Abstract
Glacier volume is known for less than 0.1% of the world's glaciers, but this information is needed to quantify the impacts of glacier changes on global sea level and regional water resources. Observations indicate a power-law relation between glacier area and volume, with an exponent 1.36. Through numerical simulations of 3D, high-order glacier mechanics, we demonstrate how different topographic and climatic settings, glacier flow dynamics, and the degree of disequilibrium with climate systematically affect the volume-area relation. We recommend more accurate scaling relations through characterization of individual glacier shape, slope and size. An ensemble of 280 randomly-generated valley glaciers spanning a spectrum of plausible glaciological conditions yields a steady-state exponent = 1.46. This declines to 1.38 for glaciers that are 100years into a sustained retreat, which corresponds exceptionally well with the observed value for present-day glaciers. © 2012. American Geophysical Union. All Rights Reserved.
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CITATION STYLE
Adhikari, S., & Marshall, S. J. (2012). Glacier volume-area relation for high-order mechanics and transient glacier states. Geophysical Research Letters, 39(16). https://doi.org/10.1029/2012GL052712
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