An email from Hartwig Volz [Hartwig.Volz@rwe.com] below referring to this article
Dear Mr. Ollier,
With reference to your recent contribution, THE GREENLAND-ANTARCTICA MELTING PROBLEM DOES NOT EXIST, you may be interested in my correponence with James Hansen some years ago.
best regards
Hartwig Volz
From: Volz, Dr. Hartwig
Sent: Thursday, March 18, 2004 5:16 PM
To: 'James Hansen'
Subject: Slippery Slope
Dear Dr. Hansen,
Thank you for sending me your submitted climate change editorial. Your publications are always interesting reading, though I do not always agree.
One remark: many years ago I did a lot of "adventure travelling", also mountain and ice climbing in Greenland. From this time I vaguely remember the following: the sub-ice geomorphology of Greenland is kind of shaped like a saucer. This is the reason why most of the Greenland glacier can not escape by glacier surge, because of the natural sediment and lava barrier. The same is true for Vatnajokull in Iceland, the third largest glacier in the world. So this situation is different from e.g. the situation of the North American ice shield at the end of the last glacial. The top of the Greenland glacier is far too high and too cold to melt. More details you may find by googling e.g. "Greenland sub-ice geomorphology" or asking an expert directly.
best regards
Hartwig Volz
Celle, Germany
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