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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.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004054060866305","@type":"Researcher","foaf:name":[{"@value":"M. Latif"}],"jpcoar:affiliationName":[{"@value":"Max-Planck-Institut für Meteorologie, Bundestrasse 55, D-20146 Hamburg, Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045159931393","@type":"Researcher","foaf:name":[{"@value":"T. P. 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