Global flood risk under climate change

Author:  ["Yukiko Hirabayashi","Roobavannan Mahendran","Sujan Koirala","Lisako Konoshima","Dai Yamazaki","Satoshi Watanabe","Hyungjun Kim","Shinjiro Kanae"]

Publication:  Nature Climate Change

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Tags:     Climate environment

Abstract

Flood risk is expected to increase as the climate warms. This study, for the first time, uses several climate models to estimate the global risk of flooding at the end of the century. Projections show a large increase in flood frequency in some areas, whereas other regions can expect a decrease. Vulnerability is dependent on the degree of warming and the interannual variability in precipitation. A warmer climate would increase the risk of floods1. So far, only a few studies2,3 have projected changes in floods on a global scale. None of these studies relied on multiple climate models. A few global studies4,5 have started to estimate the exposure to flooding (population in potential inundation areas) as a proxy of risk, but none of them has estimated it in a warmer future climate. Here we present global flood risk for the end of this century based on the outputs of 11 climate models. A state-of-the-art global river routing model with an inundation scheme6 was employed to compute river discharge and inundation area. An ensemble of projections under a new high-concentration scenario7 demonstrates a large increase in flood frequency in Southeast Asia, Peninsular India, eastern Africa and the northern half of the Andes, with small uncertainty in the direction of change. In certain areas of the world, however, flood frequency is projected to decrease. Another larger ensemble of projections under four new concentration scenarios7 reveals that the global exposure to floods would increase depending on the degree of warming, but interannual variability of the exposure may imply the necessity of adaptation before significant warming.

Cite this article

Hirabayashi, Y., Mahendran, R., Koirala, S. et al. Global flood risk under climate change. Nature Clim Change 3, 816–821 (2013). https://doi.org/10.1038/nclimate1911

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