{"refrec":{"BRefID":211090,"RR":"<b>Massom, R.A.; Stammerjohn, S.E.; Lefebvre, W.; Harangozo, S.A.; Adams, N.; Scambos, T.A.; Pook, M.J.; Fowler, C.</b> (2008). West Antarctic Peninsula sea ice in 2005: Extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate. <i>J. Geophys. Res. 113(C2)</i>. <a href=\"http://dx.doi.org/10.1029/2007JC004239\" target=\"_blank\">dx.doi.org/10.1029/2007JC004239</a>","BEntID":203012,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Geophys. Res. 113(C2)</i>. <a href=\"https://dx.doi.org/10.1029/2007JC004239\" target=\"_blank\">https://dx.doi.org/10.1029/2007JC004239</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Massom, R.A.; Stammerjohn, S.E.; Lefebvre, W.; Harangozo, S.A.; Adams, N.; Scambos, T.A.; Pook, M.J.; Fowler, C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Massom, R.A. <i>et al.</i>","Englishabstract":"In September-October 2005, the juxtaposition of low-and high-pressure anomalies at 130°W and 60°W, respectively, created strong and persistent northerly airflow across the West Antarctic Peninsula (WAP). This had a major impact on regional sea ice conditions, with extreme ice compaction in the Bellingshausen and East Amundsen seas (60°W-130°W) but divergence in the West Amundsen and East Ross seas. This resulted in the former in a highly compact marginal ice zone and ice cover, mean modeled ice thicknesses of >5 m, and an earlier-than-average maximum extent (mid-August). While rapid ice retreat in late winter-spring created a major negative ice extent anomaly, compact ice persisted in the subsequent summer. Other effects were anomalies in air temperature (of +1°C to +5°C) and precipitation rates (to >2.5 mm/d). The patterns in late 2005 are consistent with the occurrence of a weak La Nina and a near-neutral Southern Annular Mode, with a quasi-stationary zonal wave three pattern dominating hemispheric atmospheric circulation. Once a compact ice edge was created, it took only one additional week of strong winds to \"solidify'' the pack in place. Conditions in 2005 are analyzed in the context of 1979-2005 and compared with the springs of 1993, 1997, 1999, 2001, and 2004. A statistically significant increase of the northerly 10-m wind component between 110°W and 125°W occurred in the Septembers of 1979-2005. No clear trends occur in other spring months. This work underlines the key importance of ice dynamics in recent changes in the WAP sea ice regime.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"West Antarctic Peninsula sea ice in 2005: Extreme ice compaction and ice edge retreat due to strong anomaly with respect to climate","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":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2008,"MonPub":null,"DateUpdate":"2012-01-20","DateCreate":"2011-12-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000253532200002","VABBcode":null,"OpenAcc":0,"DOI":"10.1029/2007JC004239"},"refs":null,"anarec":{"AnaID":211090,"PubliDate":2008,"Pagination":null,"XtraPublOfAnaID":null,"ISBN":null,"Volume":"113","Issue":"C2","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":90908,"SerRR":"Journal of Geophysical Research. 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