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May 4, 2014 at 15:32 comment added arkaia The best way to think about that is that you are adding 66m (total sea ice + everything else) to an average depth of 4267m. Assuming an average salinity of 35 from the ocean and 0 for the melting ice (which is not really the case), then the salinity will drop by around 0.5.
May 4, 2014 at 11:39 comment added Semidiurnal Simon @aretxabaleta Interesting. Would the melting of sea ice in itself have any significant effect on global salinity? (AIUI sea ice has somewhat lower salinity than the oceans, but I don't know whether the magnitude of the difference, and the tonnages of water involved, make it matter?)
May 2, 2014 at 20:33 comment added arkaia The maximum density of sea water is not at 4 °C. It depends on the salinity of the water (in most cases larger than 30). At typical salinity, water freezes at about −2 °C. It can be even slightly colder. See Figure 3.1 of Talley et al., 2007 book (booksite.academicpress.com/DPO). Chapter 3 shows up in Google if you do a search for "maximum density seawater".
Apr 30, 2014 at 13:25 history answered Phil Perry CC BY-SA 3.0