Abstract
A parameterization of monthly mean ice sheet ablation as a function only of surface air temperature and insolation is examined. By considering differences in summer climate between the present and the last ice age, it is suggested that the parameterization adequately describes long-term changes in ablation. -from Author
Original language | English (US) |
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Pages (from-to) | 384-388 |
Number of pages | 5 |
Journal | Tellus |
Volume | 32 |
Issue number | 4 |
DOIs | |
State | Published - 1980 |
All Science Journal Classification (ASJC) codes
- General Medicine