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非绝热加热对大气局地扰动位能的影响和机理
引用本文:高丽,李建平.非绝热加热对大气局地扰动位能的影响和机理[J].地球物理学报,2013,56(10):3255-3269.
作者姓名:高丽  李建平
作者单位:1. 中国气象局 国家气象中心 数值预报中心, 北京 100081; 2. 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
基金项目:国家重点基础研究发展计划(973计划)项目(2010CB950400);国家科技支撑计划项目(2009BAC51B03)资助
摘    要:本文运用统计相关和奇异值分解方法,系统地考察了非绝热加热对大气局地扰动位能的影响特征和机理问题.分析结果表明,热带地区海表温度异常和扰动位能的耦合相关特征与厄尔尼诺和南方涛动变率的关系密切,扰动位能在热带外地区的耦合模态空间型呈现出与北太平洋-北美大气遥相关型极为相似的分布特征.通过进一步考察大气中视热源与扰动位能的耦合特征,发现在低纬地区仍主要反映了厄尔尼诺和南方涛动的影响机制,在热带外地区,视热源异常的耦合模态则表现出与北半球环状模类似的特点,这表明热带外地区大气的局地能量有效性与热带非绝热加热的遥强迫以及局地性热源加热强迫有着极为密切的联系.

关 键 词:大气非绝热加热  扰动位能  海温  视热源  
收稿时间:2012-10-12

Impacts and mechanism of diabatic heating on atmospheric perturbation potential energy
GAO Li,LI Jian-Ping.Impacts and mechanism of diabatic heating on atmospheric perturbation potential energy[J].Chinese Journal of Geophysics,2013,56(10):3255-3269.
Authors:GAO Li  LI Jian-Ping
Institution:1. Numerical Prediction Center, National Meteorological Center, China Meteorological Administration, Beijing 100081, China; 2. State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
Abstract:This study systematically examines the impacts and mechanism of diabatic heating on atmospheric perturbed potential energy (PPE) using statistical correlation analysis and singular value decomposition (SVD) analysis methods. Results show that the coupled correlation features between tropical sea surface temperature (SST) anomalies and PPE are intimately associated with the El Niño-Southern Oscillation (ENSO) phenomenon and those between tropical SST anomalies and extratropical PPE are characterized by the Pacific-North America (PNA)-like pattern. Through further examination of the coupled features between atmospheric apparent heat source (Q1) and PPE, it is demonstrated that over the tropical region the impacts and mechanism between them still mainly reflect ENSO variability, whereas over the extratropical region the coupled patterns between them are manifested by the northern-hemispheric annular mode to some extent. This indicates that the atmospheric local energy availability over the extratropics is closely linked with the remote forcing of tropical diabatic heating and the forcing of local heat source.
Keywords:Atmospheric diabatic heating  Perturbation potential energy  Sea surface temperature  Apparent heat source
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