中国过去1500年典型暖期气候的模拟研究  

SIMULATION OF THE CHARACTERISTICS AND MECHANISMS OF CHINESE TYPICAL WARM PERIODS OVER THE PAST 1500 YEARS

作　　者：严蜜[1,2] 王志远[3,4] 刘健[1,2,5] 

机构地区：[1]南京师范大学地理科学学院虚拟地理环境教育部重点实验室,南京210023 [2]江苏省地理信息资源开发与利用协同创新中心,南京210023 [2]中国科学院南京地理与湖泊研究所湖泊与环境国家重点实验室,南京210008 [4]中国科学院大学,北京100049 [3]中国科学院南京地理与湖泊研究所湖泊与环境国家重点实验室,南京210008 [4]中国科学院大学,北京100049 [5]南京师范大学数学科学学院,江苏省大规模复杂系统数值模拟重点实验室,南京210023

出　　处：《第四纪研究》2014年第6期1166-1175,共10页Quaternary Sciences

基　　金：中国科学院战略性先导科技专项项目(批准号:XDA05080800);国家重点基础研究发展规划项目(973项目)(批准号:2010CB950102);国家自然科学基金项目(批准号:41371209和41302137);高等学校博士学科点专项科研基金项目(批准号:20133207110015);江苏省高校自然科学研究重大项目(批准号:14KJA170002);江苏高校优势学科建设项目(批准号:164320H101)共同资助

摘　　要：利用地球系统模式CESM的过去1500年气候模拟试验结果,分析了中世纪暖期和现代暖期中国区域温度和降水变化特征的异同,并对形成原因进行了初步探讨。研究表明:中国的温度变化在中世纪暖期和现代暖期有着显著的区域差异,且年代际变化特征亦不尽相同。现代暖期的温度存在一个明显的年代际突变,这一突变是由温室气体含量的变化引起的,且现代暖期温度变化的空间格局受人为因子影响较大。中世纪暖期温度变化的空间格局主要受太阳辐射变化的影响,其次是土地利用/覆盖和火山活动。中国的降水变化在两个增暖期其时空格局较类似,其主要模态均体现为西部与东部反相,华南与华北反相。影响降水变化空间格局的因子较复杂,各外强迫因子的作用互补。The characteristics and causes of the climate change over China during Medieval Warm Period （MWP） and Present Warm Period （PWP） are analyzed in this paper,based on the climatic simulation results over the past 1500 years using the Community Earth System Model （CESM）.Five experiments are compared,including the solar forcing run （TSI）,volcanic forcing run （VOL）,well-mixed greenhouse gas forcing run （GHGs）,land use/Land cover forcing run （LUCC） and 4-forcing run （MASK）.The experiments are carried out from 1A.D.to 2000A.D.based on a 2400 years＇ control run under the A.D.1850＇s initial forcing,except the VOL run,which only span from 500A.D.to 2000A.D.,limited by the reconstruction of the volcanic forcing.Year 500～2000 is used in this study.We compared the climatology of the temperature and the precipitation derived from the MASK run to the reanalysis data,reconstructions and those derived from the other model simulation data,in order to do the model validation.The characteristics of the simulated temperature and the precipitation by the CESM show similarity to the reanalysis data and the reconstructions.There are three typical climate periods-MWP,Little Ice Age （LIA） and PWP-simulated by the MASK run,which are consistent with the reconstructions.In this study,the two 100 years＇ persistent warming periods during the MWP （1001～ 1100A.D.） and the PWP （1901～ 2000A.D.） are compared.The method of the empirical orthogonal function （EOF） is used in this study to find out the characteristics of the temperature and the precipitation during the two warm periods.The results show that,the spatial patterns of temperature variability over China are different during the two typical warm periods,while the spatial patterns of the precipitation variability are similar.The abrupt change of the temperature during the PWP,caused by the change of the greenhouse gas concentration,is absent during the MWP.The main cause of the temperature change is the greenhouse gas concentration du

关 键 词：中世纪暖期 现代暖期 中国气候 区域差异 气候模拟 

分 类 号：P534.632[天文地球—第四纪地质学]