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No general stability conditions for marine ice-sheet grounding lines in the presence of feedbacks
The “marine ice-sheet instability” hypothesis continues to be used to interpret the observed mass loss from the Antarctic and Greenland ice sheets. This hypothesis has been developed for conditions that do not account for feedbacks between ice sheets and environmental conditions. However, snow accum...
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2022
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9046188/ https://www.ncbi.nlm.nih.gov/pubmed/35477962 http://dx.doi.org/10.1038/s41467-022-29892-3 |