Relative humidity variation derived from tree‐ring δ 18 O and possible large‐scale atmospheric circulations linkage over the Guanzhong Plain, central northern China, since 1760 CE

Abstract China is drastically influenced by the Asian monsoon. Based on the relationship ( r = −.636, N = 62, p < .001) between tree‐ring δ 18 O values from nine cores of Pinus tabulaeformis Carr. from Nanwutai and the Asia monsoon‐related June–August relative humidity (RH JJA ), we designed a tr...

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Published in:International Journal of Climatology
Main Authors: Liu, Ruoshi, Li, Qiang, Liu, Yu, Li, Xuxiang, Ren, Meng, Ma, Yongyong, Sun, Changfeng, Song, Huiming, Cai, Qiufang
Other Authors: National Natural Science Foundation of China
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2021
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.7004
https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7004
https://onlinelibrary.wiley.com/doi/full-xml/10.1002/joc.7004
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spelling crwiley:10.1002/joc.7004 2024-06-02T08:02:28+00:00 Relative humidity variation derived from tree‐ring δ 18 O and possible large‐scale atmospheric circulations linkage over the Guanzhong Plain, central northern China, since 1760 CE Liu, Ruoshi Li, Qiang Liu, Yu Li, Xuxiang Ren, Meng Ma, Yongyong Sun, Changfeng Song, Huiming Cai, Qiufang National Natural Science Foundation of China 2021 http://dx.doi.org/10.1002/joc.7004 https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7004 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/joc.7004 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7004 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 41, issue 5, page 3044-3057 ISSN 0899-8418 1097-0088 journal-article 2021 crwiley https://doi.org/10.1002/joc.7004 2024-05-03T11:14:44Z Abstract China is drastically influenced by the Asian monsoon. Based on the relationship ( r = −.636, N = 62, p < .001) between tree‐ring δ 18 O values from nine cores of Pinus tabulaeformis Carr. from Nanwutai and the Asia monsoon‐related June–August relative humidity (RH JJA ), we designed a transfer function reconstructing the RH JJA variation from 1760 to 2018 CE. Our RH JJA reconstruction captured some extreme climatic events that occurred in the past, such as the Ding‐Wu disaster (1876–1878 CE), which was the most serious drought event of northern China in the 19th century, and the severe drought event of 1925–1930 CE. The spatial correlation analysis shows that our RH JJA reconstruction has not only local but also large‐scale hydroclimate circulations. Our reconstruction compared well with other hydroclimate series from northern China, indicating the large‐scale representativeness of our reconstruction. Both the ensemble empirical mode decomposition (EEMD) and the periodicity analyses revealed that the El Niño–South Oscillation (ENSO), the Pacific Decadal Oscillation (PDO), the Arctic Oscillation (AO) and the solar activity strongly affected Asian monsoon‐related RH JJA changes over Guanzhong Plain in the past. We believe this study is of great significance and provides an in‐depth understanding of climate change in the Guanzhong Plain and in northern China. Article in Journal/Newspaper Arctic Climate change Wiley Online Library Arctic Carr ENVELOPE(130.717,130.717,-66.117,-66.117) Pacific International Journal of Climatology 41 5 3044 3057
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract China is drastically influenced by the Asian monsoon. Based on the relationship ( r = −.636, N = 62, p < .001) between tree‐ring δ 18 O values from nine cores of Pinus tabulaeformis Carr. from Nanwutai and the Asia monsoon‐related June–August relative humidity (RH JJA ), we designed a transfer function reconstructing the RH JJA variation from 1760 to 2018 CE. Our RH JJA reconstruction captured some extreme climatic events that occurred in the past, such as the Ding‐Wu disaster (1876–1878 CE), which was the most serious drought event of northern China in the 19th century, and the severe drought event of 1925–1930 CE. The spatial correlation analysis shows that our RH JJA reconstruction has not only local but also large‐scale hydroclimate circulations. Our reconstruction compared well with other hydroclimate series from northern China, indicating the large‐scale representativeness of our reconstruction. Both the ensemble empirical mode decomposition (EEMD) and the periodicity analyses revealed that the El Niño–South Oscillation (ENSO), the Pacific Decadal Oscillation (PDO), the Arctic Oscillation (AO) and the solar activity strongly affected Asian monsoon‐related RH JJA changes over Guanzhong Plain in the past. We believe this study is of great significance and provides an in‐depth understanding of climate change in the Guanzhong Plain and in northern China.
author2 National Natural Science Foundation of China
format Article in Journal/Newspaper
author Liu, Ruoshi
Li, Qiang
Liu, Yu
Li, Xuxiang
Ren, Meng
Ma, Yongyong
Sun, Changfeng
Song, Huiming
Cai, Qiufang
spellingShingle Liu, Ruoshi
Li, Qiang
Liu, Yu
Li, Xuxiang
Ren, Meng
Ma, Yongyong
Sun, Changfeng
Song, Huiming
Cai, Qiufang
Relative humidity variation derived from tree‐ring δ 18 O and possible large‐scale atmospheric circulations linkage over the Guanzhong Plain, central northern China, since 1760 CE
author_facet Liu, Ruoshi
Li, Qiang
Liu, Yu
Li, Xuxiang
Ren, Meng
Ma, Yongyong
Sun, Changfeng
Song, Huiming
Cai, Qiufang
author_sort Liu, Ruoshi
title Relative humidity variation derived from tree‐ring δ 18 O and possible large‐scale atmospheric circulations linkage over the Guanzhong Plain, central northern China, since 1760 CE
title_short Relative humidity variation derived from tree‐ring δ 18 O and possible large‐scale atmospheric circulations linkage over the Guanzhong Plain, central northern China, since 1760 CE
title_full Relative humidity variation derived from tree‐ring δ 18 O and possible large‐scale atmospheric circulations linkage over the Guanzhong Plain, central northern China, since 1760 CE
title_fullStr Relative humidity variation derived from tree‐ring δ 18 O and possible large‐scale atmospheric circulations linkage over the Guanzhong Plain, central northern China, since 1760 CE
title_full_unstemmed Relative humidity variation derived from tree‐ring δ 18 O and possible large‐scale atmospheric circulations linkage over the Guanzhong Plain, central northern China, since 1760 CE
title_sort relative humidity variation derived from tree‐ring δ 18 o and possible large‐scale atmospheric circulations linkage over the guanzhong plain, central northern china, since 1760 ce
publisher Wiley
publishDate 2021
url http://dx.doi.org/10.1002/joc.7004
https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7004
https://onlinelibrary.wiley.com/doi/full-xml/10.1002/joc.7004
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7004
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Pacific
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Climate change
op_source International Journal of Climatology
volume 41, issue 5, page 3044-3057
ISSN 0899-8418 1097-0088
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op_doi https://doi.org/10.1002/joc.7004
container_title International Journal of Climatology
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