Potential effects of global warming on the Sacramento/San Joaquin watershed and the San Francisco estuary
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Abstract
California's primary hydrologic system, the San Francisco estuary and its upstream watershed, is vulnerable to the regional hydrologic consequences of projected global climate change. Projected temperature anomalies from a global climate model are used to drive a combined model of watershed hydrology and estuarine dynamics. By 2090, a projected temperature increase of 2.1°C results in a loss of about half of the average April snowpack storage, with greatest losses in the northern headwaters. Consequently, spring runoff is reduced by 5.6 km3(∼20% of historical annual runoff), with associated increases in winter flood peaks. The smaller spring flows yield spring/summer salinity increases of up to 9 psu, with larger increases in wet years.
Study Area
Publication type | Article |
---|---|
Publication Subtype | Journal Article |
Title | Potential effects of global warming on the Sacramento/San Joaquin watershed and the San Francisco estuary |
Series title | Geophysical Research Letters |
DOI | 10.1029/2001GL014339 |
Volume | 29 |
Issue | 18 |
Year Published | 2002 |
Language | English |
Publisher | American Geophysical Union |
Contributing office(s) | California Water Science Center, San Francisco Bay-Delta, Toxic Substances Hydrology Program |
Description | 4 p. |
First page | 38-1 |
Last page | 38-4 |
Country | United States |
State | California |
County | San Francisco |
City | San Francisco |
Other Geospatial | San Francisco Bay area |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |