Precipitation Variations in China’s Altay Mountains Detected from Tree Rings Dating Back to AD 1615

As the primary mountain range in Central Asia, the Altay Mountains receive water vapor carried by westerly circulation, resulting in relatively abundant local precipitation and lush pastures in all seasons. Consequently, it has become one of the important transportation routes between Asia and Europ...

Full description

Bibliographic Details
Published in:Forests
Main Authors: Wenxuan Pang, Qiang Li, Yu Liu, Huiming Song, Changfeng Sun, Jiachuan Wang, Yalan Yan, Qiufang Cai, Meng Ren
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/f14071496
id ftmdpi:oai:mdpi.com:/1999-4907/14/7/1496/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/1999-4907/14/7/1496/ 2023-08-20T04:04:44+02:00 Precipitation Variations in China’s Altay Mountains Detected from Tree Rings Dating Back to AD 1615 Wenxuan Pang Qiang Li Yu Liu Huiming Song Changfeng Sun Jiachuan Wang Yalan Yan Qiufang Cai Meng Ren agris 2023-07-21 application/pdf https://doi.org/10.3390/f14071496 EN eng Multidisciplinary Digital Publishing Institute Forest Meteorology and Climate Change https://dx.doi.org/10.3390/f14071496 https://creativecommons.org/licenses/by/4.0/ Forests; Volume 14; Issue 7; Pages: 1496 precipitation reconstruction tree rings Siberian larch the Altay Mountains North Arctic Oscillation Text 2023 ftmdpi https://doi.org/10.3390/f14071496 2023-08-01T10:57:41Z As the primary mountain range in Central Asia, the Altay Mountains receive water vapor carried by westerly circulation, resulting in relatively abundant local precipitation and lush pastures in all seasons. Consequently, it has become one of the important transportation routes between Asia and Europe. The exploration of long-term variations in precipitation is meaningful for understanding the ebb and flow of the Asia–Europe steppe trade routes. However, previous dendroclimatological studies of the Altay Mountains focused more on temperature changes than precipitations variations. We carried out a 404-year precipitation reconstruction based on the tree rings of Siberian larch growing on the south slopes of the Altay Mountains, which could explain 45.9% of the variance observed in the February–October precipitation. Our reconstruction demonstrated some severe drought events which could be found in the historical documents, such as the drought in the late Ming Dynasty (1640s) and the Ding-Wu Disaster (1870s). The spatial correlation analysis, cross-wavelet spectrum and wavelet coherency analysis indicated that the precipitation variations in the study area may be related to the ENSO and NAO. This study presents a robust precipitation reconstruction of the southern Altay Mountains, serving as a reference for future research on large-scale climatic forces acting on Altay precipitation. Text Arctic MDPI Open Access Publishing Arctic Forests 14 7 1496
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic precipitation reconstruction
tree rings
Siberian larch
the Altay Mountains
North Arctic Oscillation
spellingShingle precipitation reconstruction
tree rings
Siberian larch
the Altay Mountains
North Arctic Oscillation
Wenxuan Pang
Qiang Li
Yu Liu
Huiming Song
Changfeng Sun
Jiachuan Wang
Yalan Yan
Qiufang Cai
Meng Ren
Precipitation Variations in China’s Altay Mountains Detected from Tree Rings Dating Back to AD 1615
topic_facet precipitation reconstruction
tree rings
Siberian larch
the Altay Mountains
North Arctic Oscillation
description As the primary mountain range in Central Asia, the Altay Mountains receive water vapor carried by westerly circulation, resulting in relatively abundant local precipitation and lush pastures in all seasons. Consequently, it has become one of the important transportation routes between Asia and Europe. The exploration of long-term variations in precipitation is meaningful for understanding the ebb and flow of the Asia–Europe steppe trade routes. However, previous dendroclimatological studies of the Altay Mountains focused more on temperature changes than precipitations variations. We carried out a 404-year precipitation reconstruction based on the tree rings of Siberian larch growing on the south slopes of the Altay Mountains, which could explain 45.9% of the variance observed in the February–October precipitation. Our reconstruction demonstrated some severe drought events which could be found in the historical documents, such as the drought in the late Ming Dynasty (1640s) and the Ding-Wu Disaster (1870s). The spatial correlation analysis, cross-wavelet spectrum and wavelet coherency analysis indicated that the precipitation variations in the study area may be related to the ENSO and NAO. This study presents a robust precipitation reconstruction of the southern Altay Mountains, serving as a reference for future research on large-scale climatic forces acting on Altay precipitation.
format Text
author Wenxuan Pang
Qiang Li
Yu Liu
Huiming Song
Changfeng Sun
Jiachuan Wang
Yalan Yan
Qiufang Cai
Meng Ren
author_facet Wenxuan Pang
Qiang Li
Yu Liu
Huiming Song
Changfeng Sun
Jiachuan Wang
Yalan Yan
Qiufang Cai
Meng Ren
author_sort Wenxuan Pang
title Precipitation Variations in China’s Altay Mountains Detected from Tree Rings Dating Back to AD 1615
title_short Precipitation Variations in China’s Altay Mountains Detected from Tree Rings Dating Back to AD 1615
title_full Precipitation Variations in China’s Altay Mountains Detected from Tree Rings Dating Back to AD 1615
title_fullStr Precipitation Variations in China’s Altay Mountains Detected from Tree Rings Dating Back to AD 1615
title_full_unstemmed Precipitation Variations in China’s Altay Mountains Detected from Tree Rings Dating Back to AD 1615
title_sort precipitation variations in china’s altay mountains detected from tree rings dating back to ad 1615
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/f14071496
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Forests; Volume 14; Issue 7; Pages: 1496
op_relation Forest Meteorology and Climate Change
https://dx.doi.org/10.3390/f14071496
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/f14071496
container_title Forests
container_volume 14
container_issue 7
container_start_page 1496
_version_ 1774715111253999616