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Bulletin 1.pdf - California Department of Water Resources - State of ...

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346 WATER RESOURCES OF CALIFORNIA<br />

RUNOFF<br />

Estimated mean seasonal natural run<strong>of</strong>f <strong>of</strong> the Central Valley Area<br />

for the 53 years from 1894-95 to 1946-47 is 33,636,000 acre-feet, or 47.5<br />

percent <strong>of</strong> total surface run<strong>of</strong>f from mountain and foothill lands in the<br />

<strong>State</strong>. The minimum seasonal flow <strong>of</strong> 9,280,000 acre-feet occurred in<br />

1923-24, and the maximum, totalling 63,300,000 acre-feet, in 1906-07. The<br />

10-year period from 1923-24 to 1932-33 was the driest <strong>of</strong> record in this<br />

Area. Run<strong>of</strong>f during each <strong>of</strong> those 10 years, except 1926-27, was less than<br />

the 53-year mean, and the average was only 66.3 percent <strong>of</strong> this long-time<br />

mean.<br />

Run<strong>of</strong>f from drainage basins <strong>of</strong> the Central Valley Area is derived<br />

largely from snow. Consequently, the major portion <strong>of</strong> seasonal run<strong>of</strong>f<br />

comes during late spring and early summer months from March to June,<br />

inclusive. For Sacramento River the run<strong>of</strong>f during these months is 42.8<br />

percent <strong>of</strong> the seasonal total, for American River, 65.4 percent, and for<br />

Kings River, 71.8 percent. Minimum run<strong>of</strong>f comes from August to<br />

October, inclusive, flow for this period being 9.7 percent <strong>of</strong> total seasonal<br />

run<strong>of</strong>f for Sacramento River, 2.1 percent for the American, and 5.5 percent<br />

for the Kings. Sacramento River drains a region <strong>of</strong> porous lava<br />

formation, with large underground storage capacity. Summer flow <strong>of</strong><br />

the Sacramento is therefore better sustained than is that <strong>of</strong> other streams<br />

in the Area.<br />

An indication <strong>of</strong> variation in monthly flow <strong>of</strong> Central Valley Area<br />

streams, and <strong>of</strong> the percentage <strong>of</strong> seasonal run<strong>of</strong>f that comes during .<br />

each month, is given by data for Sacramento River at Red Bluff, American<br />

River at Fair Oaks and Kings River at Piedra listed in Table 59.<br />

The first records <strong>of</strong> stream flow in the Central Valley Area were<br />

obtained by Wm. Ham. Hall, <strong>State</strong> Engineer from 1878 to 1884. The<br />

only stream gaging station then maintained in the Sacramento River<br />

Basin was at Collinsville, at the mouth <strong>of</strong> the Sacramento. In the San<br />

Joaquin River Basin 20 gaging stations were maintained, most <strong>of</strong> them<br />

at the base <strong>of</strong> the foothills. All stations established by <strong>State</strong> Engineer<br />

Hall were discontinued after 1884, when the <strong>of</strong>fice <strong>of</strong> <strong>State</strong> Engineer<br />

was abolished. As <strong>of</strong> September 30, 1947, records from 96 stations were<br />

published by the United <strong>State</strong>s Geological Survey in the Sacramento<br />

River Basin and 105 in the San Joaquin River Basin.<br />

The first gaging station established in the Sacramento River Basin<br />

by the Geological Survey wa,

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