Little Ice Age cooling in the Western Hengduan Mountains, China: a 600-year warm-season temperature reconstruction from tree rings
The distributions of forest, ice and snow in the Hengduan Mountains of China have undergone significant changes due to ongoing climatic warming. To better understand the spatiotemporal pattern of temperature changes in the Hengduan Mountains, we used tree-ring cores collected from multiple individua...
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| Veröffentlicht in: | Climate dynamics 2024, Vol.62 (1), p.773-790 |
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| creator | Yue, Weipeng Chen, Feng Davi, Nicole K. Zhang, Heli Chen, Youping Zhao, Xiaoen Gao, Zhihong |
| description | The distributions of forest, ice and snow in the Hengduan Mountains of China have undergone significant changes due to ongoing climatic warming. To better understand the spatiotemporal pattern of temperature changes in the Hengduan Mountains, we used tree-ring cores collected from multiple individuals of
Larix speciosa Cheng et Law
at five sites to develop a regional chronology and to establish the relationship between tree-ring radial growth and warm-season (May–September) mean temperature. The regional chronology accounts for 46.1% of the observed variance in the warm season and was used to reconstruct regional temperature levels back to 1420. Four cool intervals (1490–1570, 1590–1660, 1700–1790, and 1800–1880) indicate that the Western Hengduan Mountains experienced the Little Ice Age, and the changes were synchronous with cooling on the Tibetan Plateau and in the Northern Hemisphere, demonstrating a well-defined Little Ice Age signal in the South Asian monsoon region. Air–sea interactions and solar activity affected the variability of the warm-season mean temperature variations on interannual or interdecadal scales. Our temperature reconstruction improves the understanding of multi-centennial climate change in the Western Hengduan Mountains and has implications for advancing high-resolution paleoclimate science in the region. |
| doi_str_mv | 10.1007/s00382-023-06932-2 |
| format | Article |
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Larix speciosa Cheng et Law
at five sites to develop a regional chronology and to establish the relationship between tree-ring radial growth and warm-season (May–September) mean temperature. The regional chronology accounts for 46.1% of the observed variance in the warm season and was used to reconstruct regional temperature levels back to 1420. Four cool intervals (1490–1570, 1590–1660, 1700–1790, and 1800–1880) indicate that the Western Hengduan Mountains experienced the Little Ice Age, and the changes were synchronous with cooling on the Tibetan Plateau and in the Northern Hemisphere, demonstrating a well-defined Little Ice Age signal in the South Asian monsoon region. Air–sea interactions and solar activity affected the variability of the warm-season mean temperature variations on interannual or interdecadal scales. Our temperature reconstruction improves the understanding of multi-centennial climate change in the Western Hengduan Mountains and has implications for advancing high-resolution paleoclimate science in the region.</description><identifier>ISSN: 0930-7575</identifier><identifier>EISSN: 1432-0894</identifier><identifier>DOI: 10.1007/s00382-023-06932-2</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Air-sea interaction ; Chronology ; Climate change ; Climatology ; Cooling ; Cores ; Earth and Environmental Science ; Earth Sciences ; Geophysics/Geodesy ; Global warming ; Ice ages ; Little Ice Age ; Mean temperatures ; Mountains ; Northern Hemisphere ; Oceanography ; Paleoclimate ; Regional development ; Seasons ; Solar activity ; South Asian monsoon ; Temperature ; Temperature changes ; Temperature variations ; Tree rings ; Trees ; Warm seasons</subject><ispartof>Climate dynamics, 2024, Vol.62 (1), p.773-790</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c319t-9815ed06c000cc8f844a685d62663aa02c1ea916738da9b870275d07977461803</citedby><cites>FETCH-LOGICAL-c319t-9815ed06c000cc8f844a685d62663aa02c1ea916738da9b870275d07977461803</cites><orcidid>0000-0002-2551-8653</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00382-023-06932-2$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00382-023-06932-2$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Yue, Weipeng</creatorcontrib><creatorcontrib>Chen, Feng</creatorcontrib><creatorcontrib>Davi, Nicole K.</creatorcontrib><creatorcontrib>Zhang, Heli</creatorcontrib><creatorcontrib>Chen, Youping</creatorcontrib><creatorcontrib>Zhao, Xiaoen</creatorcontrib><creatorcontrib>Gao, Zhihong</creatorcontrib><title>Little Ice Age cooling in the Western Hengduan Mountains, China: a 600-year warm-season temperature reconstruction from tree rings</title><title>Climate dynamics</title><addtitle>Clim Dyn</addtitle><description>The distributions of forest, ice and snow in the Hengduan Mountains of China have undergone significant changes due to ongoing climatic warming. To better understand the spatiotemporal pattern of temperature changes in the Hengduan Mountains, we used tree-ring cores collected from multiple individuals of
Larix speciosa Cheng et Law
at five sites to develop a regional chronology and to establish the relationship between tree-ring radial growth and warm-season (May–September) mean temperature. The regional chronology accounts for 46.1% of the observed variance in the warm season and was used to reconstruct regional temperature levels back to 1420. Four cool intervals (1490–1570, 1590–1660, 1700–1790, and 1800–1880) indicate that the Western Hengduan Mountains experienced the Little Ice Age, and the changes were synchronous with cooling on the Tibetan Plateau and in the Northern Hemisphere, demonstrating a well-defined Little Ice Age signal in the South Asian monsoon region. Air–sea interactions and solar activity affected the variability of the warm-season mean temperature variations on interannual or interdecadal scales. Our temperature reconstruction improves the understanding of multi-centennial climate change in the Western Hengduan Mountains and has implications for advancing high-resolution paleoclimate science in the region.</description><subject>Air-sea interaction</subject><subject>Chronology</subject><subject>Climate change</subject><subject>Climatology</subject><subject>Cooling</subject><subject>Cores</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geophysics/Geodesy</subject><subject>Global warming</subject><subject>Ice ages</subject><subject>Little Ice Age</subject><subject>Mean temperatures</subject><subject>Mountains</subject><subject>Northern Hemisphere</subject><subject>Oceanography</subject><subject>Paleoclimate</subject><subject>Regional development</subject><subject>Seasons</subject><subject>Solar activity</subject><subject>South Asian monsoon</subject><subject>Temperature</subject><subject>Temperature changes</subject><subject>Temperature variations</subject><subject>Tree rings</subject><subject>Trees</subject><subject>Warm seasons</subject><issn>0930-7575</issn><issn>1432-0894</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp9UMtOGzEUtVCRSKE_wMoSW9xe2zN-sENRWyIFsaHq0nI9N8mgxA62R4g1P8K38GU1TaXuurpXOi-dQ8g5h88cQH8pANIIBkIyUFYKJo7IjHftAWO7D2QGVgLTve5PyMdSHgB4p7SYkZflWOsW6SIgvV4jDSltx7imY6R1g_Qnloo5vr3eYFwPk4_0Nk2x-jGWSzrfjNFfUU8VAHtGn-mTzztW0JfU5LjbY_Z1ykgzhhRLzVOoY4NWOe1ozdiAllXOyPHKbwt--ntPyY9vX-_nN2x5930xv16yILmtzBre4wAqAEAIZmW6zivTD0ooJb0HETh6y5WWZvD2l9EgdD-Atlp3ihuQp-Ti4LvP6XFqzdxDmnJskU5YrjVwK7vGEgdWyKmUjCu3z-PO52fHwb2P7Q5juza2-zO2E00kD6Kyf6-E-Z_1f1S_AYzbglU</recordid><startdate>2024</startdate><enddate>2024</enddate><creator>Yue, Weipeng</creator><creator>Chen, Feng</creator><creator>Davi, Nicole K.</creator><creator>Zhang, Heli</creator><creator>Chen, Youping</creator><creator>Zhao, Xiaoen</creator><creator>Gao, Zhihong</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0002-2551-8653</orcidid></search><sort><creationdate>2024</creationdate><title>Little Ice Age cooling in the Western Hengduan Mountains, China: a 600-year warm-season temperature reconstruction from tree rings</title><author>Yue, Weipeng ; Chen, Feng ; Davi, Nicole K. ; Zhang, Heli ; Chen, Youping ; Zhao, Xiaoen ; Gao, Zhihong</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c319t-9815ed06c000cc8f844a685d62663aa02c1ea916738da9b870275d07977461803</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Air-sea interaction</topic><topic>Chronology</topic><topic>Climate change</topic><topic>Climatology</topic><topic>Cooling</topic><topic>Cores</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geophysics/Geodesy</topic><topic>Global warming</topic><topic>Ice ages</topic><topic>Little Ice Age</topic><topic>Mean temperatures</topic><topic>Mountains</topic><topic>Northern Hemisphere</topic><topic>Oceanography</topic><topic>Paleoclimate</topic><topic>Regional development</topic><topic>Seasons</topic><topic>Solar activity</topic><topic>South Asian monsoon</topic><topic>Temperature</topic><topic>Temperature changes</topic><topic>Temperature variations</topic><topic>Tree rings</topic><topic>Trees</topic><topic>Warm seasons</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yue, Weipeng</creatorcontrib><creatorcontrib>Chen, Feng</creatorcontrib><creatorcontrib>Davi, Nicole K.</creatorcontrib><creatorcontrib>Zhang, Heli</creatorcontrib><creatorcontrib>Chen, Youping</creatorcontrib><creatorcontrib>Zhao, Xiaoen</creatorcontrib><creatorcontrib>Gao, Zhihong</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Climate dynamics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yue, Weipeng</au><au>Chen, Feng</au><au>Davi, Nicole K.</au><au>Zhang, Heli</au><au>Chen, Youping</au><au>Zhao, Xiaoen</au><au>Gao, Zhihong</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Little Ice Age cooling in the Western Hengduan Mountains, China: a 600-year warm-season temperature reconstruction from tree rings</atitle><jtitle>Climate dynamics</jtitle><stitle>Clim Dyn</stitle><date>2024</date><risdate>2024</risdate><volume>62</volume><issue>1</issue><spage>773</spage><epage>790</epage><pages>773-790</pages><issn>0930-7575</issn><eissn>1432-0894</eissn><abstract>The distributions of forest, ice and snow in the Hengduan Mountains of China have undergone significant changes due to ongoing climatic warming. To better understand the spatiotemporal pattern of temperature changes in the Hengduan Mountains, we used tree-ring cores collected from multiple individuals of
Larix speciosa Cheng et Law
at five sites to develop a regional chronology and to establish the relationship between tree-ring radial growth and warm-season (May–September) mean temperature. The regional chronology accounts for 46.1% of the observed variance in the warm season and was used to reconstruct regional temperature levels back to 1420. Four cool intervals (1490–1570, 1590–1660, 1700–1790, and 1800–1880) indicate that the Western Hengduan Mountains experienced the Little Ice Age, and the changes were synchronous with cooling on the Tibetan Plateau and in the Northern Hemisphere, demonstrating a well-defined Little Ice Age signal in the South Asian monsoon region. Air–sea interactions and solar activity affected the variability of the warm-season mean temperature variations on interannual or interdecadal scales. Our temperature reconstruction improves the understanding of multi-centennial climate change in the Western Hengduan Mountains and has implications for advancing high-resolution paleoclimate science in the region.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00382-023-06932-2</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0002-2551-8653</orcidid></addata></record> |
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| subjects | Air-sea interaction Chronology Climate change Climatology Cooling Cores Earth and Environmental Science Earth Sciences Geophysics/Geodesy Global warming Ice ages Little Ice Age Mean temperatures Mountains Northern Hemisphere Oceanography Paleoclimate Regional development Seasons Solar activity South Asian monsoon Temperature Temperature changes Temperature variations Tree rings Trees Warm seasons |
| title | Little Ice Age cooling in the Western Hengduan Mountains, China: a 600-year warm-season temperature reconstruction from tree rings |
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