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Impact of ET 0 method on the simulation of historical and future crop yields: a case study of millet growth in Senegal
Author(s) -
Ramarohetra Johanna,
Sultan Benjamin
Publication year - 2018
Publication title -
international journal of climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.58
H-Index - 166
eISSN - 1097-0088
pISSN - 0899-8418
DOI - 10.1002/joc.5205
Subject(s) - evapotranspiration , yield (engineering) , precipitation , crop yield , variable (mathematics) , mathematics , climate change , crop , climatology , environmental science , statistics , agricultural engineering , meteorology , geography , agronomy , ecology , geology , forestry , thermodynamics , mathematical analysis , physics , engineering , biology
The reference evapotranspiration (ET 0 ) is an integrated climatic variable from which many crop models derive simulated crop yields. In most of these models, different equations are parameterized leaving the choice of the equation to the user. However, the impact of the choice of the ET 0 equations on crop yield prediction has been little studied. The present study proposes a sensitivity analysis of the impact of the choice of the ET 0 equation on simulated millet yields using SARRA‐H crop model over 12 Senegalese stations representative of the Sudano‐Sahelian climate conditions of West Africa. Priestley‐Taylor, a modified Priestley‐Taylor and Hargreaves equations lead to simulated yields up to 19% than those calculated using the Penman‐Monteith equation. Despite high biases in wind speed, among the tested methods, the Penman‐Monteith method remains the most robust to derive ET 0 and yield over the major part of Senegal, Hargreaves equation being more appropriated under dry climates. The choice of ET 0 formulation introduces uncertainties representing 8% of baseline yield regardless of precipitation changes; for wet conditions these uncertainties approach 30% of the overall climate change impact. The choice of ET 0 equation is increasingly important, with local temperature changes out to 4 °C, while extreme changes above 6 °C depend less on the ET 0 equation.