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

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CUMULATIVE DEPARTURE OF STREAMFLOW DIVERSION, IN ACRE-FEET PER YEAR<br />

300<br />

200<br />

100<br />

0<br />

-100<br />

-200<br />

Cool (Negative) Warm (Positive)<br />

Cool<br />

(Negative)<br />

"Variable"<br />

to<br />

Dry<br />

"Variable"<br />

to<br />

Wet<br />

-<br />

<br />

<br />

<br />

<br />

<br />

<br />

). In addition,<br />

<br />

<br />

Dry Wet<br />

Dry<br />

TIME, IN YEARS<br />

Groundwater<br />

Hydrogeology 47<br />

"Variable"<br />

to<br />

Dry<br />

1960 1965 1970 1975 1980 1985 1990 1995 2000 2005<br />

Cool<br />

(Negative)<br />

EXPLANATION<br />

Periods of Pacific Decadal Oscillation [PDO]<br />

(Mantua, 2006)<br />

Bear River Diversion cumulative departure average<br />

Cumulative annual temperature difference, 1964-2003<br />

Pacific Decadal Oscillation (PDO) average annual value<br />

Figure A19. Cumulative departure of streamflow diversions from the Bear River by South Sutter Water District, California; cumulative<br />

annual temperature from California Irrigation Management Information System’s (CIMIS) stations at Davis <strong>and</strong> the Pacific Decadal<br />

Oscillation (PDO) index, 1960–2004.<br />

Wet<br />

-2.0<br />

-4.0<br />

-6.0<br />

<br />

<br />

<br />

<br />

<br />

<br />

-<br />

<br />

<br />

6.0<br />

4.0<br />

2.0<br />

0.0<br />

CUMULATIVE ANNUAL TEMPERATURE DIFFERENCE, IN DEGREES FAHRENHEIT<br />

PDO-INDEX, UNITLESS

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