A 258-year reconstruction of precipitation for southern Northeast China and the northern Korean peninsula
Abstract We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the vari...
Ausführliche Beschreibung
Autor*in: |
Chen, Zhenju [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2016 |
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Systematik: |
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Anmerkung: |
© Springer Science+Business Media Dordrecht 2016 |
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Übergeordnetes Werk: |
Enthalten in: Climatic change - Springer Netherlands, 1977, 139(2016), 3-4 vom: 09. Sept., Seite 609-622 |
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Übergeordnetes Werk: |
volume:139 ; year:2016 ; number:3-4 ; day:09 ; month:09 ; pages:609-622 |
Links: |
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DOI / URN: |
10.1007/s10584-016-1796-9 |
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Katalog-ID: |
OLC2062621469 |
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520 | |a Abstract We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the variability of the reconstruction, and identify the leading rainfall patterns and regional dryness and wetness modes during the latest 2.5 centuries. This reconstruction shows that three persistent dry decades occurred during the 1840s, 1910s and 1850s and the three wettest decades occurred during the 1770s, 1820s and 1930s. The five years with lowest rainfall were 1759, 1917, 1841, 1747 and 1839, and 1770, 1938, 1819, 1941 and 1822 were the five years with highest rainfall, respectively. As indicated by the spatial correlation patterns, the reconstruction also exhibits regional characteristics. The variation of reconstructed rainfall significantly corresponds to East Asian monsoon. | ||
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10.1007/s10584-016-1796-9 doi (DE-627)OLC2062621469 (DE-He213)s10584-016-1796-9-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Chen, Zhenju verfasserin aut A 258-year reconstruction of precipitation for southern Northeast China and the northern Korean peninsula 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media Dordrecht 2016 Abstract We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the variability of the reconstruction, and identify the leading rainfall patterns and regional dryness and wetness modes during the latest 2.5 centuries. This reconstruction shows that three persistent dry decades occurred during the 1840s, 1910s and 1850s and the three wettest decades occurred during the 1770s, 1820s and 1930s. The five years with lowest rainfall were 1759, 1917, 1841, 1747 and 1839, and 1770, 1938, 1819, 1941 and 1822 were the five years with highest rainfall, respectively. As indicated by the spatial correlation patterns, the reconstruction also exhibits regional characteristics. The variation of reconstructed rainfall significantly corresponds to East Asian monsoon. Tree Ring East Asian Summer Monsoon East Asian Monsoon Winter East Asian Monsoon Changbai Mountain He, Xingyuan aut Davi, Nicole K. aut Zhang, Xianliang aut Enthalten in Climatic change Springer Netherlands, 1977 139(2016), 3-4 vom: 09. Sept., Seite 609-622 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:139 year:2016 number:3-4 day:09 month:09 pages:609-622 https://doi.org/10.1007/s10584-016-1796-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 RA 1000 AR 139 2016 3-4 09 09 609-622 |
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10.1007/s10584-016-1796-9 doi (DE-627)OLC2062621469 (DE-He213)s10584-016-1796-9-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Chen, Zhenju verfasserin aut A 258-year reconstruction of precipitation for southern Northeast China and the northern Korean peninsula 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media Dordrecht 2016 Abstract We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the variability of the reconstruction, and identify the leading rainfall patterns and regional dryness and wetness modes during the latest 2.5 centuries. This reconstruction shows that three persistent dry decades occurred during the 1840s, 1910s and 1850s and the three wettest decades occurred during the 1770s, 1820s and 1930s. The five years with lowest rainfall were 1759, 1917, 1841, 1747 and 1839, and 1770, 1938, 1819, 1941 and 1822 were the five years with highest rainfall, respectively. As indicated by the spatial correlation patterns, the reconstruction also exhibits regional characteristics. The variation of reconstructed rainfall significantly corresponds to East Asian monsoon. Tree Ring East Asian Summer Monsoon East Asian Monsoon Winter East Asian Monsoon Changbai Mountain He, Xingyuan aut Davi, Nicole K. aut Zhang, Xianliang aut Enthalten in Climatic change Springer Netherlands, 1977 139(2016), 3-4 vom: 09. Sept., Seite 609-622 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:139 year:2016 number:3-4 day:09 month:09 pages:609-622 https://doi.org/10.1007/s10584-016-1796-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 RA 1000 AR 139 2016 3-4 09 09 609-622 |
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10.1007/s10584-016-1796-9 doi (DE-627)OLC2062621469 (DE-He213)s10584-016-1796-9-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Chen, Zhenju verfasserin aut A 258-year reconstruction of precipitation for southern Northeast China and the northern Korean peninsula 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media Dordrecht 2016 Abstract We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the variability of the reconstruction, and identify the leading rainfall patterns and regional dryness and wetness modes during the latest 2.5 centuries. This reconstruction shows that three persistent dry decades occurred during the 1840s, 1910s and 1850s and the three wettest decades occurred during the 1770s, 1820s and 1930s. The five years with lowest rainfall were 1759, 1917, 1841, 1747 and 1839, and 1770, 1938, 1819, 1941 and 1822 were the five years with highest rainfall, respectively. As indicated by the spatial correlation patterns, the reconstruction also exhibits regional characteristics. The variation of reconstructed rainfall significantly corresponds to East Asian monsoon. Tree Ring East Asian Summer Monsoon East Asian Monsoon Winter East Asian Monsoon Changbai Mountain He, Xingyuan aut Davi, Nicole K. aut Zhang, Xianliang aut Enthalten in Climatic change Springer Netherlands, 1977 139(2016), 3-4 vom: 09. Sept., Seite 609-622 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:139 year:2016 number:3-4 day:09 month:09 pages:609-622 https://doi.org/10.1007/s10584-016-1796-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 RA 1000 AR 139 2016 3-4 09 09 609-622 |
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10.1007/s10584-016-1796-9 doi (DE-627)OLC2062621469 (DE-He213)s10584-016-1796-9-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Chen, Zhenju verfasserin aut A 258-year reconstruction of precipitation for southern Northeast China and the northern Korean peninsula 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media Dordrecht 2016 Abstract We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the variability of the reconstruction, and identify the leading rainfall patterns and regional dryness and wetness modes during the latest 2.5 centuries. This reconstruction shows that three persistent dry decades occurred during the 1840s, 1910s and 1850s and the three wettest decades occurred during the 1770s, 1820s and 1930s. The five years with lowest rainfall were 1759, 1917, 1841, 1747 and 1839, and 1770, 1938, 1819, 1941 and 1822 were the five years with highest rainfall, respectively. As indicated by the spatial correlation patterns, the reconstruction also exhibits regional characteristics. The variation of reconstructed rainfall significantly corresponds to East Asian monsoon. Tree Ring East Asian Summer Monsoon East Asian Monsoon Winter East Asian Monsoon Changbai Mountain He, Xingyuan aut Davi, Nicole K. aut Zhang, Xianliang aut Enthalten in Climatic change Springer Netherlands, 1977 139(2016), 3-4 vom: 09. Sept., Seite 609-622 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:139 year:2016 number:3-4 day:09 month:09 pages:609-622 https://doi.org/10.1007/s10584-016-1796-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 RA 1000 AR 139 2016 3-4 09 09 609-622 |
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10.1007/s10584-016-1796-9 doi (DE-627)OLC2062621469 (DE-He213)s10584-016-1796-9-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Chen, Zhenju verfasserin aut A 258-year reconstruction of precipitation for southern Northeast China and the northern Korean peninsula 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media Dordrecht 2016 Abstract We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the variability of the reconstruction, and identify the leading rainfall patterns and regional dryness and wetness modes during the latest 2.5 centuries. This reconstruction shows that three persistent dry decades occurred during the 1840s, 1910s and 1850s and the three wettest decades occurred during the 1770s, 1820s and 1930s. The five years with lowest rainfall were 1759, 1917, 1841, 1747 and 1839, and 1770, 1938, 1819, 1941 and 1822 were the five years with highest rainfall, respectively. As indicated by the spatial correlation patterns, the reconstruction also exhibits regional characteristics. The variation of reconstructed rainfall significantly corresponds to East Asian monsoon. Tree Ring East Asian Summer Monsoon East Asian Monsoon Winter East Asian Monsoon Changbai Mountain He, Xingyuan aut Davi, Nicole K. aut Zhang, Xianliang aut Enthalten in Climatic change Springer Netherlands, 1977 139(2016), 3-4 vom: 09. Sept., Seite 609-622 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:139 year:2016 number:3-4 day:09 month:09 pages:609-622 https://doi.org/10.1007/s10584-016-1796-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 RA 1000 AR 139 2016 3-4 09 09 609-622 |
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A 258-year reconstruction of precipitation for southern Northeast China and the northern Korean peninsula |
abstract |
Abstract We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the variability of the reconstruction, and identify the leading rainfall patterns and regional dryness and wetness modes during the latest 2.5 centuries. This reconstruction shows that three persistent dry decades occurred during the 1840s, 1910s and 1850s and the three wettest decades occurred during the 1770s, 1820s and 1930s. The five years with lowest rainfall were 1759, 1917, 1841, 1747 and 1839, and 1770, 1938, 1819, 1941 and 1822 were the five years with highest rainfall, respectively. As indicated by the spatial correlation patterns, the reconstruction also exhibits regional characteristics. The variation of reconstructed rainfall significantly corresponds to East Asian monsoon. © Springer Science+Business Media Dordrecht 2016 |
abstractGer |
Abstract We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the variability of the reconstruction, and identify the leading rainfall patterns and regional dryness and wetness modes during the latest 2.5 centuries. This reconstruction shows that three persistent dry decades occurred during the 1840s, 1910s and 1850s and the three wettest decades occurred during the 1770s, 1820s and 1930s. The five years with lowest rainfall were 1759, 1917, 1841, 1747 and 1839, and 1770, 1938, 1819, 1941 and 1822 were the five years with highest rainfall, respectively. As indicated by the spatial correlation patterns, the reconstruction also exhibits regional characteristics. The variation of reconstructed rainfall significantly corresponds to East Asian monsoon. © Springer Science+Business Media Dordrecht 2016 |
abstract_unstemmed |
Abstract We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the variability of the reconstruction, and identify the leading rainfall patterns and regional dryness and wetness modes during the latest 2.5 centuries. This reconstruction shows that three persistent dry decades occurred during the 1840s, 1910s and 1850s and the three wettest decades occurred during the 1770s, 1820s and 1930s. The five years with lowest rainfall were 1759, 1917, 1841, 1747 and 1839, and 1770, 1938, 1819, 1941 and 1822 were the five years with highest rainfall, respectively. As indicated by the spatial correlation patterns, the reconstruction also exhibits regional characteristics. The variation of reconstructed rainfall significantly corresponds to East Asian monsoon. © Springer Science+Business Media Dordrecht 2016 |
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container_issue |
3-4 |
title_short |
A 258-year reconstruction of precipitation for southern Northeast China and the northern Korean peninsula |
url |
https://doi.org/10.1007/s10584-016-1796-9 |
remote_bool |
false |
author2 |
He, Xingyuan Davi, Nicole K. Zhang, Xianliang |
author2Str |
He, Xingyuan Davi, Nicole K. Zhang, Xianliang |
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hochschulschrift_bool |
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doi_str |
10.1007/s10584-016-1796-9 |
up_date |
2024-07-03T15:48:40.408Z |
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1803573495496441856 |
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