地理研究 ›› 2016, Vol. 35 ›› Issue (9): 1659-1671.doi: 10.11821/dlyj201609006
收稿日期:
2016-03-07
修回日期:
2016-07-14
出版日期:
2016-09-10
发布日期:
2016-09-23
作者简介:
作者简介:刘斌(1991- ),男,山西寿阳人,博士研究生,主要从事气候模拟与全球变化研究。E-mail:
基金资助:
Bin LIU1(), Jian LIU1,2,3(
), Zhiyuan WANG1
Received:
2016-03-07
Revised:
2016-07-14
Online:
2016-09-10
Published:
2016-09-23
摘要:
利用通用地球系统模式CESM过去1500年气候模拟试验结果,对比分析中世纪暖期南、北半球气候变化特征及成因,对认识南、北半球暖期气候变化规律及其与外强迫变化的关系有重要科学意义。结果表明:中世纪暖期全球及南、北半球总体是变暖的,但仍存在峰谷变化,高纬地区增温幅度大于低纬地区,北半球中世纪暖期比南半球更为明显,其距平变幅也大于南半球。全球降水距平基本为正,南、北半球降水变幅基本相当,降水变化显著区域集中于低纬地区。太阳辐射是影响中世纪暖期全球及半球气温变化最显著的因素,火山活动对北半球气温变化也有较显著的影响。从全球尺度来看,降水由太阳辐射和火山活动共同影响,其中太阳辐射影响最为显著,但从半球尺度来看,火山活动是影响半球降水的重要因素。
刘斌, 刘健, 王志远. 中世纪暖期南北半球气候变化特征与成因的模拟对比[J]. 地理研究, 2016, 35(9): 1659-1671.
Bin LIU, Jian LIU, Zhiyuan WANG. Inter-hemispheric comparison of characteristics and causes of climate change during the Medieval Warm Period based on CESM simulation[J]. GEOGRAPHICAL RESEARCH, 2016, 35(9): 1659-1671.
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