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uk.sci.weather (UK Weather) (uk.sci.weather) For the discussion of daily weather events, chiefly affecting the UK and adjacent parts of Europe, both past and predicted. The discussion is open to all, but contributions on a practical scientific level are encouraged. |
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On 29/01/2017 09:24, JohnD wrote:
"N_Cook" wrote in message news ![]() The lack of Antarctic sea-ice area is before Larsen C breaks off Are you sure that the ice-shelf areas contribute to the overall sea ice figures? My impression was that they didn't - I guess on the basis that are (largely?) grounded ice fed by glaciers rather than floating sea ice. I thought that the 'land' area boundaries of Antarctica on the extent maps actually included the ice shelves. But ICBW and I'm sure someone here must know for sure. I've no knowledge on that, this is just my halfpennyworth. If the ice is over seawater and when it breaks off it forms an ice-berg, then classed as sea-ice I would have thought. Penetrating radar has long since defined the boundary of the land. |
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"N_Cook" wrote in message news
![]() I've no knowledge on that, this is just my halfpennyworth. If the ice is over seawater and when it breaks off it forms an ice-berg, then classed as sea-ice I would have thought. Penetrating radar has long since defined the boundary of the land. ================ Yes, certainly, the true land boundary of the Antarctica is well known. But that's not to say that the ice-shelves are not added to the land boundary for the purpose of the sea ice maps. Take a look for example at the extent of the Ross ice shelf, as per: https://en.wikipedia.org/wiki/Ross_Ice_Shelf Then compare that to the current NSIDC map. The Ross sea ice looks to have very largely gone, yet there's no suggestion AFAIK that the Ross ice shelf is actively melting. So it's presumably still all there, yet not showing up on the NSIDC map. And the introductory notes to sea ice at eg: https://nsidc.org/cryosphere/seaice/index.html make a major distinction between sea ice and land-derived ice, eg: 'Sea ice is simply frozen ocean water. It forms, grows, and melts in the ocean. In contrast, icebergs, glaciers, ice sheets, and ice shelves all originate on land. ' 'The most basic difference is that sea ice forms from salty ocean water, whereas icebergs, glaciers, and lake ice form from fresh water or snow. Sea ice grows, forms, and melts strictly in the ocean. Glaciers are considered land ice, and icebergs are chunks of ice that break off of glaciers and fall into the ocean.' (Though this para doesn't specifically mention ice shelves, AIUI the shelves are made from glacier ice and so aren't sea-ice by definition.) |
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