Projected Climate Change against Natural Internal Variability over China
The ability of 42 Coupled Model Intercomparison Project Phase 5(CMIP5) models in simulating the annual and seasonal temperature and precipitation over China is first examined by using their historical experiments for 1986–2005, and then 39 relatively reliable models are chosen to project temperature...
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Veröffentlicht in: | Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao 2015, Vol.8 (4), p.193-200 |
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creator | Jiang, Jiang Yue, Sui Xian-Mei, Lang |
description | The ability of 42 Coupled Model Intercomparison Project Phase 5(CMIP5) models in simulating the annual and seasonal temperature and precipitation over China is first examined by using their historical experiments for 1986–2005, and then 39 relatively reliable models are chosen to project temperature and precipitation changes against the natural internal variability over the country under the Representative Concentration Pathways(RCP) scenarios in the 21 st century. The result shows the temperature continuing to increase, especially in northern China. The annual warming for 2081–2099 relative to 1986–2005 over the whole of the country is larger than the background variability, with the multimodel median changes under RCP2.6, RCP4.5, RCP6.0, and RCP8.5 being 9.9, 19.3, 22.8, and 35.9 times greater than one standard deviation of internal variability, respectively. The annual precipitation is projected to increase by 6.1%, 9.3%, 9.6%, and 16.2% for 2081–2099 relative to 1986–2005 under RCP2.6, RCP4.5, RCP6.0, and RCP8.5 respectively, while large changes with high model agreement only occur over the northern Tibetan Plateau and Northeast China, which is mainly due to the robust changes in winter and spring under RCP6.0 and RCP8.5. |
doi_str_mv | 10.1080/16742834.2015.11447259 |
format | Article |
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The result shows the temperature continuing to increase, especially in northern China. The annual warming for 2081–2099 relative to 1986–2005 over the whole of the country is larger than the background variability, with the multimodel median changes under RCP2.6, RCP4.5, RCP6.0, and RCP8.5 being 9.9, 19.3, 22.8, and 35.9 times greater than one standard deviation of internal variability, respectively. The annual precipitation is projected to increase by 6.1%, 9.3%, 9.6%, and 16.2% for 2081–2099 relative to 1986–2005 under RCP2.6, RCP4.5, RCP6.0, and RCP8.5 respectively, while large changes with high model agreement only occur over the northern Tibetan Plateau and Northeast China, which is mainly due to the robust changes in winter and spring under RCP6.0 and RCP8.5.</description><identifier>ISSN: 1674-2834</identifier><identifier>EISSN: 2376-6123</identifier><identifier>DOI: 10.1080/16742834.2015.11447259</identifier><language>eng</language><subject>中国东北地区 ; 中国北方 ; 变异 ; 模型模拟 ; 气候变化 ; 自然 ; 降水变化 ; 青藏高原北部</subject><ispartof>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao, 2015, Vol.8 (4), p.193-200</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c282t-c5aac2beb11ae5c62ac974b7e8f42d1d10ba2e7a482676de747c295ef630059f3</citedby><cites>FETCH-LOGICAL-c282t-c5aac2beb11ae5c62ac974b7e8f42d1d10ba2e7a482676de747c295ef630059f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/89435X/89435X.jpg</thumbnail><link.rule.ids>315,781,785,4025,27928,27929,27930</link.rule.ids></links><search><creatorcontrib>Jiang, Jiang</creatorcontrib><creatorcontrib>Yue, Sui</creatorcontrib><creatorcontrib>Xian-Mei, Lang</creatorcontrib><title>Projected Climate Change against Natural Internal Variability over China</title><title>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao</title><addtitle>Atmospheric and Oceanic Science Letters</addtitle><description>The ability of 42 Coupled Model Intercomparison Project Phase 5(CMIP5) models in simulating the annual and seasonal temperature and precipitation over China is first examined by using their historical experiments for 1986–2005, and then 39 relatively reliable models are chosen to project temperature and precipitation changes against the natural internal variability over the country under the Representative Concentration Pathways(RCP) scenarios in the 21 st century. The result shows the temperature continuing to increase, especially in northern China. The annual warming for 2081–2099 relative to 1986–2005 over the whole of the country is larger than the background variability, with the multimodel median changes under RCP2.6, RCP4.5, RCP6.0, and RCP8.5 being 9.9, 19.3, 22.8, and 35.9 times greater than one standard deviation of internal variability, respectively. The annual precipitation is projected to increase by 6.1%, 9.3%, 9.6%, and 16.2% for 2081–2099 relative to 1986–2005 under RCP2.6, RCP4.5, RCP6.0, and RCP8.5 respectively, while large changes with high model agreement only occur over the northern Tibetan Plateau and Northeast China, which is mainly due to the robust changes in winter and spring under RCP6.0 and RCP8.5.</description><subject>中国东北地区</subject><subject>中国北方</subject><subject>变异</subject><subject>模型模拟</subject><subject>气候变化</subject><subject>自然</subject><subject>降水变化</subject><subject>青藏高原北部</subject><issn>1674-2834</issn><issn>2376-6123</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><recordid>eNo9kE1Lw0AURQdRMNT-BQnuU-crM8lSgtpCURfqNrxMXtIpcaIzo9B_b4Ktq_cW91wuh5BrRleMFvSWKS15IeSKU5avGJNS87w8IwkXWmWKcXFOkjmUzalLsgxhTyllgitNRULWL37co4nYptVgPyBiWu3A9ZhCD9aFmD5B_PYwpBsX0bvpeQdvobGDjYd0_EE_AdbBFbnoYAi4PN4FeXu4f63W2fb5cVPdbTPDCx4zkwMY3mDDGGBuFAdTatloLDrJW9Yy2gBHDbKYBqoWtdSGlzl2SlCal51YEPXXa_wYgseu_vTTbn-oGa1nJfVJST0rqU9KJvDmCO5G139Z1_-TSkldCCqE-AXOLV-Z</recordid><startdate>2015</startdate><enddate>2015</enddate><creator>Jiang, Jiang</creator><creator>Yue, Sui</creator><creator>Xian-Mei, Lang</creator><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>2015</creationdate><title>Projected Climate Change against Natural Internal Variability over China</title><author>Jiang, Jiang ; Yue, Sui ; Xian-Mei, Lang</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c282t-c5aac2beb11ae5c62ac974b7e8f42d1d10ba2e7a482676de747c295ef630059f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>中国东北地区</topic><topic>中国北方</topic><topic>变异</topic><topic>模型模拟</topic><topic>气候变化</topic><topic>自然</topic><topic>降水变化</topic><topic>青藏高原北部</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Jiang, Jiang</creatorcontrib><creatorcontrib>Yue, Sui</creatorcontrib><creatorcontrib>Xian-Mei, Lang</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><jtitle>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Jiang, Jiang</au><au>Yue, Sui</au><au>Xian-Mei, Lang</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Projected Climate Change against Natural Internal Variability over China</atitle><jtitle>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao</jtitle><addtitle>Atmospheric and Oceanic Science Letters</addtitle><date>2015</date><risdate>2015</risdate><volume>8</volume><issue>4</issue><spage>193</spage><epage>200</epage><pages>193-200</pages><issn>1674-2834</issn><eissn>2376-6123</eissn><abstract>The ability of 42 Coupled Model Intercomparison Project Phase 5(CMIP5) models in simulating the annual and seasonal temperature and precipitation over China is first examined by using their historical experiments for 1986–2005, and then 39 relatively reliable models are chosen to project temperature and precipitation changes against the natural internal variability over the country under the Representative Concentration Pathways(RCP) scenarios in the 21 st century. The result shows the temperature continuing to increase, especially in northern China. The annual warming for 2081–2099 relative to 1986–2005 over the whole of the country is larger than the background variability, with the multimodel median changes under RCP2.6, RCP4.5, RCP6.0, and RCP8.5 being 9.9, 19.3, 22.8, and 35.9 times greater than one standard deviation of internal variability, respectively. The annual precipitation is projected to increase by 6.1%, 9.3%, 9.6%, and 16.2% for 2081–2099 relative to 1986–2005 under RCP2.6, RCP4.5, RCP6.0, and RCP8.5 respectively, while large changes with high model agreement only occur over the northern Tibetan Plateau and Northeast China, which is mainly due to the robust changes in winter and spring under RCP6.0 and RCP8.5.</abstract><doi>10.1080/16742834.2015.11447259</doi><tpages>8</tpages></addata></record> |
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source | Access via Taylor & Francis (Open Access Collection); EZB-FREE-00999 freely available EZB journals |
subjects | 中国东北地区 中国北方 变异 模型模拟 气候变化 自然 降水变化 青藏高原北部 |
title | Projected Climate Change against Natural Internal Variability over China |
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