Plant physiological responses to rising CO2 modify simulated daily runoff intensity with implications for global-scale flood risk assessment
Climate change is expected to increase the frequency of flooding events and, thus, the risks of flood-related mortality and infrastructure damage. Global-scale assessments of future flooding from Earth system models based only on precipitation changes neglect important processes that occur within the land surface, particularly plant physiological responses to rising CO2. Higher CO2 can reduce stomatal conductance and transpiration, which may lead to increased soil moisture and runoff in some regions, promoting flooding even without changes in precipitation. Here we assess the relative impacts of plant physiological and radiative greenhouse effects on changes in daily runoff intensity over tropical continents using the Community Earth System Model. We find that extreme percentile rates increase significantly more than mean runoff in response to higher CO2. Plant physiological effects have a small impact on precipitation intensity but are a dominant driver of runoff intensification, contributing to one half of the 99th and one third of the 99.9th percentile runoff intensity changes.
document
http://n2t.net/ark:/85065/d7nk3j0n
eng
geoscientificInformation
Text
publication
2016-01-01T00:00:00Z
publication
2018-11-28T00:00:00Z
Copyright 2018 American Geophysical Union.
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