To start with no one is entirely sure how warm the Medieval Warm period was, and definitely what the temperatures of Greenland were. It does seem clear though that Greenland was warmer and a number of climate reconstructions do have varying amount of warming, some little other more from that time period. The regional nature of the climate change of this period and type of proxy likely contribute to those model differences. See my post below for agriculture on Greenland and links for "Medieval Warm period"
As for the Icesheets, a major study was conducted by Ola M. Johannessen, Kirill Khvorostovsky, Martin W. Miles, Leonid P. Bobylev 2, 2005, titled "Recent Ice-Sheet Growth in the Interior of Greenland". To view the abstract.
http://www.sciencemag.org/cgi/content/abstract/1115356v1
Also a good summary from where my quotes are taken from
http://www.sciencedaily.com/releases/2005/11/051107080830.htm
In any regard, ill sum up the import part of this research, by taking a variety of their statements
"The result is a mixed picture, with a net increase of 6.4 centimetres per year in the interior area above 1500 metres elevation. Below that altitude, the elevation-change rate is minus 2.0 cm per year, broadly matching reported thinning in the ice-sheet margins. The trend below 1500 metres however does not include the steeply-sloping marginal areas where current altimeter data are unusable."
"The spatially averaged increase is 5.4 cm per year over the study area, when corrected for post-Ice Age uplift of the bedrock beneath the ice sheet. These results are remarkable because they are in contrast to previous scientific findings of balance in Greenland's high-elevation ice."
This means the icesheet is growing in +1500m elevation in the central portions while the edges or margins are shrinking. Furthermore, the reasons given for these changes include
"interior growth of the Greenland Ice Sheet to increased snowfall linked to variability in regional atmospheric circulation known as the North Atlantic Oscillation (NAO). First discovered in the 1920s, the NAO acts in a similar way to the El Niño phenomenon in the Pacific, contributing to climate fluctuations across the North Atlantic and Europe."
"Modelling studies of the Greenland Ice Sheet mass balance under greenhouse global warming have shown that temperature increases up to about 3ºC lead to positive mass balance changes at high elevations – due to snow accumulation – and negative at low elevations – due to snow melt exceeding accumulation."
In orderwords the ice isnt getting thicker because the climate in greenland is cooling but the warming is affecting weather patterns such that greater amounts of snow are accumulating in the higher elevations, while in the lower elevations are melting due to the increased warming.









Recorded History