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Lower Pilarcitos Creek Groundwater Basin Study - Coastside ...

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ET can be expressed in terms of percent precipitation. For the Purisima <strong>Creek</strong><br />

watershed, 74.8 percent of the precipitation on the upper Purisima <strong>Creek</strong> watershed is<br />

removed from the watershed by ET. The surface water runoff coefficient for the Purisima<br />

<strong>Creek</strong> watershed is 0.76 AF/acre, consistent with the bedrock geology of the watershed.<br />

Area above the <strong>Pilarcitos</strong> <strong>Creek</strong> below Stone Dam Gauge<br />

A second regional water balance was conducted for the watershed above the<br />

<strong>Pilarcitos</strong> <strong>Creek</strong> below Stone Dam gauge (Table 9, Column B). The results of the water<br />

balance for this area are similar to the results estimated for the Purisima <strong>Creek</strong><br />

watershed.<br />

The average annual precipitation on the 4,090 acre watershed is 38.98 inches<br />

(about 3.25 feet). No surface or subsurface inflow occurs in the watershed and no water<br />

is imported into the watershed. Therefore, the total inflow to the upper <strong>Pilarcitos</strong> <strong>Creek</strong><br />

watershed is about 13,284 AFY or approximately 27 percent greater than the upper<br />

Purisima <strong>Creek</strong> watershed, comparable to the difference in areas (23 percent).<br />

Precipitation that falls on the upper <strong>Pilarcitos</strong> <strong>Creek</strong> watershed drains toward the<br />

Pacific Ocean and eventually passes the gauge stations on <strong>Pilarcitos</strong> <strong>Creek</strong> as surface<br />

water or groundwater. ET becomes an unknown quantity to be derived as the residual or<br />

remaining quantity of water after all other water balance components are itemized and<br />

accounted. Change in storage is assumed to be zero.<br />

Average streamflow for the <strong>Pilarcitos</strong> <strong>Creek</strong> below Stone Dam gauge station is<br />

about 2,339 AFY for the record between 1997 and 2001. The undetected subsurface<br />

outflow for the upper <strong>Pilarcitos</strong> <strong>Creek</strong> watershed is about 23 AFY (1 percent). Based on<br />

records provided by the City of San Francisco (see Appendix 5), diversions from<br />

<strong>Pilarcitos</strong> <strong>Creek</strong> amount to about 760 AFY. Therefore, the difference between the inflow<br />

(13,284 AFY) and outflow (3,122 AFY) suggests that 10,162 AFY is removed by ET and<br />

deep percolation.<br />

ET as a percent of precipitation is 76.5 percent, similar to the 74.8 percent ET<br />

estimated for the upper Purisima <strong>Creek</strong> watershed. The surface water runoff coefficient<br />

for the upper <strong>Pilarcitos</strong> <strong>Creek</strong> watershed is 0.76 AF/acre, consistent with the bedrock<br />

geology of the watershed.<br />

32

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