Cloud radiative effects significantly increase wintertime atmospheric blocking in the Euro-Atlantic sector. [PDF]
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North Atlantic Subtropical High forcing of Atlantic Warm Pool hydroclimate variability on millennial to orbital timescales. [PDF]
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Monthly-Resolved Cave Proxy Evidence for Northward Gulf Stream Migration During the Little Ice Age
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Back to the Seabed: The Unique Photosystem I Architecture of the Seagrass Posidonia oceanica
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Concentration gradients and growth/decay characteristics of the seasonal sea ice cover
Journal of Geophysical Research: Oceans, 1984The growth and decay characteristics of sea ice in the northern and southern hemispheres are presented quantitatively by using brightness temperature data from the Nimbus 5 Electrically Scanning Microwave Radiometer. The areal extent of >15% ice cover follows a basically symmetrical seasonal cycle in the northern hemisphere, ranging from 8×106 km2 ...
J. C. Comiso, H. J. Zwally
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The Barents Sea Ice Sheet — A model of its growth and decay during the last ice maximum
Quaternary Science Reviews, 1993On the basis of geomorphological and sedimentological data, we believe that the entire Barents Sea was covered by grounded ice during the last glacial maximum. 14C dates on shells embedded in tills suggest marine conditions in the Barents Sea as late as 22 ka BP; and models of the deglaciation history based on uplift data from the northern Norwegian ...
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The paleoceanography in the Nordic seas was characterized by apparently repeated switching on and off of Atlantic water advection. In contrast, a continous influx of Atlantic waters probably occurred along the northern Barents Sea margin during the last 150 ka.
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