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We investigate the consequences of remittances inflows on the macroeconomic performance of West African countries over the 1985–2007 period. We take into account the exposure of those countries to climate variability by estimating a PCHVAR model which allows heterogeneity between countries’ responses to rainfall shocks. Our results show that the impact of remittances on macroeconomic performance is highly sensitive to those shocks. In particular, when drought conditions prevail, remittances no longer exert any short-term spillover effects on growth and may increase a situation of economic dependence, by spurring agricultural imports.

This paper contributes to the climate-economy literature by analysing the role of weather patterns in influencing the transmission of global climate cycles to economic growth. More specifically, we focus on El Niño Southern Oscillation (ENSO) events and their interactions with local weather conditions, taking into account the heterogeneous and cumulative effects of weather patterns on economic growth and the asymmetry and nonlinearity in the global influence of ENSO on economic activity. Using data on 75 countries over the period 1975-2014, we provide evidence for the negative growth effects of ENSO events and show that there are substantial differences between its warm (El Niño) and cold (La Niña) phases and between climate zones. These differences are due to the heterogeneity in weather responses to ENSO events, known as teleconnections, which has so far not been taken into account by economists, and which will become more important in the climate-economy relationship given that climate change may substantially strengthen long-distance relationships between weather patterns around the world. We also show that the negative growth effects associated with these teleconnections are robust to the definition of ENSO events and more important over shorter meteorological onsets.

Nous mettons en évidence un effet non linéaire exercé par les conditions hydro-climatiques, mesurées par un indicateur standardisé de précipitation et d’évapotranspiration, sur la croissance économique d’un échantillon de pays en développement de 1980 à 2011. Nous montrons (i) que cette relation non linéaire s’observe uniquement pour les pays à dominante agricole, et (ii) que les conditions hydro-climatiques à l’origine des changements de régime sont beaucoup plus faibles que celles correspondant à des conditions extrêmes.