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North Atlantic storm track changes during the Last Glacial Maximum recorded by Alpine speleothems
The European Alps are an effective barrier for meridional moisture transport and are thus uniquely placed to record shifts in the North Atlantic storm track pattern associated with the waxing and waning of Late-Pleistocene Northern Hemisphere ice sheets. The lack of well-dated terrestrial proxy reco...
Uloženo v:
| Vydáno v: | Nat Commun |
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| Hlavní autoři: | , , , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Pub. Group
2015
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4351561/ https://ncbi.nlm.nih.gov/pubmed/25724008 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms7344 |
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