Literature DB >> 33641464

Towards advancing scientific knowledge of climate change impacts on short-duration rainfall extremes.

Hayley J Fowler1, Haider Ali1, Richard P Allan2, Nikolina Ban3, Renaud Barbero4, Peter Berg5, Stephen Blenkinsop1, Nalan Senol Cabi6, Steven Chan1,7, Murray Dale8, Robert J H Dunn7, Marie Ekström9, Jason P Evans10, Giorgia Fosser11, Brian Golding12, Selma B Guerreiro1, Gabriele C Hegerl13, Abdullah Kahraman1,7, Elizabeth J Kendon7, Geert Lenderink14, Elizabeth Lewis1, Xiaofeng Li1, Paul A O'Gorman15, Harriet G Orr16, Katy L Peat1,16, Andreas F Prein17, David Pritchard1, Christoph Schär18, Ashish Sharma19, Peter A Stott7,20, Roberto Villalobos-Herrera1,21, Gabriele Villarini22, Conrad Wasko23, Michael F Wehner24, Seth Westra25, Anna Whitford1.   

Abstract

A large number of recent studies have aimed at understanding short-duration rainfall extremes, due to their impacts on flash floods, landslides and debris flows and potential for these to worsen with global warming. This has been led in a concerted international effort by the INTENSE Crosscutting Project of the GEWEX (Global Energy and Water Exchanges) Hydroclimatology Panel. Here, we summarize the main findings so far and suggest future directions for research, including: the benefits of convection-permitting climate modelling; towards understanding mechanisms of change; the usefulness of temperature-scaling relations; towards detecting and attributing extreme rainfall change; and the need for international coordination and collaboration. Evidence suggests that the intensity of long-duration (1 day+) heavy precipitation increases with climate warming close to the Clausius-Clapeyron (CC) rate (6-7% K-1), although large-scale circulation changes affect this response regionally. However, rare events can scale at higher rates, and localized heavy short-duration (hourly and sub-hourly) intensities can respond more strongly (e.g. 2 × CC instead of CC). Day-to-day scaling of short-duration intensities supports a higher scaling, with mechanisms proposed for this related to local-scale dynamics of convective storms, but its relevance to climate change is not clear. Uncertainty in changes to precipitation extremes remains and is influenced by many factors, including large-scale circulation, convective storm dynamics andstratification. Despite this, recent research has increased confidence in both the detectability and understanding of changes in various aspects of intense short-duration rainfall. To make further progress, the international coordination of datasets, model experiments and evaluations will be required, with consistent and standardized comparison methods and metrics, and recommendations are made for these frameworks. This article is part of a discussion meeting issue 'Intensification of short-duration rainfall extremes and implications for flash flood risks'.

Entities:  

Keywords:  Clausius–Clapeyron; climate change; extreme precipitation; flooding; short-duration; sub-daily

Year:  2021        PMID: 33641464     DOI: 10.1098/rsta.2019.0542

Source DB:  PubMed          Journal:  Philos Trans A Math Phys Eng Sci        ISSN: 1364-503X            Impact factor:   4.226


  2 in total

1.  Towards Quantifying the Uncertainty in Estimating Observed Scaling Rates.

Authors:  Haider Ali; Hayley J Fowler; David Pritchard; Geert Lenderink; Stephen Blenkinsop; Elizabeth Lewis
Journal:  Geophys Res Lett       Date:  2022-06-18       Impact factor: 5.576

2.  Intensification of short-duration rainfall extremes and implications for flood risk: current state of the art and future directions.

Authors:  Hayley J Fowler; Conrad Wasko; Andreas F Prein
Journal:  Philos Trans A Math Phys Eng Sci       Date:  2021-03-01       Impact factor: 4.226

  2 in total

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