Central Valley Aquifer, Chapters A and B - MAE Class Websites
Central Valley Aquifer, Chapters A and B - MAE Class Websites Central Valley Aquifer, Chapters A and B - MAE Class Websites
46 Groundwater Availability of the Central Valley Aquifer, California Surface Water - ( - ). North much smaller ( - - acre-ft/yr ( ). - - ). ). - - - - - but also is controlled by other factors. These factors may
CUMULATIVE DEPARTURE OF STREAMFLOW DIVERSION, IN ACRE-FEET PER YEAR 300 200 100 0 -100 -200 Cool (Negative) Warm (Positive) Cool (Negative) "Variable" to Dry "Variable" to Wet - ). In addition, Dry Wet Dry TIME, IN YEARS Groundwater Hydrogeology 47 "Variable" to Dry 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005 Cool (Negative) EXPLANATION Periods of Pacific Decadal Oscillation [PDO] (Mantua, 2006) Bear River Diversion cumulative departure average Cumulative annual temperature difference, 1964-2003 Pacific Decadal Oscillation (PDO) average annual value Figure A19. Cumulative departure of streamflow diversions from the Bear River by South Sutter Water District, California; cumulative annual temperature from California Irrigation Management Information System’s (CIMIS) stations at Davis and the Pacific Decadal Oscillation (PDO) index, 1960–2004. Wet -2.0 -4.0 -6.0 - 6.0 4.0 2.0 0.0 CUMULATIVE ANNUAL TEMPERATURE DIFFERENCE, IN DEGREES FAHRENHEIT PDO-INDEX, UNITLESS
- Page 13 and 14: Figure B12. Map of altitude of the
- Page 15 and 16: Figure C28. Pie chart and histogram
- Page 17 and 18: Conversion Factors Inch/Pound to SI
- Page 19 and 20: Chapter A. Introduction, Overview o
- Page 21 and 22: - - precipitation. -
- Page 23 and 24: 40° 39° 38° 37° 36° 35° Klama
- Page 25 and 26: Texture Model DATA Centralized Geos
- Page 27 and 28: Hydrology Water Well Information Aq
- Page 29 and 30: Table A1. Water-balance subregions
- Page 31 and 32: B Red Bluff 0 50 100 Miles 0 50 100
- Page 33 and 34: Delta and Eastside Streams ).
- Page 35 and 36: for about 30 percent of the annual
- Page 37 and 38: 0 50 100 Miles 0 50 100 Kilometers
- Page 39 and 40: A Coast Ranges Clayey lenses Fault
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- Page 43 and 44: C DEPTH TO MIDPOINT OF INCREMENT, I
- Page 45 and 46: ). The southern part, referred , in
- Page 47 and 48: 3-D Model of Percentage of Coarse-G
- Page 49 and 50: A Layer 1 EXPLANATION Central Valle
- Page 51 and 52: C Layer Corcoran Clay EXPLANATION C
- Page 53 and 54: E Layer 9 EXPLANATION Central Valle
- Page 55 and 56: Geomorphic province— Basin Delta
- Page 57 and 58: San Joaquin Valley ),
- Page 59 and 60: - Water supplied from aquifers
- Page 61 and 62: C Figure A16. Continued. 3.54% 5.45
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46 Groundwater Availability of the <strong>Central</strong> <strong>Valley</strong> <strong>Aquifer</strong>, California<br />
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but also is controlled by other factors. These factors may