{"refrec":{"BRefID":23581,"RR":"<b>Goosse, H.; Campin, J.M.; Fichefet, T.; Deleersnijder, E.</b> (1997). Impact of sea-ice formation on the properties of Antarctic bottom water. <i>Ann. Glaciol. 25</i>: 276-281","BEntID":23581,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Ann. Glaciol. 25</i>: 276-281","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Goosse, H.; Campin, J.M.; Fichefet, T.; Deleersnijder, E.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Goosse, H. <i>et al.</i>","Englishabstract":"It is generally accepted that fresh-water fluxes due to ice accretion or melting profoundly influence the formation of Antarctic bottom water (AABW). This is investigated by means of a global, three-dimensional ice-ocean model. Two model runs were conducted. At the high southern latitudes, the control experiment exhibits positive (i.e. towards the ocean) fresh-water fluxes over the deep ocean, and large negative fluxes over the Antarctic continental shelf, because of the intense ice-production taking place in this region. The salinity of shelf water can increase in such a way that deep-water formation is facilitated. The simulated net fresh-water flux over the shelf has an annual mean value of -1 m a<sup>-1</sup>. This flux induces a transport of salt to bottom waters, which corresponds to an increase of their salinity estimated to be around 0.05 psu. In the second model run, the fresh-water fluxes due to ice melting or freezing are neglected, leading to a rearrangement of the water masses. In particular, the AABW-formation rate decreases, which allows the influence of North Atlantic deep water (NADW) to increase. 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