Lower Pilarcitos Creek Groundwater Basin Study - Coastside ...
Lower Pilarcitos Creek Groundwater Basin Study - Coastside ...
Lower Pilarcitos Creek Groundwater Basin Study - Coastside ...
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Area above <strong>Pilarcitos</strong> <strong>Creek</strong> at Half Moon Bay Gauge<br />
A water balance was conducted for the area above the <strong>Pilarcitos</strong> <strong>Creek</strong> at Half<br />
Moon Bay gauge (Table 9, Column C). This balance includes the upper <strong>Pilarcitos</strong> <strong>Creek</strong><br />
watershed and provides an estimate of the groundwater outflow to the <strong>Lower</strong> <strong>Pilarcitos</strong><br />
<strong>Creek</strong> groundwater basin.<br />
Based on the isohyetal map (Figure 4), the average annual rainfall on the 17,069<br />
acre watershed is 34.08 inches (about 2.84 feet). No surface or subsurface inflow occurs<br />
in the watershed. After treatment at the Nunes Water Treatment Plant (WTP), minor<br />
amounts of imported water (77 AFY) are brought into the watershed from Crystal<br />
Springs Reservoir (see Appendix 6). Therefore, the total inflow to the <strong>Pilarcitos</strong> <strong>Creek</strong><br />
watershed is about 48,552 AFY or approximately 365 percent greater than the upper<br />
<strong>Pilarcitos</strong> <strong>Creek</strong> watershed.<br />
Because of the proximity to the coast (fog belt), the ET for the entire <strong>Pilarcitos</strong><br />
<strong>Creek</strong> watershed was assumed to be approximately five percent less than the average<br />
ET of the upper <strong>Pilarcitos</strong> <strong>Creek</strong> (76.5 percent) and Purisima <strong>Creek</strong> (74.8 percent)<br />
watersheds or about 71.5 percent. Accordingly, ET is estimated to be 34,660 AFY.<br />
Average streamflow for the <strong>Pilarcitos</strong> <strong>Creek</strong> at Half Moon Bay gauge station is<br />
11,543 AFY for the record between 1967 and 2001. Subsurface outflow cannot be<br />
readily measured and is estimated from the residual of the water balance. Based on<br />
records provided by the City of San Francisco (see Appendix 5), exported water from the<br />
watershed amounts to about 760 AFY. Other diversions include the <strong>Pilarcitos</strong> <strong>Creek</strong><br />
wellfield operated by CCWD (155 AFY) and <strong>Pilarcitos</strong> Lake diversions (913 AFY) (see<br />
Appendix 6). Therefore, the difference between the inflow (48,552 AFY) and outflow<br />
(48,031 AFY) suggests that 521 AFY is groundwater outflow. The undetected<br />
subsurface outflow for the <strong>Pilarcitos</strong> <strong>Creek</strong> watershed can also be estimated using<br />
Darcy’s Law (254 to 508 AFY). In terms of the surface water runoff coefficient for the<br />
<strong>Pilarcitos</strong> <strong>Creek</strong> watershed, calculations show that 0.68 AF/acre of water drains from the<br />
watershed.<br />
Precipitation at the Half Moon Bay Station ranges between 13.03 inches in 1972<br />
to 52.92 inches in 1983; the long-term average is 26.40 inches. Therefore, total inflow to<br />
the <strong>Pilarcitos</strong> <strong>Creek</strong> watershed could range between 23,985 (49.4 percent of average) in<br />
dry years to 97,347 (200.5 percent of average) in wet years. The total estimated<br />
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