1990年代初夏季东北亚低压的年代际转变  

Inter-decadal Change in the Summertime Northeast Asia Low-Pressure System in the Early 1990s

作　　者：杜梦醒 林中达[1] 陆日宇[1] 

机构地区：[1]中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室,北京100029 [2]中国科学院大学,北京100049

出　　处：《大气科学》2016年第4期805-816,共12页Chinese Journal of Atmospheric Sciences

基　　金：国家自然科学基金项目41375086~~

摘　　要：夏季东亚地区对流层低层受到一个陆地低压系统控制;该低压中心位于东亚的北部地区,文中称之为东北亚低压。基于NCEP/DOE、NCEP/NCAR、ERA-40和ERA-Interim四种不同的再分析数据,本文分析了夏季东北亚低压的年代际变化特征,并进一步探讨了其转变的可能物理机理。研究结果表明夏季东北亚低压在1990年代初期存在一次显著的年代际转变,之后低压强度减弱。对应此次年代际转变,东北亚地区对流层位势高度呈现为正压结构的正异常,其南侧的高空西风急流中心强度减弱。进一步,基于观测和简单线性斜压模式模拟结果,我们提出环贝加尔湖地区夏季气温增加可能是导致1990年代初期之后夏季东北亚低压减弱的原因。East Asian summer climate is controlled by a low pressure system centered over continental northern East Asia in the lower troposphere, which is named as the Northeast Asia low pressure （NEAL）. Based on the NCEP-DOE, NCEP-NCAR, ERA-40, and ERA-Interim reanalysis data, we investigate the inter-decadal change of the summertime Northeast Asia Low-pressure system and discuss the possible physical mechanism associated with this change. Results show that NEAL experienced a significant decadal change in the early 1990s. The intensity of NEAL has decreased since 1991. Corresponding to the weakened NEAL, the tropospheric geopotential height field over Northeast Asia presents a barotropic-structure positive anomaly and the intensity of upper-tropospheric westerly jet to the south decreases. Based on results from the observational analysis and simulations of a linear baroclinic model, it is found that the surface warming around the Lake Baikal in the summer may be responsible for the weakening of the NEAL after the early 1990s.

关 键 词：夏季东北亚低压 年代际变化 环贝加尔湖增暖 

分 类 号：P424[天文地球—大气科学及气象学]