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SST Key area to east China summer rainfall

Qian Zhu

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Abstract

Based on global SST and China rainfall datasets in 1951~1994,the SST in the preceding March over north Pacific region(42.5~52.5°N,170°E~170°W) is found to be essential to China summer rainfall and the region is defined as the SST key area.A possible teleconnection pattern is presented to explain the effects of SST in the preceding March over the key area on China summer rainfall.It is found that correlation between SST in key area and China summer rainfall is good and stable,which is not under the influence of interdecadal variation in SST.

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What this paper is about

Based on global SST and China rainfall datasets in 1951~1994,the SST in the preceding March over north Pacific region(42.5~52.5°N,170°E~170°W) is found to be essential to China summer rainfall and the region is defined as the SST key area.A possible teleconnection pattern is presented to explain the effects of SST in the preceding March over the key area on China summer rainfall.It is found that correlation between SST in key area and China summer rainfall is good and stable,which is not under the influence of interdecadal variation in SST.

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Available abstract

Based on global SST and China rainfall datasets in 1951~1994,the SST in the preceding March over north Pacific region(42.5~52.5°N,170°E~170°W) is found to be essential to China summer rainfall and the region is defined as the SST key area.A possible teleconnection pattern is presented to explain the effects of SST in the preceding March over the key area on China summer rainfall.It is found that correlation between SST in key area and China summer rainfall is good and stable,which is not under the influence of interdecadal variation in SST.

Key concepts: Teleconnection, Climatology, China, Environmental science, Sea surface temperature, Key (lock), Geography, Geology

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