Glacier Terminus Morphology Informs Calving Style
Abstract Terminus change is a complex outcome of ice‐ocean boundary processes and poses challenges for ice sheet models due to inadequate calving laws, creating uncertainty in sea level change projections. To address this, we quantify glacier termini sinuosity and convexity, testing the hypothesis t...
| Published in: | Geophysical Research Letters |
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| Main Authors: | , |
| Format: | Article |
| Language: | English |
| Published: |
Wiley
2024-08-01
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| Subjects: | |
| Online Access: | https://doi.org/10.1029/2024GL108530 |