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Drought is a complex concept with both physical and socially constructed components. The idea of a drought conjures a popular image of cracked brown earth, fallow agricultural fields, and suffering human communities. This realistic image confuses the physical drought hazard with the social impacts of drought in contexts with high drought risk. Drought does not lend itself to a single, universal definition because drought has different spatial and temporal characteristics in distinct climates and regions. Drought hazard refers to the physical phenomenon of a meteorological drought, generally defined as a departure from a long-term precipitation (e.g, rainfall or snowfall) average that results in an impact in a specific place. A drought is a temporary yet recurring phenomenon that occurs in all climates, but occurs with a greater frequency and more severe impacts under certain regional conditions than in others.

Unlike other hazards such as floods and tropical storms, a drought is gradual or “creeping.” Drought hazards are spatially vast and affect more people worldwide than do other “natural” disasters. Notable drought-prone regions of the world include Australia, Northern Mexico, northeast Brazil, Western Africa, and southwestern United States. With respect to drought, Africa experiences the greatest loss of life, Asia has the most people affected, and the West sustains the highest economic damages. Drought can lead to a massive loss of life, famine, desertification, deforestation, loss of livelihood, and migration.

Drought risk refers to the vulnerability associated with the exposure of an individual, a community, or a region to a drought hazard, as well as the capacity of that entity to adapt or respond in an effective way to the drought hazard. A drought hazard does not in itself cause a social disaster. Rather, socioeconomic attributes and policy choices determine whether a meteorological drought will create conditions of high drought risk. For example, in a poor country with a high proportion of subsistence farmers, a drought may imperil the country's overall food security, while in a country with high levels of imported foods and widespread irrigation, a drought may have limited impacts. Drought hazard and risk are therefore separate yet related concepts.

Drought Types

Donald Wilhite, a geographer and former director of the U.S. National Drought Mitigation Center, defines four distinct types of drought: meteorological drought, hydrological drought, agricultural drought, and socioeconomic drought. At their root, all droughts originate as meteorological drought, defined as a deficiency in precipitation over a preestablished time period relative to an accepted “normal” longer-term historical average (e.g., 75% of normal precipitation over a 6-month period). Meteorological droughts in turn give rise to other identifiable types of drought. Agricultural drought refers to an insufficiency in soil water to support crop and forage growth; regional variations in crops and soil types help condition whether decreased precipitation develops into an agricultural drought. Hydrological drought occurs when there are insufficient surface and groundwater supplies to fulfill multiple and competing water demands, including irrigation, hydroelectric power, domestic use, and ecosystem management. Socioeconomic drought is at the nexus of the supply and demand for water or an economic good reliant on water (e.g., hydroelectric power). The supply is variable, based on precipitation and water availability, while the demand is conditioned by dynamic social factors such as demographic change and economic development trends. A precise definition of drought with regard to its type, timing, climate, and region can help in the development of targeted adaptive responses.

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