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  2. 地质与地球物理研究所
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  4. 中国科学院新生代地质与环境重点实验室
Mid-Holocene climate change over China: model-data discrepancy

文献类型：期刊论文

作者Lin, Yating4,5,6; Ramstein, Gilles5; Wu, Haibin2,4,6; Rani, Raj5; Braconnot, Pascale5; Kageyama, Masa5; Li, Qin2,6; Luo, Yunli3; Zhang, Ran1; Guo, Zhengtang2,4,6
刊名CLIMATE OF THE PAST
出版日期2019-07-02
卷号15期号:4页码:1223-1249
ISSN号1814-9324
DOI10.5194/cp-15-1223-2019
英文摘要The mid-Holocene period (MH) has long been an ideal target for the validation of general circulation model (GCM) results against reconstructions gathered in global datasets. These studies aim to test GCM sensitivity, mainly to seasonal changes induced by the orbital parameters (longitude of the perihelion). Despite widespread agreement between model results and data on the MH climate, some important differences still exist. There is no consensus on the continental size (the area of the temperature anomaly) of the MH thermal climate response, which makes regional quantitative reconstruction critical to obtain a comprehensive understanding of the MH climate patterns. Here, we compare the annual and seasonal outputs from the most recent Paleoclimate Modelling Intercomparison Project Phase 3 (PMIP3) models with an updated synthesis of climate reconstruction over China, including, for the first time, a seasonal cycle of temperature and precipitation. Our results indicate that the main discrepancies between model and data for the MH climate are the annual and winter mean temperature. A warmerthan-present climate condition is derived from pollen data for both annual mean temperature (similar to 0.7K on average) and winter mean temperature (similar to 1K on average), while most of the models provide both colder-than-present annual and winter mean temperature and a relatively warmer summer, showing a linear response driven by the seasonal forcing. By conducting simulations in BIOME4 and CESM, we show that surface processes are the key factors creating the uncertainties between models and data. These results pinpoint the crucial importance of including the non-linear responses of the surface water and energy balance to vegetation changes.
WOS关键词LAST GLACIAL MAXIMUM ; HOLOCENE VEGETATION HISTORY ; PMIP2 COUPLED SIMULATIONS ; EARTH SYSTEM MODEL ; POLLEN RECORD ; INNER-MONGOLIA ; ASIAN MONSOON ; PALEOCLIMATE RECONSTRUCTION ; ENVIRONMENTAL-CHANGES ; FUTURE PROJECTIONS
资助项目National Basic Research Program of China[2016YFA0600504] ; National Science Foundation of China[41572165] ; National Science Foundation of China[41690114] ; National Science Foundation of China[41125011]
WOS研究方向Geology ; Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000520467400001
出版者COPERNICUS GESELLSCHAFT MBH
资助机构National Basic Research Program of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China ; National Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/95587]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Wu, Haibin
作者单位1.Chinese Acad Sci, Inst Atmospher Phys, Beijing 100029, Peoples R China
2.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
3.Chinese Acad Sci, Inst Bot, Beijing 100093, Peoples R China
4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
5.Univ Paris Saclay, LSCE, IPSL, CEA,CNRS,UVSQ, F-91191 Gif Sur Yvette, France
6.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Lin, Yating,Ramstein, Gilles,Wu, Haibin,et al. Mid-Holocene climate change over China: model-data discrepancy[J]. CLIMATE OF THE PAST,2019,15(4):1223-1249.
APA Lin, Yating.,Ramstein, Gilles.,Wu, Haibin.,Rani, Raj.,Braconnot, Pascale.,...&Guo, Zhengtang.(2019).Mid-Holocene climate change over China: model-data discrepancy.CLIMATE OF THE PAST,15(4),1223-1249.
MLA Lin, Yating,et al."Mid-Holocene climate change over China: model-data discrepancy".CLIMATE OF THE PAST 15.4(2019):1223-1249.

入库方式： OAI收割

来源：地质与地球物理研究所

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