Abstract
The cause of decadal climate variability over the North Pacific Ocean and North America is investigated by the analysis of data from a multidecadal integration with a state-of-the-art coupled ocean-atmosphere model and observations. About one-third of the low-frequency climate variability in the region of interest can be attributed to a cycle involving unstable air-sea interactions between the subtropical gyre circulation in the North Pacific and the Aleutian low-pressure system. The existence of this cycle provides a basis for long-range climate forecasting over the western United States at decadal time scales.
Keywords
Ocean gyreClimatologyPacific decadal oscillationOceanographySubtropicsEnvironmental scienceGeneral Circulation ModelRange (aeronautics)Pacific oceanClimate modelClimate changeNorth Pacific HighSea surface temperatureGeology
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Publication Info
- Year
- 1994
- Type
- article
- Volume
- 266
- Issue
- 5185
- Pages
- 634-637
- Citations
- 1071
- Access
- Closed
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Cite This
Mojib Latif,
T. P. Barnett
(1994).
Causes of Decadal Climate Variability over the North Pacific and North America.
Science
, 266
(5185)
, 634-637.
https://doi.org/10.1126/science.266.5185.634
Identifiers
- DOI
- 10.1126/science.266.5185.634