{"refrec":{"BRefID":107132,"RR":"<b>Rahmstorf, S.</b> (2007). A semi-empirical approach to projecting future sea-level rise. <i>Science (Wash.) 315(5810)</i>: 368-370. <a href=\"https://dx.doi.org/10.1126/science.1135456\" target=\"_blank\">https://dx.doi.org/10.1126/science.1135456</a>","BEntID":101432,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 315(5810)</i>: 368-370. <a href=\"https://dx.doi.org/10.1126/science.1135456\" target=\"_blank\">https://dx.doi.org/10.1126/science.1135456</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Rahmstorf, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Rahmstorf, S.","Englishabstract":"A semi-empirical relation is presented that connects global sea-level rise to global mean surface temperature. It is proposed that, for time scales relevant to anthropogenic warming, the rate of sea-level rise is roughly proportional to the magnitude of warming above the temperatures of the pre–Industrial Age. This holds to good approximation for temperature and sea-level changes during the 20th century, with a proportionality constant of 3.4 millimeters/year per °C. 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