MODELING THE RESPONSE OF GLACIERS TO CLIMATE WARMING

Dynamic ice-flow models for 12 glaciers and ice caps have been forced with various climate change scenarios. The volume of this sample spans three orders of magnitude. Six climate scenarios were considered: fro m 1990 onwards linear warming rates of 0.01, 0.02 and 0.04 K a(-1), wi th and without concurrent changes in precipitation. The models, calibr ated against the historic record of glacier length where possible, wer e integrated until 2100. The differences in individual glacier respons es are very large. No straightforward relationship between glacier siz e and fractional change of ice volume emerges for any given climate sc enario. The hypsometry of individual glaciers and ice caps plays an im portant role in their response, thus making it difficult to generalize results. For a warming rate of 0.04 K a(-1), without increase in prec ipitation, results indicate that few glaciers would survive until 2100 . On the other hand, if the warming rate were to be limited to 0.01 K a(-1) with an increase in precipitation of 10% per degree a warming, w e predict that overall loss would be restricted to 10 to 20% of the 19 90 volume.