Imperial College London
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ProfessorApostolosVoulgarakis

Faculty of Natural Sciences, Department of Physics

Professor in Global Climate and Environmental Change
 
 
 
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Contact

 

a.voulgarakis Website

 
 
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Location

 

Huxley 709BHuxley BuildingSouth Kensington Campus

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Summary

 

Publications

Citation

BibTex format

@article{Teixeira:2021:10.5194/gmd-14-6515-2021,
author = {Teixeira, JC and Folberth, GA and O'Connor, FM and Unger, N and Voulgarakis, A},
doi = {10.5194/gmd-14-6515-2021},
journal = {Geoscientific Model Development},
pages = {6515--6539},
title = {Coupling interactive fire with atmospheric composition and climate in the UK Earth System Model},
url = {http://dx.doi.org/10.5194/gmd-14-6515-2021},
volume = {14},
year = {2021}
}
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RIS format (EndNote, RefMan)

TY  - JOUR
AB  - Fire constitutes a key process in the Earth system (ES), being driven by climate as well as affecting the climate by changing atmospheric composition and impacting the terrestrial carbon cycle. However, studies on the effects of fires on atmospheric composition, radiative forcing and climate have been limited to date, as the current generation of ES models (ESMs) does not include fully atmosphere–composition–vegetation coupled fires feedbacks. The aim of this work is to develop and evaluate a fully coupled fire–composition–climate ES model. For this, the INteractive Fires and Emissions algoRithm for Natural envirOnments (INFERNO) fire model is coupled to the atmosphere-only configuration of the UK's Earth System Model (UKESM1). This fire–atmosphere interaction through atmospheric chemistry and aerosols allows for fire emissions to influence radiation, clouds and generally weather, which can consequently influence the meteorological drivers of fire. Additionally, INFERNO is updated based on recent developments in the literature to improve the representation of human and/or economic factors in the anthropogenic ignition and suppression of fire. This work presents an assessment of the effects of interactive fire coupling on atmospheric composition and climate compared to the standard UKESM1 configuration that uses prescribed fire emissions. Results show a similar performance when using the fire–atmosphere coupling (the “online” version of the model) when compared to the offline UKESM1 that uses prescribed fire. The model can reproduce observed present-day global fire emissions of carbon monoxide (CO) and aerosols, despite underestimating the global average burnt area. However, at a regional scale, there is an overestimation of fire emissions over Africa due to the misrepresentation of the underlying vegetation types and an underestimation over equatorial Asia due to a lack of representation of peat fires. Despite this, co
AU  - Teixeira,JC
AU  - Folberth,GA
AU  - O'Connor,FM
AU  - Unger,N
AU  - Voulgarakis,A
DO  - 10.5194/gmd-14-6515-2021
EP  - 6539
PY  - 2021///
SN  - 1991-959X
SP  - 6515
TI  - Coupling interactive fire with atmospheric composition and climate in the UK Earth System Model
T2  - Geoscientific Model Development
UR  - http://dx.doi.org/10.5194/gmd-14-6515-2021
UR  - http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000712043200001&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=1ba7043ffcc86c417c072aa74d649202
UR  - https://gmd.copernicus.org/articles/14/6515/2021/
UR  - http://hdl.handle.net/10044/1/96462
VL  - 14
ER  -
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