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...
Main Authors: | Shaw, TA, Graham, RJ |
---|---|
Format: | Journal article |
Language: | English |
Published: |
Wiley
2020
|
Similar Items
-
The Snowball Stratosphere
by: Graham, RJ, et al.
Published: (2019) -
The Snowball Earth Episodes
by: Angelos Siozos, et al.
Published: (2023-08-01) -
Future changes in extratropical storm tracks and baroclinicity under climate change
by: Jascha Lehmann, et al.
Published: (2014-01-01) -
Storm tracks, baroclinic waves propagation and their interannual variability in the northern hemisphere
by: Chen, Yijian
Published: (2010) -
Simple Stochastic Modeling of Snowball Probability Throughout Earth History
by: Mark Baum, et al.
Published: (2022-11-01)