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A New Rossby Wave–Breaking Interpretation of the North Atlantic Oscillation

JOURNAL OF THE ATMOSPHERIC SCIENCES, no. 2 (2010): 609-626

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This paper proposes the hypothesis that the low-frequency variability of the North Atlantic Oscillation (NAO) arises as a result of variations in the occurrence of upper-level Rossby wave-breaking events over the North Atlantic. These events lead to synoptic situations similar to midlatitude blocking that are referred to as high-latitude ...更多

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