Imperial College London
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DrPauloCeppi

Faculty of Natural Sciences, Department of Physics

Senior Lecturer in Climate Science
 
 
 
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Contact

 

+44 (0)20 7594 1710p.ceppi Website

 
 
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Location

 

725Huxley BuildingSouth Kensington Campus

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Summary

 

Publications

Citation

BibTex format

@article{Chen:2021:10.1175/jcli-d-20-0949.1,
author = {Chen, Y-J and Hwang, Y-T and Ceppi, P},
doi = {10.1175/jcli-d-20-0949.1},
journal = {Journal of Climate},
pages = {7857--7874},
title = {The impacts of cloud-radiative changes on poleward atmospheric and oceanic energy transport in a warmer climate},
url = {http://dx.doi.org/10.1175/jcli-d-20-0949.1},
volume = {34},
year = {2021}
}
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RIS format (EndNote, RefMan)

TY  - JOUR
AB  - Based on theory and climate model experiments, previous studies suggest most of the uncertainties in projected future changes in meridional energy transport and zonal mean surface temperature can be attributed to cloud feedback. To investigate how radiative and dynamical adjustments modify the influence of cloud-radiative changes on energy transport, this study applies a cloud-locking technique in a fully-coupled climate model, CESM. Under global warming, the impacts of cloud-radiative changes on the meridional energy transport are asymmetric in the two hemispheres. In the Northern Hemisphere, the cloud-radiative changes have little impact on energy transport, because 89% of the cloud-induced heating is balanced locally by increasing outgoing longwave radiation. In the Southern Hemisphere, on the other hand, cloud-induced dynamical changes in the atmosphere and the ocean cause enhanced poleward energy transport, accounting for most of the increase in energy transport under warming. Our experiments highlight that the local longwave radiation adjustment induced by temperature variation can partially offset the impacts of cloud-radiative changes on energy transport, making the estimated impacts smaller than those obtained from directly integrating cloud-radiative changes in previous studies. It is also demonstrated that the cloud-radiative impacts on temperature and energy transport can be significantly modulated by the oceanic circulation, suggesting the necessity of considering atmospheric-oceanic coupling when estimating the impacts of cloud-radiative changes on the climate system.
AU  - Chen,Y-J
AU  - Hwang,Y-T
AU  - Ceppi,P
DO  - 10.1175/jcli-d-20-0949.1
EP  - 7874
PY  - 2021///
SN  - 0894-8755
SP  - 7857
TI  - The impacts of cloud-radiative changes on poleward atmospheric and oceanic energy transport in a warmer climate
T2  - Journal of Climate
UR  - http://dx.doi.org/10.1175/jcli-d-20-0949.1
UR  - https://journals.ametsoc.org/view/journals/clim/aop/JCLI-D-20-0949.1/JCLI-D-20-0949.1.xml
UR  - http://hdl.handle.net/10044/1/90454
VL  - 34
ER  -
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