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Chapter 6 <br />Water Supply Characterization <br />THE CITY OF <br />PL£ASANTON <br />Zone 7's latest modeling forecasts future average yields from Arroyo Valle to Zone 7 at approximately <br />5,500 AFY, using historical hydrology adjusted for climate change impacts. Previous planning documents, <br />including Zone 7's 2015 UWMP, assumed an average yield of 7,300 AFY, and the ten-year calendar year <br />average (2011-2020) has been 3,500 AFY; local climate change effects on the watershed—specifically a <br />net average reduction in precipitation—are expected to reduce the yield over time. Construction of the <br />Chain of Lakes Arroyo Valle diversion structure and pipeline will allow Zone 7 to capture more of the storm <br />releases from Lake Del Valle and likely increase the yield from this water supply in the future. The <br />conservative average yield estimate of 5,500 AFY is consistent with the 2019 WSE Update; it will be <br />re-evaluated as more climate change downscaled information is developed and as the Chain of Lakes <br />projects progress. <br />6.2.1.2.3 Local Storage <br />Zone 7 has two existing local storage options: Lake Del Valle and the Main Basin. Lake Del Valle stores <br />both runoff from the Arroyo Valle watershed and imported surface water deliveries from the SWP. Zone 7 <br />can store up to about 7,500 AF of its share of Arroyo Valle runoff in the lake; runoff collected in any given <br />year is required to be delivered to Zone 7 by the end of the following year. The Main Basin is used <br />conjunctively and is artificially recharged with SWP water. Zone 7 relies on the operational storage <br />capacity of 126,000 AF in the Main Basin. Section 6.2.2.1 provides additional information on the <br />Main Basin. <br />6.2.1.2.4 Non -Local Storage <br />In addition to local storage, Zone 7 also participates in the two non -local (also called "out -of -basin") <br />groundwater banking programs described below; both banks are located in Kern County. Note that while <br />these banking programs provide a water source during drought years, they represent water previously <br />stored from Zone 7's surface water supplies during wet years. Therefore, they do not have a net <br />contribution to Zone 7's water supply over the long-term and in fact result in some operational losses as <br />described below. While the out -of -basin groundwater banks significantly enhance system reliability, this <br />banked water supply requires Banks Pumping Plant in the Delta and the SBA to be operational; low SWP <br />Table A allocations (and generally low levels of water movement in the SWP system) can limit the delivery <br />of these banked supplies via exchange. Figure 6-1 shows the historical operation of the Kern County <br />banks—note the successful use of the groundwater banks to augment water supplies during the recent <br />drought, and the recovery in the following years. <br />Point of Delivery Agreements with DWR and Kern County Water Agency, a SWP contractor, allow Zone 7 <br />to store SWP water in and recover water from Semitropic Water Storage District (Semitropic) and Cawelo <br />Water District (Cawelo). Semitropic and Cawelo are member units of Kern County Water Agency, which <br />manages water deliveries to these agencies. Zone 7 has been storing water in the water banks operated <br />by Semitropic since 1998 and by Cawelo since 2006. In November 2020, the Zone 7 Board of Directors <br />(Zone 7 Board) authorized the execution of amendments to existing Point of Delivery Agreements that <br />would extend water delivery terms for storage in Semitropic and Cawelo through 2030 and recovery of <br />banked water through 2035. <br />WEST YOST 6-6 City of Pleasanton <br />2020 Urban Water Management Plan <br />May 2021 <br />