Results 211 to 220 of about 1,196 (236)
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Glaciological Research in the Canadian Arctic
ARCTIC, 1955The "glacierized" highland rim of the Eastern Arctic extends north for 1,600 miles from southern Baffin Island to northernmost Ellesmere. Ice forms include glacier caps, highland, transection, valley, cirque, and piedmont glaciers, and shelf ice on the north coast of Ellesmere. Incidental ice observations prior to, and glaciological work after 1945 are
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1964
When the range of temperatures is close to the freezing point, different methods of determining mean daily temperatures can cause disparities in melting and freezing degree-day totals. On the basis of data collected under such conditions, the disparities are examined and their relevancy to glaciological studies is considered.
K C Arnold, D K MacKay
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When the range of temperatures is close to the freezing point, different methods of determining mean daily temperatures can cause disparities in melting and freezing degree-day totals. On the basis of data collected under such conditions, the disparities are examined and their relevancy to glaciological studies is considered.
K C Arnold, D K MacKay
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In the Arctic, extreme weather conditions such as rain-on-snow events (ROS) make the monitoring of the snowpack with remote sensing techniques increasingly relevant and necessary. In recent years, remote sensing methods based on active radar images (SAR) are well described for mapping the spatial extent of ROS events in the terrestrial Arctic (Vickers,
Jean-Pierre Dedieu +8 more
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Jean-Pierre Dedieu +8 more
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Structural glaciology of Austre Brøggerbreen, northwest Svalbard
Journal of Maps, 2016Stephen J A Jennings +2 more
exaly
Variability of Arctic sea ice thickness and volume from CryoSat-2
Philosophical Transactions Series A, Mathematical, Physical, and Engineering Sciences, 2015R Kwok, G F Cunningham
exaly

