Geothermal heat may be melting the Greenland glaciers
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“Hansen’s Glacier Model is Wrong! “Hansen is a modeler, and his scenario for the collapse of the ice sheets is based on a false model. His model has the ice sheet sliding along an inclined plane, lubricated by meltwater, which is increasing because of global warming. “Unfortunately, Hansen’s model includes neither the main form of the Greenland and Antarctic Ice Sheets, nor an understanding of how glaciers flow. “Greenland differs from Antarctica in that the ice
sheet spills out through gaps in the mountain rim, and the glaciers
overlie deep narrow valleys. According to van der Veen et al. (2007),
such valleys have higher than usual geothermal gradients, so it might be
geothermal heat, rather than global warming, that causes some Greenland
glaciers to have higher than usual flow rates. (citation below) “In reality, the Greenland and Antarctic ice sheets occupy deep basins, and cannot slide down a plane. Furthermore glacial flow depends on stress (including the important yield stress) as well as temperature, and much of the ice sheets are well below melting point. The accumulation of kilometers of undisturbed ice in cores in Greenland and Antarctica (the same ones that are sometimes used to fuel ideas of global warming) show hundreds of thousands of years of accumulation with no melting or flow. Except around the edges, ice sheets flow at the base and depend on geothermal heat, not the climate at the surface. It is impossible for the Greenland and Antarctic ice sheets to “collapse.” See all of this 7-page paper by geologist Cliff Ollier, School of Earth and Geographical Sciences, The University of Western Australia. Paper was published under the name “Are the Greenland and Antarctic Ice Sheets in Danger of Collapse?” http://ff.org/images/stories/sciencecenter/greenland_and_antarctic_in_danger_of_collapse.pdf http://www.globalwarming.org/files/Melting%20No%20Problem.pdf 1. van der Veen, C.J., Leftwich, T., von Frese, R., Csatho, B.M. & Li, J. (2007), “Subglacial topography and geothermal heat flux: Potential interactions with drainage of the Greenland ice sheet,” Geophysical Research Letters, v.34, LI2501, doi:10.1029/2007 GL030046.)
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