CAJ | 학술논문

2013年秋季，东北地区气候异常特征总体表现为：气温偏高，降水总体偏多，尤其10和11月降水持续异常偏多。分析表明，西北太平洋中纬度地区暖海温外强迫和大气环流系统的组合异常是东北地区气候异常的主要原因。秋季北极涛动正位相特征显著，东北地区上空为异常正高度距平控制，环流异常形势不利于冷空气扩散南下影响东北地区，造成秋季东北地区明显偏暖。秋季中后期，东北地区降水偏多主要受西北太平洋中纬度地区异常偏强的东南风水汽输送影响。
2013년추계，동북지구기후이상특정총체표현위：기온편고，강수총체편다，우기10화11월강수지속이상편다。분석표명，서북태평양중위도지구난해온외강박화대기배류계통적조합이상시동북지구기후이상적주요원인。추계북겁도동정위상특정현저，동북지구상공위이상정고도거평공제，배류이상형세불리우랭공기확산남하영향동북지구，조성추계동북지구명현편난。추계중후기，동북지구강수편다주요수서북태평양중위도지구이상편강적동남풍수기수송영향。
During the autumn of 2013,the surface air temperature was higher than normal and the precipi-tation amount was above normal in most part of the Northeast China,especially from October to Novem-ber.The diagnosing results show that the external forcing of higher sea surface temperature in Northwest Pacific Ocean and atmospheric circulation features,may lead to the climatic anomaly in Northeast China. The abnormal circulation pattern with obviously positive phase of Arctic Oscillation,and positive anomaly of geopotential height over Northeast China is unfavorable for cold air to move southward causing higher air temperature in Northeast China for the season.Meanwhile,in mid-late Autumn,precipitation anomaly in the Northeast China is mainly influenced by the stronger southeasterly moisture transport from the western North Pacific Ocean.