Hydrogeologic Framework of the Puget Sound Aquifer System, Washington and British Columbia Volume 1424, PT. 4
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Hydrogeologic Framework of the Puget Sound Aquifer System, Washington and British Columbia Volume 1424, PT. 4

Hydrogeologic Framework of the Puget Sound Aquifer System, Washington and British Columbia Volume 1424, PT. 4


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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1998-06-01 Excerpt: ...for mean annual values to estimate annual recharge values. The problem is due to the fact that annual precipitation values may be outside of the range in values used to develop the regression relations (tables 4 and 5). This is the case for many of the precipitation values at the Port Townsend site. This particular problem is mainly related to small precipitation values (the limitations for large precipitation values were described previously). The major aspect suggested by this limitation is the need to estimate recharge in a small-precipitation area for both types of deposits using daily water-budgeting methods for a long simulation period. This would provide additional information for (1) developing more accurate relations and (2) improving the understanding of the interannual variability in recharge in this climatic setting. However, although annual precipitation within the Puget Sound Lowland may be much smaller than the smallest value used to develop the relations, small values may not be a major limitation because the mean annual precipitation is more than about 16 in/yr everywhere in the Puget Sound Lowland and is more than 27 in/yr in most of the Puget Sound Lowland. The relation between the interannual variability of precipitation and recharge and the subsequent response of water levels because of recharge variations was recognized early in the Puget Sound Lowland by Walters and Kimmel (1968) and Anderson (1968). Walters and Kimmel (1968) show that the timing and magnitude of the winter peak in water levels is related to both differences and trends in annual precipitation. Walters and Kimmel (1968) further show that seasonal water-level changes can have annual differences of at least 4 ft; for 1945-50, there was a positive trend in precipita...


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Product Details
  • ISBN-13: 9781235949593
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 48
  • Spine Width: 3 mm
  • Width: 189 mm
  • ISBN-10: 1235949591
  • Publisher Date: 01 May 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 104 gr


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Hydrogeologic Framework of the Puget Sound Aquifer System, Washington and British Columbia Volume 1424, PT. 4
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