Climate Dynamics

, Volume 38, Issue 9, pp 1849–1865

Examining evapotranspiration trends in Africa


    • Department of Geography, Climate Hazards GroupUniversity of California Santa Barbara
  • Christopher Funk
    • US Geological Survey Earth Resources Observation and Science (EROS) Center, Department of GeographyUniversity of California Santa Barbara
  • Joel Michaelsen
    • Department of Geography, Climate Hazards GroupUniversity of California Santa Barbara

DOI: 10.1007/s00382-012-1299-y

Cite this article as:
Marshall, M., Funk, C. & Michaelsen, J. Clim Dyn (2012) 38: 1849. doi:10.1007/s00382-012-1299-y


Surface temperatures are projected to increase 3–4°C over much of Africa by the end of the 21st century. Precipitation projections are less certain, but the most plausible scenario given by the Intergovernmental Panel on Climate Change (IPCC) is that the Sahel and East Africa will experience modest increases (~5%) in precipitation by the end of the 21st century. Evapotranspiration (Ea) is an important component of the water, energy, and biogeochemical cycles that impact several climate properties, processes, and feedbacks. The interaction of Ea with climate change drivers remains relatively unexplored in Africa. In this paper, we examine the trends in Ea, precipitation (P), daily maximum temperature (Tmax), and daily minimum temperature (Tmin) on a seasonal basis using a 31 year time series of variable infiltration capacity (VIC) land surface model (LSM) Ea. The VIC model captured the magnitude, variability, and structure of observed runoff better than other LSMs and a hybrid model included in the analysis. In addition, we examine the inter-correlations of Ea, P, Tmax, and Tmin to determine relationships and potential feedbacks. Unlike many IPCC climate change simulations, the historical analysis reveals substantial drying over much of the Sahel and East Africa during the primary growing season. In the western Sahel, large increases in daily maximum temperature appear linked to Ea declines, despite modest rainfall recovery. The decline in Ea and latent heating in this region could lead to increased sensible heating and surface temperature, thus establishing a possible positive feedback between Ea and surface temperature.


Evapotranspiration Climate change Land surface models VIC Africa

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© Springer-Verlag 2012