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spelling ftpekinguniv:oai:localhost:20.500.11897/149065 2023-05-15T16:39:10+02:00 Reconstruction of temperature series of China for the last 1000 years Wang ShaoWu Wen XinYu Luo Yong Dong WenJie Zhao ZongCi Yang Bao Wang, SW (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China. Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China. China Meteorol Adm, Lab Climate Studies, Beijing 100081, Peoples R China. China Meteorol Adm, Natl Climate Ctr, Beijing 100081, Peoples R China. Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lab Desert & Desertificat, Lanzhou 730000, Peoples R China. 2007 https://hdl.handle.net/20.500.11897/149065 https://doi.org/10.1007/s11434-007-0425-4 en eng 科学通报 英文版 CHINESE SCIENCE BULLETIN.2007,52,(23),3272-3280. 972367 1001-6538 http://hdl.handle.net/20.500.11897/149065 doi:10.1007/s11434-007-0425-4 WOS:000251407900017 SCI last 1000 years China temperature variations Medieval Warm Period Little Ice Age Modern Warming NORTHERN-HEMISPHERE TEMPERATURES ICE CORES CLIMATE RECORDS MILLENNIUM RESOLUTION VARIABILITY DELTA-O-18 HOLOCENE TAIWAN Journal 2007 ftpekinguniv https://doi.org/20.500.11897/149065 https://doi.org/10.1007/s11434-007-0425-4 2021-08-01T07:58:47Z This paper reports a study on reconstructing temperature series for ten regions of China over the last 1000 years with a time resolution of 10 a. The regions concerned are: Northeast, North, East, South China, Taiwan, Central, Southwest, Northwest China, Xinjiang and Qinghai-Tibet Plateau. A variety of proxy data, such as ice core, tree-rings, stalagmites, peat, lake sediments, pollen and historical records, were validated with instrumental observations made in the last 120 years, and applied in the reconstruction of the temperature series. A temperature series for whole China is then established by averaging the ten regional series with a weighting proportional to the area of each region. Finally, temperature variations for the last 1000 years are examined, with special focus placed on the characteristics of the Medieval Warm Period (MWP), the Little Ice Age (LIA), and Modern Warming (MW). http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000251407900017&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Multidisciplinary Sciences SCI(E) 33 ARTICLE 23 3272-3280 52 Journal/Newspaper ice core Peking University Institutional Repository (PKU IR) Peat Lake ENVELOPE(-137.390,-137.390,68.919,68.919) Chinese Science Bulletin 52 23 3272 3280
institution Open Polar
collection Peking University Institutional Repository (PKU IR)
op_collection_id ftpekinguniv
language English
topic last 1000 years
China
temperature variations
Medieval Warm Period
Little Ice Age
Modern Warming
NORTHERN-HEMISPHERE TEMPERATURES
ICE CORES
CLIMATE
RECORDS
MILLENNIUM
RESOLUTION
VARIABILITY
DELTA-O-18
HOLOCENE
TAIWAN
spellingShingle last 1000 years
China
temperature variations
Medieval Warm Period
Little Ice Age
Modern Warming
NORTHERN-HEMISPHERE TEMPERATURES
ICE CORES
CLIMATE
RECORDS
MILLENNIUM
RESOLUTION
VARIABILITY
DELTA-O-18
HOLOCENE
TAIWAN
Wang ShaoWu
Wen XinYu
Luo Yong
Dong WenJie
Zhao ZongCi
Yang Bao
Reconstruction of temperature series of China for the last 1000 years
topic_facet last 1000 years
China
temperature variations
Medieval Warm Period
Little Ice Age
Modern Warming
NORTHERN-HEMISPHERE TEMPERATURES
ICE CORES
CLIMATE
RECORDS
MILLENNIUM
RESOLUTION
VARIABILITY
DELTA-O-18
HOLOCENE
TAIWAN
description This paper reports a study on reconstructing temperature series for ten regions of China over the last 1000 years with a time resolution of 10 a. The regions concerned are: Northeast, North, East, South China, Taiwan, Central, Southwest, Northwest China, Xinjiang and Qinghai-Tibet Plateau. A variety of proxy data, such as ice core, tree-rings, stalagmites, peat, lake sediments, pollen and historical records, were validated with instrumental observations made in the last 120 years, and applied in the reconstruction of the temperature series. A temperature series for whole China is then established by averaging the ten regional series with a weighting proportional to the area of each region. Finally, temperature variations for the last 1000 years are examined, with special focus placed on the characteristics of the Medieval Warm Period (MWP), the Little Ice Age (LIA), and Modern Warming (MW). http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000251407900017&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Multidisciplinary Sciences SCI(E) 33 ARTICLE 23 3272-3280 52
author2 Wang, SW (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China.
Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China.
China Meteorol Adm, Lab Climate Studies, Beijing 100081, Peoples R China.
China Meteorol Adm, Natl Climate Ctr, Beijing 100081, Peoples R China.
Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lab Desert & Desertificat, Lanzhou 730000, Peoples R China.
format Journal/Newspaper
author Wang ShaoWu
Wen XinYu
Luo Yong
Dong WenJie
Zhao ZongCi
Yang Bao
author_facet Wang ShaoWu
Wen XinYu
Luo Yong
Dong WenJie
Zhao ZongCi
Yang Bao
author_sort Wang ShaoWu
title Reconstruction of temperature series of China for the last 1000 years
title_short Reconstruction of temperature series of China for the last 1000 years
title_full Reconstruction of temperature series of China for the last 1000 years
title_fullStr Reconstruction of temperature series of China for the last 1000 years
title_full_unstemmed Reconstruction of temperature series of China for the last 1000 years
title_sort reconstruction of temperature series of china for the last 1000 years
publisher 科学通报 英文版
publishDate 2007
url https://hdl.handle.net/20.500.11897/149065
https://doi.org/10.1007/s11434-007-0425-4
long_lat ENVELOPE(-137.390,-137.390,68.919,68.919)
geographic Peat Lake
geographic_facet Peat Lake
genre ice core
genre_facet ice core
op_source SCI
op_relation CHINESE SCIENCE BULLETIN.2007,52,(23),3272-3280.
972367
1001-6538
http://hdl.handle.net/20.500.11897/149065
doi:10.1007/s11434-007-0425-4
WOS:000251407900017
op_doi https://doi.org/20.500.11897/149065
https://doi.org/10.1007/s11434-007-0425-4
container_title Chinese Science Bulletin
container_volume 52
container_issue 23
container_start_page 3272
op_container_end_page 3280
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