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首页> 外文期刊>Acta Oceanologica Sinica >Relationship between SSTA in the northwestern Pacific and winter climate anomaly in China
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Relationship between SSTA in the northwestern Pacific and winter climate anomaly in China

机译:西北太平洋海温异常与中国冬季气候异常的关系

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摘要

The relationship between sea surface temperature anomaly (SSTA) in the domain from the northwest of the Pacific to China seas (NWP-CS) and climate (precipitation and surface temperature) anomaly in winters over east of Chinese Mainland (ECM) are investigated with composite analysis. The results suggest that (1) SSTA in NWP-CS usually appears as "seesaw" pattern, i.e., sign of SSTA in the northwest of the Philippines is positive (negative) while in the southeast it is negative (positive), defined as SSTA "seesaw" positive (negative) pattern. When SSTA "seesaw" positive (negative) pattern appears, the surface temperature in ECM is higher (lower) than the normal winters but the precipitation anomaly is hot distinct; (2) there are two anomalous anticyclones (cyclones) locating in the northwest Pacific and east of the Philippines at 850 hPa level and an anomalous anti-Hadley (Hadley) circulation, which descends (ascends) south of 18°N, ascends (descends) north of 18°N; (3) heat flux anomaly from ocean into atmosphere is weaker (stronger) in the northwest of the Philippines but stronger (weaker) in the southeast of the Philippines than the normal winters, because the weaker (stronger) northerly prevails in the northwest of the Philippines and stronger (weaker) northeaster in the southeast of the Philippines induced by anomalous anticyclones (cyclones).
机译:结合西北太平洋西北向中国海(NWP-CS)区域的海表温度异常(NSTA-CS)与中国大陆东部(ECM)冬季的气候(降水和表面温度)异常之间的关系。分析。结果表明:(1)NWP-CS中的SSTA通常以“跷跷板”形式出现,即菲律宾西北部SSTA的符号为正(负),而东南部为负(正),定义为SSTA。 “跷跷板”正(负)模式。当出现SSTA“跷跷板”正(负)模式时,ECM中的地表温度高于(低于)正常冬季,但降水异常明显。 (2)在太平洋西北部和菲律宾东部以850 hPa的高度有两个反气旋(旋风),反哈德利(Hadley)异常环流在18°N以南下降(上升),上升(下降) )18°N以北; (3)在菲律宾西北部,从海洋到大气的热通量异常较弱(强),但在菲律宾东南部则比正常冬季强(弱),因为在该国西北部,北部较弱(强)。菲律宾和反东南气旋(反气旋)引起的菲律宾东南部的东北偏强(较弱)。

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