{"refrec":{"BRefID":352716,"RR":"<b>Slangen, A.B.A.; Haasnoot, M.; Winter, G.</b> (2022). Rethinking sea‐level projections using families and timing differences. <i>Earth's Future 10(4)</i>: e2021EF002576. <a href=\"https://dx.doi.org/10.1029/2021ef002576\" target=\"_blank\">https://dx.doi.org/10.1029/2021ef002576</a>","BEntID":350424,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Earth's Future 10(4)</i>: e2021EF002576. <a href=\"https://dx.doi.org/10.1029/2021ef002576\" target=\"_blank\">https://dx.doi.org/10.1029/2021ef002576</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Slangen, A.B.A.; Haasnoot, M.; Winter, G.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Slangen, A.B.A.; Haasnoot, M.; Winter, G.","Englishabstract":"<p>    In the recent decade, many global and regional sea-level rise (SLR)    projections have been published, which raises questions for users. Here, we    present a series of strategies to help users to see the forest for the    trees, by reducing the number of choices to be made. First, we use the    similarities in the methodologies and contributing sources of the    projections to group 82 projections from 29 publications into only 8    families. Second, we focus on the timing of reaching several global mean    SLR thresholds, and the uncertainty therein, rather than the projected    value in the year 2100. Finally, we combine the information on timing and    families to define three categories which can support decision making. For    global mean SLR up to 0.50 m the differences in timing are small,    regardless of climate scenario or family, clearly indicating a timing    window for adaptation decisions. For larger global mean SLR (0.75–1.00 m),    the climate scenario becomes more important for the uncertainties in    timing, but the SLR threshold will be crossed within a limited window of    time, supporting adaptation decision making on the medium to long term.    Beyond 1.00 m the differences between the families and climate scenario    strongly determine the uncertainties in timing, and more information is    needed, for instance using early warning signals, before decisions for    adaptation can be made. We make recommendations on how each of these three    categories, combined with the lead time and lifespan of adaptation options,    can inform decisions on adaptation strategies using adaptation pathways    planning.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Rethinking sea‐level projections using families and timing differences","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":2022,"MonPub":null,"DateUpdate":"2023-02-01","DateCreate":"2022-06-20","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000786352600001","VABBcode":null,"OpenAcc":1,"DOI":"10.1029/2021ef002576"},"refs":null,"anarec":{"AnaID":352716,"PubliDate":2022,"Pagination":"e2021EF002576","XtraPublOfAnaID":null,"ISBN":null,"Volume":"10","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":238930,"SerRR":"Earth's Future. 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