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DZT ELA is the difference in elevation between the equilibrium line altitude and an ef-
fective or weighted average altitude where retreat of the terminus takes place. Large glaciers
tend to extend to lower elevations with respect to the ELA, that is have a larger DZT ELA, which
leads to a shorter tV according to this equation, but they also tend to be thicker, which leads to
a longer tV
/media/ces/ces-glacier-scaling-memo2009-01.pdf