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

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126 Groundwater Availability of the Central Valley Aquifer, California Table C2. Coordinates of the Central Valley Hydrologic Model grid. Corner of model grid Model coordinates X (column) - - - for purposes of this study, are less critical. In addition, to - patterns simulated. ( Temporal Discretization Model coordinates Y (row) Latitude (DMS) - Longitude (DMS) - Boundary Conditions Albers coordinates X (easting) (meters) Albers coordinates Y (northing) (meters) 1 1 1,890,733 Northeast 98 1 1,969,734 1 441 38,818 1,280,164 98 441 173,410 1,359,209 - - - - this chapter.
0 Suisun Bay 50 100 Miles 0 50 100 Kilometers Shaded relief derived from U.S. Geological Survey National Elevation Dataset, 2006. Albers Equal Area Conic Projection 1 3 2 6 4 5 9 7 8 11 10 12 13 12 14 EXPLANATION Model stream cell Model general-head boundary cell Active model boundary Water-balance subregion receiving non-routed deliveries Diversion location Inflow location Model Development 127 California Department of Water Resources water-balance subregions and identifier Figure C2. Distribution of general-head boundary cells and major streams and canals with streamflow-routing cells (including location of inflows and diversions). The water-balance subregions are described in . 16 15 19 17 18 20 21
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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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