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in quite a different manner to a relatively small difference in weather conditions. The cause is obviously the difference in their inclinations. This raises the further question of how climatic changes influence glaciers and also in what manner climatic fluctuations and changes can b e known or calculated from the behaviour of glaciers. The problems involved by such questions could well be the subject for the n ext symposium for the Commission on Snow and Ice, which is to be held between thedoi:10.3189/s0022143000017329 fatcat:ah56fcy6dzdqffrx4vjjm5xfyy