Spatiotemporal patterns of rain-on-snow and basal ice in high Arctic Svalbard: detection of a climate-cryosphere regime shift
Arctic winters have become increasingly warmer and rainier. Where permafrost prevails, winter rain (or rain-on-snow) is known to occasionally cause extensive ice layers at the snow/ground interface, i.e. ‘basal ice’ or ‘ground ice’, with potentially large ecological and socio-economic implications....
محفوظ في:
| المؤلفون الرئيسيون: | , , , , , , , , , |
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| التنسيق: | Artigo |
| اللغة: | Inglês |
| منشور في: |
IOP Publishing
2019-01-01
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| سلاسل: | Environmental Research Letters |
| الموضوعات: | |
| الوصول للمادة أونلاين: | https://doi.org/10.1088/1748-9326/aaefb3 |
| الوسوم: |
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