{"refrec":{"BRefID":211450,"RR":"<b>Renssen, H.; Beets, C.J.; Fichefet, T.; Goosse, H.; Kroon, D.</b> (2004). Modeling the climate response to a massive methane release from gas hydrates. <i>Paleoceanography 19(2)</i>. <a href=\"http://dx.doi.org/10.1029/2003PA000968\" target=\"_blank\">dx.doi.org/10.1029/2003PA000968</a>","BEntID":203372,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Paleoceanography 19(2)</i>. <a href=\"https://dx.doi.org/10.1029/2003PA000968\" target=\"_blank\">https://dx.doi.org/10.1029/2003PA000968</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Renssen, H.; Beets, C.J.; Fichefet, T.; Goosse, H.; Kroon, D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Renssen, H. <i>et al.</i>","Englishabstract":"[1] The climate response to a massive release of methane from gas hydrates is simulated in two 2500-year-long numerical experiments performed with a three-dimensional, global coupled atmosphere-sea ice-ocean model of intermediate complexity. Two different equilibrium states were used as reference climates; the first state with preindustrial forcing conditions and the second state with a four times higher atmospheric CO<sub>2</sub> concentration. These climates were perturbed by prescribing a methane emission scenario equivalent to that computed for the Paleocene/Eocene thermal maximum (PETM; similar to 55.5 Ma), involving a sudden release of 1500 Gt of carbon into the atmosphere in 1000 years. In both cases, this produced rapid atmospheric warming (up to 10°C at high latitudes) and a reorganization of the global overturning ocean circulation. In the ocean, maximum warming (2-4°C) occurred at intermediate depths where methane hydrates are stored in the upper slope sediments, suggesting that further hydrate instability could result from the prescribed scenario.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Modeling the climate response to a massive methane release from gas hydrates","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"methane; climate model","OtherDescriptors":null,"Notes":null,"AnaPub":2004,"MonPub":null,"DateUpdate":"2012-01-30","DateCreate":"2011-12-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000221326500002","VABBcode":null,"OpenAcc":0,"DOI":"10.1029/2003PA000968"},"refs":null,"anarec":{"AnaID":211450,"PubliDate":2004,"Pagination":null,"XtraPublOfAnaID":null,"ISBN":null,"Volume":"19","Issue":"2","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45633,"SerRR":"Paleoceanography. 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