Ice Sheet Melt Pond at Kristy Mulkey blog

Ice Sheet Melt Pond. We apply the technique to sequences of satellite imagery acquired over the western margin of the greenland ice sheet to derive changes in melt pond extent. Dangers to ancient antarctic ice portend a future of rapidly rising seas, but a new study may relieve one nagging fear: In greenland, melt ponds ultimately find their way into crevasses or moulins —chutes that carry melt water through the ice sheet. Stanford researchers have developed open radar code. This extraordinary event was preceded by a heatwave and followed by the surface snow and ice rapidly melting. Surface melt ponds form intermittently on several antarctic ice shelves. Many glaciologists suspect that the melt water.

ESA Earth from Space Melt ponds in West Greenland
from www.esa.int

We apply the technique to sequences of satellite imagery acquired over the western margin of the greenland ice sheet to derive changes in melt pond extent. Dangers to ancient antarctic ice portend a future of rapidly rising seas, but a new study may relieve one nagging fear: Surface melt ponds form intermittently on several antarctic ice shelves. Many glaciologists suspect that the melt water. Stanford researchers have developed open radar code. This extraordinary event was preceded by a heatwave and followed by the surface snow and ice rapidly melting. In greenland, melt ponds ultimately find their way into crevasses or moulins —chutes that carry melt water through the ice sheet.

ESA Earth from Space Melt ponds in West Greenland

Ice Sheet Melt Pond Stanford researchers have developed open radar code. In greenland, melt ponds ultimately find their way into crevasses or moulins —chutes that carry melt water through the ice sheet. Many glaciologists suspect that the melt water. Stanford researchers have developed open radar code. Dangers to ancient antarctic ice portend a future of rapidly rising seas, but a new study may relieve one nagging fear: We apply the technique to sequences of satellite imagery acquired over the western margin of the greenland ice sheet to derive changes in melt pond extent. This extraordinary event was preceded by a heatwave and followed by the surface snow and ice rapidly melting. Surface melt ponds form intermittently on several antarctic ice shelves.

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