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Droughts

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Hydrometeorology

Abstract

Droughts usually arise from a shortfall in precipitation, and can be exacerbated by increases in demand for water supply, agriculture and other applications. The onset of a drought is often recognised through the impacts on key water users, and may include meteorological, hydrological, groundwater, agricultural and socioeconomic droughts. Some difficulties in forecasting the onset and progression of droughts include factors such as their slowly developing nature, the large spatial extent, and the spatial and temporal variations in impacts which often occur. This has led to the development of a wide range of possible indices and indicators, of which several may be used operationally to identify different stages in the progression of a drought. For short-term forecasts, forecasting techniques range from simple regression techniques through to integrated catchment models driven by rainfall observations and forecasts. At longer time scales, ensemble forecasting techniques are widely used, together with statistical techniques relating conditions to oceanic and atmospheric phenomena such as the El Niño-Southern Oscillation. These methods may also be combined with forecasting techniques for individual applications, such as supply-demand models for water resources operations, and crop simulation models for irrigation scheduling. This chapter presents an introduction to these topics, and includes several examples of operational drought warning systems.

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Correspondence to Kevin Sene .

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Sene, K. (2010). Droughts. In: Hydrometeorology. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-3403-8_8

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