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The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon

Qiang Li, Yu Liu, Takeshi Nakatsuka, Huiming Song, Danny McCarroll, Yinke Yang, Jun Qi

Global and Planetary Change, Volume: 132, Pages: 11 - 19

Swansea University Author: Danny McCarroll

DOI (Published version): 10.1016/j.gloplacha.2015.06.005

Abstract

Understanding the interactions between the East Asian summer monsoon and Indian summer monsoon is a challenging task because of the insufficient proxy records. In this study, we reconstructed a 225-year precipitation record by combining ring widths of Pinus tabulaeformis and stable oxygen isotope ra...

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Published in: Global and Planetary Change
Published: 2015
URI: https://cronfa.swan.ac.uk/Record/cronfa24953
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spelling 2016-02-25T18:20:13.4690688 v2 24953 2015-12-05 The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon 6d181d926aaac8932c2bfa8d0e7f6960 Danny McCarroll Danny McCarroll true false 2015-12-05 FGSEN Understanding the interactions between the East Asian summer monsoon and Indian summer monsoon is a challenging task because of the insufficient proxy records. In this study, we reconstructed a 225-year precipitation record by combining ring widths of Pinus tabulaeformis and stable oxygen isotope ratios of Larix principis-rupprechtii using a multi-proxy dendroclimatology approach in the North China. The reconstructed record explained 51.9% of the variance in the observed precipitation during 1955–2003. The precipitation series could indicate the intensity of the East Asian summer monsoon. A spatial field analysis indicated that the series was strongly correlated with the reconstructed records of the surrounding area and a large part of the Indian subcontinent. The reconstructed records were significantly and positively correlated with All Indian Precipitation records (r = 0.32, n = 132, p < 0.001) and with a proxy of the Indian summer monsoon. These findings suggest that a persistent teleconnection exists between the reconstructed record and the Indian summer monsoon records from the past 225 years. The observed interannual synchronisation potentially resulted from the transport of partial water vapour from the Indian summer monsoon area to NC; however, this synchronisation could not be attributed to the El Nino-South Oscillation (ENSO). When considering an interdecadal time scale, the synchronisation with the North Atlantic Oscillation (NAO) has varied since 1779, implying that the NAO may serve as an additional atmospheric pattern that affects this teleconnection Journal Article Global and Planetary Change 132 11 19 Tree-ring width; Shanxi Province; Teleconnection; East Asian summer monsoon; Indian summer monsoon teleconnection 30 9 2015 2015-09-30 10.1016/j.gloplacha.2015.06.005 Available online 23 June 2015 COLLEGE NANME Science and Engineering - Faculty COLLEGE CODE FGSEN Swansea University 2016-02-25T18:20:13.4690688 2015-12-05T12:54:09.4069784 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography Qiang Li 1 Yu Liu 2 Takeshi Nakatsuka 3 Huiming Song 4 Danny McCarroll 5 Yinke Yang 6 Jun Qi 7 0024953-25022016181921.pdf McCarroll225Year2015AM.pdf 2016-02-25T18:19:21.8630000 Output 2547721 application/pdf Accepted Manuscript true 2016-06-23T00:00:00.0000000 true
title The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon
spellingShingle The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon
Danny McCarroll
title_short The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon
title_full The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon
title_fullStr The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon
title_full_unstemmed The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon
title_sort The 225-year precipitation variability inferred from tree-ring records in Shanxi Province, the North China, and its teleconnection with Indian summer monsoon
author_id_str_mv 6d181d926aaac8932c2bfa8d0e7f6960
author_id_fullname_str_mv 6d181d926aaac8932c2bfa8d0e7f6960_***_Danny McCarroll
author Danny McCarroll
author2 Qiang Li
Yu Liu
Takeshi Nakatsuka
Huiming Song
Danny McCarroll
Yinke Yang
Jun Qi
format Journal article
container_title Global and Planetary Change
container_volume 132
container_start_page 11
publishDate 2015
institution Swansea University
doi_str_mv 10.1016/j.gloplacha.2015.06.005
college_str Faculty of Science and Engineering
hierarchytype
hierarchy_top_id facultyofscienceandengineering
hierarchy_top_title Faculty of Science and Engineering
hierarchy_parent_id facultyofscienceandengineering
hierarchy_parent_title Faculty of Science and Engineering
department_str School of Biosciences, Geography and Physics - Geography{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Biosciences, Geography and Physics - Geography
document_store_str 1
active_str 0
description Understanding the interactions between the East Asian summer monsoon and Indian summer monsoon is a challenging task because of the insufficient proxy records. In this study, we reconstructed a 225-year precipitation record by combining ring widths of Pinus tabulaeformis and stable oxygen isotope ratios of Larix principis-rupprechtii using a multi-proxy dendroclimatology approach in the North China. The reconstructed record explained 51.9% of the variance in the observed precipitation during 1955–2003. The precipitation series could indicate the intensity of the East Asian summer monsoon. A spatial field analysis indicated that the series was strongly correlated with the reconstructed records of the surrounding area and a large part of the Indian subcontinent. The reconstructed records were significantly and positively correlated with All Indian Precipitation records (r = 0.32, n = 132, p < 0.001) and with a proxy of the Indian summer monsoon. These findings suggest that a persistent teleconnection exists between the reconstructed record and the Indian summer monsoon records from the past 225 years. The observed interannual synchronisation potentially resulted from the transport of partial water vapour from the Indian summer monsoon area to NC; however, this synchronisation could not be attributed to the El Nino-South Oscillation (ENSO). When considering an interdecadal time scale, the synchronisation with the North Atlantic Oscillation (NAO) has varied since 1779, implying that the NAO may serve as an additional atmospheric pattern that affects this teleconnection
published_date 2015-09-30T03:29:39Z
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score 11.013148

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