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![Figure 13.—Trend in seasonal [A, summer; B, winter] and [C] cumulative mass balances for about 300 mountain and subpolar glaciers, not including the Greenland
and Antarctica ice sheets. Figure based on Dyurgerov (2003).](images/gallery-1/large/pp1386a1-fig13.jpg)
Figure 13. Trend in seasonal [A, summer; B, winter] and [C] cumulative mass balances for about 300 mountain and subpolar glaciers, not including the Greenland and Antarctica ice sheets. Figure based on Dyurgerov (2003). |