中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Spatial patterns of multi-centennial surface air temperature trends in Antarctica over 1-1000 CE: Insights from ice core records and modeling

文献类型:期刊论文

作者Lyu, Zhiqiang1; Goosse, Hugues1; Dalaiden, Quentin1; Klein, Francois1; Shi, Feng2,3; Wagner, Sebastian4; Braconnot, Pascale5
刊名QUATERNARY SCIENCE REVIEWS
出版日期2021-11-01
卷号271页码:16
关键词First millennium Antarctica Data assimilation Spatial pattern Reconstruction
ISSN号0277-3791
DOI10.1016/j.quascirev.2021.107205
英文摘要The spatial pattern of Antarctic surface air temperature variability on multi-decadal to multi-centennial time scales is poorly known because of the short instrumental records, the relatively small number of high-resolution paleoclimate observations, and biases in climate models. Here, changes in surface air temperature over Antarctica are reconstructed over the past two millennia using data assimilation constrained by different ice core water isotope records in order to identify robust signals. The comparison between previous statistically based temperature reconstructions and simulations covering the full Common Era driven by natural and anthropogenic forcings shows major discrepancies occurring in the period 1-1000 CE over East Antarctica, with the reconstructions displaying a warming over 1-500 CE that is not reproduced by the simulations. This suggests that the trends in the first millennium deduced from the statistically based reconstructions are unlikely to be entirely forced by external forcings. Our reconstructions show the high sensitivity of the 500-year temperature trend in Antarctica and its spatial distribution to selection of the records for the reconstructions, especially during 1-500 CE. A robust cooling over Antarctica during 501-1000 CE has been obtained in three data assimilation-based reconstructions with a larger magnitude in the WAIS than elsewhere over Antarctica, in agreement with previous estimates with the larger changes than simulated in climate models. The reconstructions for atmospheric circulation indicate that the pattern of temperature changes over 501-1000 CE is related to the positive trend of Southern Annular Mode and a deepening of Amundsen Sea Low. This confirms the role of internal variability in the temperature trends on multi-centennial scales. (C) 2021 Elsevier Ltd. All rights reserved.
WOS关键词SOUTHERN ANNULAR MODE ; EARTH SYSTEM MODEL ; LAST MILLENNIUM ; HEMISPHERE CLIMATE ; SNOW ACCUMULATION ; DATA ASSIMILATION ; WEST ANTARCTICA ; MASS-BALANCE ; VARIABILITY ; SIMULATIONS
资助项目Belgian Research Action through Interdisciplinary Networks (BRAINebe) from the Belgian Science Policy Office[BR/165/A2/Mass2Ant] ; China Scholarship Council (CSC) -Universite catholique de Louvain CoeFunding ; Youth Innovation Promotion Association CAS ; Key Research Program of the Institute of Geology & Geophysics, CAS[IGGCAS-201905] ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS)
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000703097800010
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构Belgian Research Action through Interdisciplinary Networks (BRAINebe) from the Belgian Science Policy Office ; Belgian Research Action through Interdisciplinary Networks (BRAINebe) from the Belgian Science Policy Office ; China Scholarship Council (CSC) -Universite catholique de Louvain CoeFunding ; China Scholarship Council (CSC) -Universite catholique de Louvain CoeFunding ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Key Research Program of the Institute of Geology & Geophysics, CAS ; Key Research Program of the Institute of Geology & Geophysics, CAS ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Belgian Research Action through Interdisciplinary Networks (BRAINebe) from the Belgian Science Policy Office ; Belgian Research Action through Interdisciplinary Networks (BRAINebe) from the Belgian Science Policy Office ; China Scholarship Council (CSC) -Universite catholique de Louvain CoeFunding ; China Scholarship Council (CSC) -Universite catholique de Louvain CoeFunding ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Key Research Program of the Institute of Geology & Geophysics, CAS ; Key Research Program of the Institute of Geology & Geophysics, CAS ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Belgian Research Action through Interdisciplinary Networks (BRAINebe) from the Belgian Science Policy Office ; Belgian Research Action through Interdisciplinary Networks (BRAINebe) from the Belgian Science Policy Office ; China Scholarship Council (CSC) -Universite catholique de Louvain CoeFunding ; China Scholarship Council (CSC) -Universite catholique de Louvain CoeFunding ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Key Research Program of the Institute of Geology & Geophysics, CAS ; Key Research Program of the Institute of Geology & Geophysics, CAS ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Belgian Research Action through Interdisciplinary Networks (BRAINebe) from the Belgian Science Policy Office ; Belgian Research Action through Interdisciplinary Networks (BRAINebe) from the Belgian Science Policy Office ; China Scholarship Council (CSC) -Universite catholique de Louvain CoeFunding ; China Scholarship Council (CSC) -Universite catholique de Louvain CoeFunding ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; Key Research Program of the Institute of Geology & Geophysics, CAS ; Key Research Program of the Institute of Geology & Geophysics, CAS ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS) ; Fond de la Recherche Scientifique de Belgique (F.R.S.-FNRS)
源URL[http://ir.iggcas.ac.cn/handle/132A11/102726]  
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Lyu, Zhiqiang
作者单位1.Univ Catholique Louvain UCL, Georges Lemaitre Ctr Earth & Climate Res TECLIM, Earth & Life Inst ELI, Louvain La Neuve, Belgium
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing, Peoples R China
3.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
4.Helmholtz Zentrum Hereon, Inst Coastal Syst, D-21502 Geesthacht, Germany
5.Univ Paris Saclay, Unite Mixte CEA CNRS UVSQ, IPSL Lab Sci Climat & Environm, Bat 714, F-91191 Gif Sur Yvette, France
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GB/T 7714
Lyu, Zhiqiang,Goosse, Hugues,Dalaiden, Quentin,et al. Spatial patterns of multi-centennial surface air temperature trends in Antarctica over 1-1000 CE: Insights from ice core records and modeling[J]. QUATERNARY SCIENCE REVIEWS,2021,271:16.
APA Lyu, Zhiqiang.,Goosse, Hugues.,Dalaiden, Quentin.,Klein, Francois.,Shi, Feng.,...&Braconnot, Pascale.(2021).Spatial patterns of multi-centennial surface air temperature trends in Antarctica over 1-1000 CE: Insights from ice core records and modeling.QUATERNARY SCIENCE REVIEWS,271,16.
MLA Lyu, Zhiqiang,et al."Spatial patterns of multi-centennial surface air temperature trends in Antarctica over 1-1000 CE: Insights from ice core records and modeling".QUATERNARY SCIENCE REVIEWS 271(2021):16.

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来源:地质与地球物理研究所

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