Hydrological Cycle Changes Explain Weak Snowball Earth Storm Track Despite Increased Surface Baroclinicity
Author:
Affiliation:
1. Department of the Geophysical Sciences The University of Chicago Chicago IL USA
2. Department of Physics The University of Oxford Oxford UK
Funder
Office of the Director
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL089866
Reference40 articles.
1. Using the Moist Static Energy Budget to Understand Storm-Track Shifts across a Range of Time Scales
2. Surface Fluxes Modulate the Seasonality of Zonal-Mean Storm Tracks
3. Thermodynamic Scaling of the Hydrological Cycle of the Last Glacial Maximum
4. Monsoons as eddy-mediated regime transitions of the tropical overturning circulation
5. The dynamic range of poleward energy transport in an atmospheric general circulation model
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