English
 
Help Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT
Add to Basket
  Local TagsRelease HistoryDetailsSummary

Released
Journal Article

Sensitivity of tropical extreme precipitation to surface warming in aquaplanet experiments using a global nonhydrostatic model

MPS-Authors

Uribe,  A.
The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society;

/persons/resource/persons242110

Vial,  Jessica
Director’s Research Group AES, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society;

/persons/resource/persons37260

Mauritsen,  Thorsten
The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society;

External Resource
No external resources are shared
Fulltext (restricted access)
There are currently no full texts shared for your IP range.
Fulltext (public)

2020GL091371.pdf
(Publisher version), 307KB

Supplementary Material (public)
There is no public supplementary material available
Citation

Uribe, A., Vial, J., & Mauritsen, T. (2021). Sensitivity of tropical extreme precipitation to surface warming in aquaplanet experiments using a global nonhydrostatic model. Geophysical Research Letters, 48: e2020GL091371. doi:10.1029/2020GL091371.


Cite as: https://hdl.handle.net/21.11116/0000-0008-991D-C
Abstract
Increases of atmospheric water vapor holding capacity with temperature (7 K−1–8 K−1, CC-rate) can lead to increasing extreme precipitation (EP). Observations show that tropical EP has increased during the last five decades with a rate higher than in the extratropics. Global climate models (GCM's) diverge in the magnitude of increase in the tropics, and cloud-resolving models (CRM's) indicate correlations between changes in tropical EP and organization of deep convection. We conducted global-scale aquaplanet experiments at a wide range of resolutions with explicit and parameterized convection to bridge the gap between GCM's and CRM's. We found increases of tropical EP beyond the CC rate, with similar magnitudes when using explicit convection and parametrized convection at the resolution it is tuned for. Those super-CC rates are produced due to strengthening updrafts where extreme precipitation occurs, and they do not exhibit relations with changes in convective organization. © 2021. The Authors.