Relationship between western North Pacific typhoon activity and Tibetan Plateau winter and spring snow cover

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Abstract

The annual frequency of western North Pacific (WNP) typhoons and the number of landfall typhoons in China are shown to negatively correlate with the Tibetan Plateau snow cover (TP-SC) during the preceding winter and spring. When TP-SC was above normal, fewer typhoons formed in the WNP and made landfall in China, and vice versa. The observed seasonal lag correlation between the TP-SC and the WNP typhoon activity suggests the existence of a seasonal memory of the East Asia - West Pacific regional climate system which provides a means for the seasonal prediction of WNP typhoon activity and typhoon landfall frequency in China. Copyright 2005 by the American Geophysical Union.

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Xie, L., Yan, T., Pietrafesa, L. J., Karl, T., & Xu, X. (2005). Relationship between western North Pacific typhoon activity and Tibetan Plateau winter and spring snow cover. Geophysical Research Letters, 32(16), 1–4. https://doi.org/10.1029/2005GL023237

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