly both as regards time and area. \<br />

"Run<strong>of</strong>f in inches* Is <strong>the</strong> depth to which an area' would be covered if all <strong>the</strong> water<br />

draining from it in a given period were uniformly distributed on its surface. It is used<br />

for comparing run<strong>of</strong>f with rainfall, which is usually expressed in inches.<br />

An ^acte-foot* is <strong>the</strong> quantity <strong>of</strong> water required to cover an a.ere to tJnie depth <strong>of</strong><br />

1 foot and Is equivalent to 43,560 cubic feet. The term ts commonly usefl In connection<br />

with storage for irrigation.<br />

"Second-root-day" is <strong>the</strong> volume <strong>of</strong> water represented by a flow <strong>of</strong> T second-foot for 24 '<br />

* . *<br />

hours. It Is equivalent to 86,400 cubic fjest, 1.983471 acre-feat, or 646,317 'nlloos and<br />

represents a run<strong>of</strong>f <strong>of</strong> 0.0372 inch from 1 square mile.<br />

"Stage-discharge relation" la an abbreviation' for <strong>the</strong> term "relation betweer gage height<br />

arid discharge." .<br />

"Control" is a term used to designate a feature downstream from <strong>the</strong> gage thnt determines<br />

<strong>the</strong> stage-discharge relation at <strong>the</strong> gage, nils feature nay be a natural section, a reach,<br />

<strong>of</strong> th* channel, or an artificial structure. . . .

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