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      A review of the effects of climate change on riverine flooding in subtropical and tropical regions

      1 , 1 , 2
      Journal of Water and Climate Change
      IWA Publishing

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          Abstract

          Tropical and subtropical regions can be particularly severely affected by flooding. Climate change is expected to lead to more intense precipitation in many regions of the world, increasing the frequency and magnitude of flood events. This paper presents a review of studies assessing the impacts of climate change on riverine flooding in the world's tropical and subtropical regions. A systematic quantitative approach was used to evaluate the literature. The majority of studies reported increases in flooding under climate change, with the most consistent increases predicted for South Asia, South East Asia, and the western Amazon. Results were more varied for Latin America and Africa where there was a notable paucity of studies. Our review points to the need for further studies in these regions as well as in Australia, in small to mid-sized catchments, and in rapidly urbanising catchments in the developing world. Adoption of non-stationary flood analysis techniques and improved site-specific socio-economic and environmental model scenarios were identified as important future directions for research. Data accessibility and mitigation of model uncertainty were recognised as the principal issues faced by researchers investigating the impacts of climate change on tropical and subtropical rivers.

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          Trends in Intense Precipitation in the Climate Record

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            Increasing risk of great floods in a changing climate.

            Radiative effects of anthropogenic changes in atmospheric composition are expected to cause climate changes, in particular an intensification of the global water cycle with a consequent increase in flood risk. But the detection of anthropogenically forced changes in flooding is difficult because of the substantial natural variability; the dependence of streamflow trends on flow regime further complicates the issue. Here we investigate the changes in risk of great floods--that is, floods with discharges exceeding 100-year levels from basins larger than 200,000 km(2)--using both streamflow measurements and numerical simulations of the anthropogenic climate change associated with greenhouse gases and direct radiative effects of sulphate aerosols. We find that the frequency of great floods increased substantially during the twentieth century. The recent emergence of a statistically significant positive trend in risk of great floods is consistent with results from the climate model, and the model suggests that the trend will continue.
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              sdsm — a decision support tool for the assessment of regional climate change impacts

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                Author and article information

                Journal
                Journal of Water and Climate Change
                IWA Publishing
                2040-2244
                2408-9354
                December 01 2019
                August 26 2019
                December 01 2019
                August 26 2019
                : 10
                : 4
                : 687-707
                Affiliations
                [1 ]School of Engineering and Built Environment, Griffith University, Gold Coast Campus, Gold Coast, Queensland 4215, Australia
                [2 ]Australian Rivers Institute, Griffith University, Nathan Campus, Brisbane, Queensland 4111, Australia
                Article
                10.2166/wcc.2019.175
                115cb61a-adc7-480a-883b-7133dea7fc8b
                © 2019
                History

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