The great ice sheets of Greenland and Antarctica, which rise to over 13,000 feet above sea level, accumulate ice over most of their surfaces and melt
only at their lower elevations near the edges.
Not exact matches
Do regional sets of tree ring data exist which contain not
only trees close to the alpine tree line but also
at lower elevations?
Not
only did Greenland Ice Sheet surface melt in 2012 occur over a bigger - than - average area, it also began about two weeks earlier
at lower elevations and, for any given
elevation, lasted longer.
Of course, this may
only happen mostly on the 30 % land surfaces, predominantly
at lower elevations, I would think — not on water covered surfaces where the heat capacity of water would limit the cooling or heating of the crust, although any part of the affected plate that is land bound would still lever the whole plate to or fro.