Central Valley Aquifer, Chapters A and B - MAE Class Websites

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178 Groundwater Availability of the Central Valley Aquifer, California B (Cont.) SIMULATED SUBSIDENCE, IN FEET 26 1960 1970 1980 1990 2000 2010 Figure C21. Continued. 7 0 10 20 7 0 10 20 23S/25E-16N4 24S/26E-34F1 EXPLANATION Simulated subsidence Measured subsidence 25S/26E-1A2 26 1960 1970 1980 1990 2000 2010 26 26 1960 1970 1980 1990 2000 2010 1960 1970 1980 1990 2000 2010 7 0 10 20 26S/23E-16H3 26 26 1960 1970 1980 1990 2000 2010 1960 1970 1980 1990 2000 2010 7 0 10 20 24S/26E-36A2 23S/25E-16N3 WATER YEAR WATER YEAR 7 0 10 20 7 0 10 20 7 0 10 20 32S/28E-20Q1 26 26 1960 1970 1980 1990 2000 2010 1960 1970 1980 1990 2000 2010 7 0 10 20 26S/23E-16H2
- - ), they likely - - - Pumpage Observations - - - Model Calibration and Sensitivity 179 ). In particular, the trends are matched. The simulation matches closely in drier the proportions and total 21 million acre-ft of annual farm (1989). - - ). This most likely is a contradict this. Water-Use Observations most of the factors used in its calculation are indirect measure- - - some cases, is less than those estimated by Williamson (1982). ), the amount of
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GROUNDWATER RESOURCES PROGRAM Groun
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Groundwater Availability of the Cen
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Foreword An adequate supply of grou
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Contents Chapter A Introduction, Ov
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Chapter C Numerical Model of the Hy
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Figures Chapter A Figure A1. Map of
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Figure B12. Map of altitude of the
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Figure C28. Pie chart and histogram
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Conversion Factors Inch/Pound to SI
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Chapter A. Introduction, Overview o
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- - precipitation. -
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40° 39° 38° 37° 36° 35° Klama
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Texture Model DATA Centralized Geos
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Hydrology Water Well Information Aq
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Table A1. Water-balance subregions
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B Red Bluff 0 50 100 Miles 0 50 100
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Delta and Eastside Streams ).
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for about 30 percent of the annual
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0 50 100 Miles 0 50 100 Kilometers
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A Coast Ranges Clayey lenses Fault
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- the distribution of these pro
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C DEPTH TO MIDPOINT OF INCREMENT, I
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). The southern part, referred , in
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3-D Model of Percentage of Coarse-G
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A Layer 1 EXPLANATION Central Valle
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C Layer Corcoran Clay EXPLANATION C
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E Layer 9 EXPLANATION Central Valle
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Geomorphic province— Basin Delta
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San Joaquin Valley ),
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- Water supplied from aquifers
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C Figure A16. Continued. 3.54% 5.45
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CUMULATIVE DEPARTURE OF PRECIPITATI
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CUMULATIVE DEPARTURE OF STREAMFLOW
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700 500 600 400 200 160 0 50 100 Mi
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B 0 50 100 Miles 0 50 100 Kilometer
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Water Budget per year (
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References Cited 55 -
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References Cited 57 - - 2009, at
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60 Groundwater Availability of the
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