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

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162 Groundwater Availability of the Central Valley Aquifer, California 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 EXPLANATION Model calibration— Location of stream segments used for model calibration Location of wells used for model calibration Location of subsidence measurements used for model calibration Central Valley model boundary Water-balance subregion Figure C15. Distribution of calibration data (groundwater levels, gains and losses of streamflow, and subsidence observations).
Water-Level Altitudes, Water-Level Altitude Changes, and Water-Level Altitude Maps http://waterdata.usgs. gov and ). simulation period. - on the basis of perforation depths, completeness of record, - ( parameter estimation. tudes at a particular time, it is necessary to accurately simu- Model Calibration and Sensitivity 163 in the northern part of the study area, increased dramatically in - - 10 7 10 ft 2 for the 42.5-year simulation period - possibly represent errors in the databases, measurements that ). In
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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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