全球增暖背景下大气经向热量输送气候变化特征Climate Change Characteristics of Atmospheric Meridional Heat Transport Under Global Warming
李张瑞,余锦华,李青青,纪源
摘要(Abstract):
基于1979—2019年ERA5月平均资料,采用信息流和线性回归分析大气经向热量输送(Atmospheric heat transpont, AHT)线性趋势,并讨论全球增暖和Hadley环流对AHT的影响程度。结果表明:AHT在南北半球各纬度带及不同季节表现出不同的变化特征:6—8月,15°N—65°N和35°S—60°S分别呈现向北输送减弱和向南输送增强的趋势,12—2月,5°N—15°S和15°N—40°S分别呈现向北输送增强和向南输送减弱的趋势,表明从夏半球向冬半球的AHT净通量有增加的趋势。信息流显示,经向不均匀增暖是北半球夏季向极AHT减弱的原因。南半球冬季,Hadley环流边界南移导致潜热在副热带的辐散中心南移,感热在副热带的辐散中心南移与环流边界南移相互反馈。北半球春(秋)季,感热向赤道辐合增强(减弱)与Hadley环流增强(减弱)相互反馈。南半球春季,Hadley环流增强导致位能向副热带辐合增强,南半球秋季,Hadley环流增强导致潜热向赤道辐合增强。
关键词(KeyWords): 经向热量输送;全球增暖;Hadley环流;信息流;热带扩张
基金项目(Foundation): 国家重点研究发展计划项目(2018YFC1507704);; 南京信息工程大学大学生创新创业训练计划项目(202010300051Y)资助~~
作者(Author): 李张瑞,余锦华,李青青,纪源
DOI: 10.16441/j.cnki.hdxb.20210092
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