{"refrec":{"BRefID":102791,"RR":"<b>Vancoppenolle, M.; Fichefet, T.; Bitz, C.M.</b> (2005). On the sensitivity of undeformed Arctic sea ice to its vertical salinity profile. <i>Geophys. Res. Lett. 32(16)</i>: L16502 (1-4). <a href=\"http://dx.doi.org/10.1029/2005GL023427\" target=\"_blank\">dx.doi.org/10.1029/2005GL023427</a>","BEntID":99580,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geophys. Res. Lett. 32(16)</i>: L16502 (1-4). <a href=\"https://dx.doi.org/10.1029/2005GL023427\" target=\"_blank\">https://dx.doi.org/10.1029/2005GL023427</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vancoppenolle, M.; Fichefet, T.; Bitz, C.M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vancoppenolle, M. <i>et al.</i>","Englishabstract":"The temporal evolution of sea ice salinity affects the temperature profile and vertical growth and decay of the ice cover, as well as many other important properties. Here, we use a one-dimensional thermodynamic sea ice model to explore the sensitivity to the vertical profile of ice salinity of (1) Arctic first-year and equilibrium multiyear sea ice thickness, and (2) the salt/freshwater flux at the ice/ocean interface. Results indicate that increasing the mean salinity induces a higher thermal inertia reducing summer melt and finally increasing ice thickness. 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