{"refrec":{"BRefID":213169,"RR":"<b>Jacob, T.; Wahr, J.; Pfeffer, W.T.; Swenson, S.</b> (2012). Recent contributions of glaciers and ice caps to sea level rise. <i>Nature (Lond.) 482(7386)</i>: 514-518. <a href=\"https://dx.doi.org/10.1038/nature10847\" target=\"_blank\">https://dx.doi.org/10.1038/nature10847</a>","BEntID":205066,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature (Lond.) 482(7386)</i>: 514-518. <a href=\"https://dx.doi.org/10.1038/nature10847\" target=\"_blank\">https://dx.doi.org/10.1038/nature10847</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Jacob, T.; Wahr, J.; Pfeffer, W.T.; Swenson, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Jacob, T. <i>et al.</i>","Englishabstract":"Glaciers and ice caps (GICs) are important contributors to present-day global mean sea level rise(1-4). Most previous global mass balance estimates for GICs rely on extrapolation of sparse mass balance measurements(1,2,4) representing only a small fraction of the GIC area, leaving their overall contribution to sea level rise unclear. Here we show that GICs, excluding the Greenland and Antarctic peripheral GICs, lost mass at a rate of 148 +/- 30 Gt yr(-1) from January 2003 to December 2010, contributing 0.41 +/- 0.08 mm yr(-1) to sea level rise. Our results are based on a global, simultaneous inversion of monthly GRACE-derived satellite gravity fields, from which we calculate the mass change over all ice-covered regions greater in area than 100 km(2). The GIC rate for 2003-2010 is about 30 per cent smaller than the previous mass balance estimate that most closely matches our study period(2). The high mountains of Asia, in particular, show a mass loss of only 4 +/- 20 Gt yr(-1) for 2003-2010, compared with 47-55 Gt yr(-1) in previously published estimates(2,5). For completeness, we also estimate that the Greenland and Antarctic ice sheets, including their peripheral GICs, contributed 1.06 +/- 0.19 mm yr(-1) to sea level rise over the same time period. The total contribution to sea level rise from all ice-covered regions is thus 1.48 +/- 0.26 mm yr(-1), which agrees well with independent estimates of sea level rise originating from land ice loss and other terrestrial sources(6).","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Recent contributions of glaciers and ice caps to sea level rise","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-05-15 01:32:16.786603","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2012,"MonPub":null,"DateUpdate":"2018-02-13","DateCreate":"2012-03-01","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000300770500048","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/nature10847"},"refs":null,"anarec":{"AnaID":213169,"PubliDate":2012,"Pagination":"514-518","XtraPublOfAnaID":null,"ISBN":null,"Volume":"482","Issue":"7386","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43431,"SerRR":"Nature: International Weekly Journal of Science. 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