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

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172 Groundwater Availability of the Central Valley Aquifer, California B Stony Creek Cache Creek Putah Cr ek 0 50 100 Miles 0 50 100 Kilometers Shaded relief derived from U.S. Geological Survey National Elevation Dataset, 2006. Albers Equal Area Conic Projection Figure C19. Continued. Stanislaus Tuolumne Merced San Joaquin STREAMFLOW GAIN LOSS Fresno San Joaquin Fresno Slough EXPLANATION Groundwater/surface-water interaction, in acre-feet per year Kings River Less than -500 -500 to -100 -99.9 to -25 Active model grid boundary Model water-balance subregions Kaweah River -24.9 to 0 0.1 to 25 25.1 to 100 100.1 to 500 Greater than 500 Kern River Out of groundwater system Into groundwater system
- - - - (- Boundary Flow Observations - Model Calibration and Sensitivity 173 - Subsidence Observations - - and ). - - ). - - ). Uplift also ). pared to estimated-subsidence maps. The simulated subsidence ( and - ). In part, this subsidence likely is caused by the the measured declines, in these areas.
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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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Manuscript appproved on April 16, 2
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