Journal article icon

Journal article

Risks of seasonal extreme rainfall events in Bangladesh under 1.5 and 2.0 degrees’ warmer worlds – how anthropogenic aerosols change the story

Abstract:
Anthropogenic climate change is likely to increase the frequency of extreme weather events in future. Previous studies have robustly shown how and where climate change has already changed the risks of weather extremes. However, developing countries have been somewhat underrepresented in these studies, despite high vulnerability and limited capacities to adapt. How additional global warming would affect the future risks of extreme rainfall events in Bangladesh needs to be addressed to limit adverse impacts. Our study focuses on understanding and quantifying the relative risks of seasonal extreme rainfall events in Bangladesh under the Paris Agreement temperature goals of 1.5 °C and 2 °C warming above pre-industrial levels. In particular, we investigate the influence of anthropogenic aerosols on these risks given their likely future reduction and resulting amplification of global warming. Using large ensemble regional climate model simulations from weather@home under different forcing scenarios, we compare the risks of rainfall events under pre-industrial (natural), current (actual), 1.5 °C, and 2.0 °C warmer and greenhouse gas only (anthropogenic aerosols removed) conditions. We find that the risk of a 1 in 100 year rainfall event has already increased significantly compared with pre-industrial levels across parts of Bangladesh, with additional increases likely for 1.5 and 2.0 degree warming (of up to 5.5 times higher, with an uncertainty range of 3.5 to 7.8 times). Impacts were observed during both the pre-monsoon and monsoon periods, but were spatially variable across the country in terms of the level of impact. Results also show that reduction in anthropogenic aerosols plays an important role in determining the overall future climate change impacts; by exacerbating the effects of GHG induced global warming and thereby increasing the rainfall intensity. We highlight that the net aerosol effect varies from region to region within Bangladesh, which leads to different outcomes of aerosol reduction on extreme rainfall statistics, and must therefore be considered in future risk assessments. Whilst there is a substantial reduction in the impacts resulting from 1.5 °C compared with 2 °C warming, the difference is spatially and temporally variable, specifically with respect to seasonal extreme rainfall events.
Publication status:
Published
Peer review status:
Not peer reviewed

Actions


Access Document


Files:
Publisher copy:
10.5194/hess-2018-400

Authors


More by this author
Institution:
University of Oxford
Department:
Oxford University Centre for the Environment
Role:
Author
ORCID:
0000-0001-5344-1924
More by this author
Institution:
University of Oxford
Department:
Oxford University Centre for the Environment
Role:
Author
More by this author
Institution:
University of Oxford
Department:
Engineering Science
Role:
Author
ORCID:
0000-0002-1802-6909
More by this author
Institution:
University of Oxford
Department:
Oxford University Centre for the Environment
Role:
Author



Language:
English
Pubs id:
pubs:974683
UUID:
uuid:7ab1d0e6-4bbe-40d5-9062-542de31e719e
Local pid:
pubs:974683
Source identifiers:
974683
Deposit date:
2019-07-04

Terms of use



Views and Downloads






If you are the owner of this record, you can report an update to it here: Report update to this record

TO TOP