Hydrological cycle changes explain weak snowball earth storm track despite increased surface baroclinicity
Simulations show that storm tracks were weaker during past cold, icy climates relative to the modern climate despite increased surface baroclinicity. Previous work explained the weak North Atlantic storm track during the Last Glacial Maximum using dry zonally asymmetric mechanisms associated with or...
| Príomhchruthaitheoirí: | , |
|---|---|
| Formáid: | Journal article |
| Teanga: | English |
| Foilsithe / Cruthaithe: |
Wiley
2020
|