Seasonally stable temperature gradients through supraglacial debris in the Everest region of Nepal, Central Himalaya
Rock debris covers ~30% of glacier ablation areas in the Central Himalaya and modifies the impact of atmospheric conditions on mass balance. The thermal properties of supraglacial debris are diurnally variable but remain poorly constrained for monsoon-influenced glaciers over the timescale of the ab...
| Päätekijät: | , , , , , , , , , , |
|---|---|
| Aineistotyyppi: | Artikkeli |
| Kieli: | English |
| Julkaistu: |
Cambridge University Press
2021-02-01
|
| Sarja: | Journal of Glaciology |
| Linkit: | https://www.cambridge.org/core/product/identifier/S0022143020001008/type/journal_article |