Quantifying Global Warming from the Retreat of Glaciers
Records of glacier fluctuations compiled by the World Glacier Monitoring Service can be used to derive an independent estimate of global warming during the last 100 years. Records of different glaciers are made comparable by a two-step scaling procedure: one allowing for differences in glacier geome...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 1994-04, Vol.264 (5156), p.243-245 |
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| creator | Oerlemans, Johannes |
| description | Records of glacier fluctuations compiled by the World Glacier Monitoring Service can be used to derive an independent estimate of global warming during the last 100 years. Records of different glaciers are made comparable by a two-step scaling procedure: one allowing for differences in glacier geometry, the other for differences in climate sensitivity. The retreat of glaciers during the last 100 years appears to be coherent over the globe. On the basis of modeling of the climate sensitivity of glaciers, the observed glacier retreat can be explained by a linear warming trend of 0.66 kelvin per century. |
| doi_str_mv | 10.1126/science.264.5156.243 |
| format | Article |
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Records of different glaciers are made comparable by a two-step scaling procedure: one allowing for differences in glacier geometry, the other for differences in climate sensitivity. The retreat of glaciers during the last 100 years appears to be coherent over the globe. On the basis of modeling of the climate sensitivity of glaciers, the observed glacier retreat can be explained by a linear warming trend of 0.66 kelvin per century.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.264.5156.243</identifier><identifier>PMID: 17749022</identifier><identifier>CODEN: SCIEAS</identifier><language>eng</language><publisher>United States: American Society for the Advancement of Science</publisher><subject>540110 ; Alpine glaciers ; Climate ; Climate change ; Climate models ; CLIMATIC CHANGE ; Climatic changes ; EARTH PLANET ; ENVIRONMENTAL SCIENCES ; FLUCTUATIONS ; Glacial epoch ; Glacial retreat ; Glacier mass balance ; GLACIERS ; Global climate models ; Global warming ; GREENHOUSE EFFECT ; Ice ages ; Microtubules ; Outlet glaciers ; PLANETS ; Reaction Time ; Scientific Concepts ; Valley glaciers ; VARIATIONS</subject><ispartof>Science (American Association for the Advancement of Science), 1994-04, Vol.264 (5156), p.243-245</ispartof><rights>Copyright 1994 American Association for the Advancement of Science</rights><rights>COPYRIGHT 1994 American Association for the Advancement of Science</rights><rights>COPYRIGHT 1994 American Association for the Advancement of Science</rights><rights>Copyright American Association for the Advancement of Science Apr 8, 1994</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a819t-adccdaff543eb3d003bb12b6c22b34d41f9c94174ccf1e64acbddcaa3d462dbb3</citedby><cites>FETCH-LOGICAL-a819t-adccdaff543eb3d003bb12b6c22b34d41f9c94174ccf1e64acbddcaa3d462dbb3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/2883373$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/2883373$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,780,784,803,885,2884,2885,27924,27925,58017,58250</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/17749022$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://www.osti.gov/biblio/7173364$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Oerlemans, Johannes</creatorcontrib><title>Quantifying Global Warming from the Retreat of Glaciers</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>Records of glacier fluctuations compiled by the World Glacier Monitoring Service can be used to derive an independent estimate of global warming during the last 100 years. Records of different glaciers are made comparable by a two-step scaling procedure: one allowing for differences in glacier geometry, the other for differences in climate sensitivity. The retreat of glaciers during the last 100 years appears to be coherent over the globe. On the basis of modeling of the climate sensitivity of glaciers, the observed glacier retreat can be explained by a linear warming trend of 0.66 kelvin per century.</description><subject>540110</subject><subject>Alpine glaciers</subject><subject>Climate</subject><subject>Climate change</subject><subject>Climate models</subject><subject>CLIMATIC CHANGE</subject><subject>Climatic changes</subject><subject>EARTH PLANET</subject><subject>ENVIRONMENTAL SCIENCES</subject><subject>FLUCTUATIONS</subject><subject>Glacial epoch</subject><subject>Glacial retreat</subject><subject>Glacier mass balance</subject><subject>GLACIERS</subject><subject>Global climate models</subject><subject>Global warming</subject><subject>GREENHOUSE EFFECT</subject><subject>Ice ages</subject><subject>Microtubules</subject><subject>Outlet glaciers</subject><subject>PLANETS</subject><subject>Reaction Time</subject><subject>Scientific Concepts</subject><subject>Valley 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Records of different glaciers are made comparable by a two-step scaling procedure: one allowing for differences in glacier geometry, the other for differences in climate sensitivity. The retreat of glaciers during the last 100 years appears to be coherent over the globe. On the basis of modeling of the climate sensitivity of glaciers, the observed glacier retreat can be explained by a linear warming trend of 0.66 kelvin per century.</abstract><cop>United States</cop><pub>American Society for the Advancement of Science</pub><pmid>17749022</pmid><doi>10.1126/science.264.5156.243</doi><tpages>3</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0036-8075 |
| ispartof | Science (American Association for the Advancement of Science), 1994-04, Vol.264 (5156), p.243-245 |
| issn | 0036-8075 1095-9203 |
| language | eng |
| recordid | cdi_osti_scitechconnect_7173364 |
| source | JSTOR Archive Collection A-Z Listing; American Association for the Advancement of Science |
| subjects | 540110 Alpine glaciers Climate Climate change Climate models CLIMATIC CHANGE Climatic changes EARTH PLANET ENVIRONMENTAL SCIENCES FLUCTUATIONS Glacial epoch Glacial retreat Glacier mass balance GLACIERS Global climate models Global warming GREENHOUSE EFFECT Ice ages Microtubules Outlet glaciers PLANETS Reaction Time Scientific Concepts Valley glaciers VARIATIONS |
| title | Quantifying Global Warming from the Retreat of Glaciers |
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