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Identifying Precipitation and Reference Evapotranspiration Trends in West Africa to Support Drought Insurance

May 29, 2020

West Africa represents a wide gradient of climates, extending from tropical conditions along the Guinea Coast to the dry deserts of the south Sahara, and it has some of the lowest income, most vulnerable populations on the planet, which increases catastrophic impacts of low and high frequency climate variability. This paper investigates low and high frequency climate variability in West African monthly and seasonal precipitation and reference evapotranspiration from the early 1980s to 2016. We examine the impact of those trends and how they interact with payouts from index insurance products. Understanding low and high frequency variability in precipitation and reference evapotranspiration at these scales can provide insight into trends during periods critical to agricultural performance across the region. For index insurance, it is important to identify low-frequency variability, which can result in radical departures between designed/planned and actual insurance payouts, especially in the later part of a 30-year period, a common climate analysis period. We find that evaporative demand and precipitation are not perfect substitutes for monitoring crop deficits and that there may be space to use both for index insurance design. We also show that low yields—aligned with the need for insurance payouts—can be predicted using classification trees that include both precipitation and reference evapotranspiration.

Publication Year 2020
Title Identifying Precipitation and Reference Evapotranspiration Trends in West Africa to Support Drought Insurance
DOI 10.3390/RS12152432
Authors Sari Blakeley, Stuart Sweeney, Gregory Husak, Laura Harrison, Chris Funk, Pete Peterson, Daniel E Osgood
Publication Type Article
Publication Subtype Journal Article
Series Title Remote Sensing
Index ID 70254533
Record Source USGS Publications Warehouse
USGS Organization Earth Resources Observation and Science (EROS) Center
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