Evidence that extreme rainfall intensity is increasing at the global scale has strengthened
considerably in recent years. Research now indicates that the greatest increases are likely to occur in
short-duration storms lasting less than a day, potentially leading to an increase in the magnitude and
frequency of flash floods. This review examines the evidence for subdaily extreme rainfall intensification
due to anthropogenic climate change and describes our current physical understanding of the association
between subdaily extreme rainfall intensity and atmospheric temperature. We also examine the nature,
quality, and quantity of information needed to allow society to adapt successfully to predicted future
changes, and discuss the roles of observational and modeling studies in helping us to better understand the
physical processes that can influence subdaily extreme rainfall characteristics. We conclude by describing
the types of research required to produce a more thorough understanding of the relationships between
local-scale thermodynamic effects, large-scale atmospheric circulation, and subdaily extreme rainfall intensity.
Figure 4. Conceptual overview of cloud feedbacks in relation to moisture availability, depicting (left) the reference situation and three possible future situations: (a) with
the same cloud dynamics and warmer and moister air entering the cloud from the same source area, (b) with stronger cloud dynamics, and warmer and moister air
entering the cloud from the same source area, and (c) with warmer and moister air entering the cloud from a greater source area due to enhanced cloud dynamics.
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Last updated 29 November 2013