Late Quaternary temperature changes seen in world-wide continental heat flow measurements
Analysis of more than six thousand continental heat flow measurements as a function of depth has yielded a reconstruction of a global average ground surface temperature history over the last 20,000 years. The early to mid‐Holocene appears as a relatively long warm interval some 0.2–0.6 K above prese...
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| Veröffentlicht in: | Geophysical research letters 1997-08, Vol.24 (15), p.1947-1950 |
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| container_end_page | 1950 |
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| container_issue | 15 |
| container_start_page | 1947 |
| container_title | Geophysical research letters |
| container_volume | 24 |
| creator | Huang, Shaopeng Pollack, Henry N. Shen, Po Yu |
| description | Analysis of more than six thousand continental heat flow measurements as a function of depth has yielded a reconstruction of a global average ground surface temperature history over the last 20,000 years. The early to mid‐Holocene appears as a relatively long warm interval some 0.2–0.6 K above present‐day temperatures, the culmination of the warming that followed the end of the last glaciation. Temperatures were also warmer than present 500–1,000 years ago, but then cooled to a minimum some 0.2–0.7 K below present about 200 years ago. Although temperature variations in this type of reconstruction are highly smoothed, the results clearly resemble the broad outlines of late Quaternary climate changes suggested by proxies. |
| doi_str_mv | 10.1029/97GL01846 |
| format | Article |
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The early to mid‐Holocene appears as a relatively long warm interval some 0.2–0.6 K above present‐day temperatures, the culmination of the warming that followed the end of the last glaciation. Temperatures were also warmer than present 500–1,000 years ago, but then cooled to a minimum some 0.2–0.7 K below present about 200 years ago. Although temperature variations in this type of reconstruction are highly smoothed, the results clearly resemble the broad outlines of late Quaternary climate changes suggested by proxies.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/97GL01846</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Geophysics: general, magnetic, electric and thermic methods and properties ; Internal geophysics ; Marine and continental quaternary ; Surficial geology</subject><ispartof>Geophysical research letters, 1997-08, Vol.24 (15), p.1947-1950</ispartof><rights>Copyright 1997 by the American Geophysical Union.</rights><rights>1997 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4008-90caeab1164bcc6e1aabee6adde9a0a66ae8984adc4038097c06886b2dd3d3373</citedby><cites>FETCH-LOGICAL-c4008-90caeab1164bcc6e1aabee6adde9a0a66ae8984adc4038097c06886b2dd3d3373</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F97GL01846$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F97GL01846$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1416,1432,11513,27923,27924,45573,45574,46408,46467,46832,46891</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=2783225$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Huang, Shaopeng</creatorcontrib><creatorcontrib>Pollack, Henry N.</creatorcontrib><creatorcontrib>Shen, Po Yu</creatorcontrib><title>Late Quaternary temperature changes seen in world-wide continental heat flow measurements</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>Analysis of more than six thousand continental heat flow measurements as a function of depth has yielded a reconstruction of a global average ground surface temperature history over the last 20,000 years. The early to mid‐Holocene appears as a relatively long warm interval some 0.2–0.6 K above present‐day temperatures, the culmination of the warming that followed the end of the last glaciation. Temperatures were also warmer than present 500–1,000 years ago, but then cooled to a minimum some 0.2–0.7 K below present about 200 years ago. Although temperature variations in this type of reconstruction are highly smoothed, the results clearly resemble the broad outlines of late Quaternary climate changes suggested by proxies.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Geophysics: general, magnetic, electric and thermic methods and properties</subject><subject>Internal geophysics</subject><subject>Marine and continental quaternary</subject><subject>Surficial geology</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1997</creationdate><recordtype>article</recordtype><recordid>eNp1kE1LAzEQhoMoWKsH_0EOInhYnWzWbPYoflRhUSpK9RSm2amu7mZrsqX6702p9OYlCZPneWFexg4FnApIi7MiH5UgdKa22EAUWZZogHybDQCK-E5ztcv2QvgAAAlSDNhriT3x8SKe3qH_4T21c_LYLzxx-47ujQIPRI7Xji8731TJsq7iV-f62pHrseHvhD2fNd2St4Qhim2ch322M8Mm0MHfPWTPN9dPl7dJ-TC6u7woE5sB6KQAi4RTIVQ2tVaRQJwSKawqKhBQKSRd6AyriEsNRW5Baa2maVXJSspcDtnxOnfuu68Fhd60dbDUNOioWwQjtJCw2nfITtag9V0InmZm7us27mwEmFV5ZlNeZI_-QjFYbGYena3DRkhzLdP0PGJna2xZN_Tzf54ZPZYi9q2jkayNOvT0vTHQfxqVy_zcTO5HBibZy3g8npgr-QveRI06</recordid><startdate>19970801</startdate><enddate>19970801</enddate><creator>Huang, Shaopeng</creator><creator>Pollack, Henry N.</creator><creator>Shen, Po Yu</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope></search><sort><creationdate>19970801</creationdate><title>Late Quaternary temperature changes seen in world-wide continental heat flow measurements</title><author>Huang, Shaopeng ; Pollack, Henry N. ; Shen, Po Yu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4008-90caeab1164bcc6e1aabee6adde9a0a66ae8984adc4038097c06886b2dd3d3373</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1997</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Geophysics: general, magnetic, electric and thermic methods and properties</topic><topic>Internal geophysics</topic><topic>Marine and continental quaternary</topic><topic>Surficial geology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Huang, Shaopeng</creatorcontrib><creatorcontrib>Pollack, Henry N.</creatorcontrib><creatorcontrib>Shen, Po Yu</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Huang, Shaopeng</au><au>Pollack, Henry N.</au><au>Shen, Po Yu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Late Quaternary temperature changes seen in world-wide continental heat flow measurements</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>1997-08-01</date><risdate>1997</risdate><volume>24</volume><issue>15</issue><spage>1947</spage><epage>1950</epage><pages>1947-1950</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>Analysis of more than six thousand continental heat flow measurements as a function of depth has yielded a reconstruction of a global average ground surface temperature history over the last 20,000 years. The early to mid‐Holocene appears as a relatively long warm interval some 0.2–0.6 K above present‐day temperatures, the culmination of the warming that followed the end of the last glaciation. Temperatures were also warmer than present 500–1,000 years ago, but then cooled to a minimum some 0.2–0.7 K below present about 200 years ago. 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| ispartof | Geophysical research letters, 1997-08, Vol.24 (15), p.1947-1950 |
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| language | eng |
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| source | Wiley Free Content; Wiley-Blackwell AGU Digital Library; EZB-FREE-00999 freely available EZB journals; Wiley Online Library All Journals |
| subjects | Earth sciences Earth, ocean, space Exact sciences and technology Geophysics: general, magnetic, electric and thermic methods and properties Internal geophysics Marine and continental quaternary Surficial geology |
| title | Late Quaternary temperature changes seen in world-wide continental heat flow measurements |
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