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Temperature, rainfall and economic growth in Africa

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Abstract

Following a recent line of research, this paper investigates the aggregated effects of temperature and rainfall on economic growth in Africa. Our econometric approach is based on a reduced-form model and takes account explicitly of parameter heterogeneity and cross section dependence, relying on ARDL modelling and panel estimators with multifactor structures. We find clear supportive evidence of short- and long-run relations between temperature and per-capita GDP growth, while the role played by rainfall appears to be less important and the evidence on its statistical significance is less clear-cut. Very similar results are reported when the analysis is carried out by focusing solely on Sub-Saharan African countries or considering GDP growth per worker. This evidence is in sharp contrast to the results obtained via standard MG estimation and this confirms that, by not controlling for cross section dependence, traditional panel estimators are likely to provide misleading inference. The empirical results suggest that, far from adapting quickly to weather shocks, African economies appear to be significantly damaged by them. In the absence of corrective measures, the current trends in climate change may impose a progressively heavier burden on African countries.

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Notes

  1. This view is implicitly or explicitly shared by many studies in the literature, e.g. Brückner and Ciccone (2010); Miguel et al. (2004).

  2. For a more complete discussion of these points, see Barrios et al. (2010).

  3. The simulations in Barrios et al. (2010) suggest that, depending on the level of rainfall assumed as a benchmark, the per-capita GDP differential between Sub-Saharan African and non-African developing countries could have been 15-40 % lower than it turned out to be.

  4. Commenting the cross section estimation results in their Table 7, Dell et al. (2008) state that ‘The Africa sample shows similarly large effects in poor countries as other specifications, but the standard errors have increased with the substantially smaller sample size, so the result is not quite statistically significant’. (p. 23, footnote 27).

  5. This choice facilitates comparison of our results with the evidence presented by other studies, notably Dell et al. (2008) and Barrios et al. (2010), also centred on per-capita GDP.

  6. Our study covers approximately the same time span as Dell et al. (2008), which is longer than that considered by Barrios et al. (2010).

  7. We are grateful to Ben Jones for kindly making the dataset available.

  8. For a detailed description of the dataset, see Appendix I in Dell et al. (2008).

  9. Between the two extremes, the pooled mean group (PMG) approach, developed by Pesaran et al. (1999), combines both pooling and averaging. PMG estimation allows the intercept and short-run coefficients to differ, but restricts the long-run slope coefficients to be the same across groups. When this hypothesis is correct, the PMG estimator is more efficient than the MG approach. However, if the hypothesis of long-run parameter homogeneity is invalid, the PMG estimates are inconsistent while the MG estimator remains consistent. As there is no a priori reason to expect the long-run influence of temperature and rainfall to be the same for all countries in the sample, we do not rely on PMG estimation in this paper.

  10. See Appendix for a more detailed discussion of this point.

  11. The ‘common dynamic process’ is extracted from the pooled regression in thefirst differences as unobservables (as well as the possible presence of nonstationary variables) would lead to biased estimates in pooled levels regressions.

  12. Regarding the issues associated to second stage ‘regressions with generated regressors’ (Pagan 1984), Eberhardt and Teal (2010) point to the theoretical results in Bai and Ng (2008), who show that second stage standard errors need not be adjusted for first stage estimation uncertainty if \(\sqrt{T}/N\rightarrow 0\), as is arguably the case here. This is supported by simulation results in Bond and Eberhardt (2009), indicating that the average standard error of AMG estimates is of similar magnitude to the empirical standard deviation.

  13. Indeed, this is the key feature of the AMG estimator, which Eberhardt and Teal (2010) develop as an alternative to the CCE approach for macro production function estimation.

  14. We carried out lag selection tests for all the regressions reported in the paper, also using general-to-specific modelling methods. In all cases, the ARDL(1,0,0) turned out to be the most suitable model for the panel as a whole.

  15. There is broad consensus that climate and weather shocks can have important effects on Northern African countries too. The World Bank, for instance, talks openly of a water crisis in Middle East and North African (MENA) countries, where in many cases more water is consumed on average than is received in rainfall (e.g. Bucknall 2007).

  16. CCEMG and AMG estimations were carried out using the statistical software Stata 11 and the XTMG Stata module developed by Eberhardt (2012).

  17. The country-specific trends represent deviations from \(\hat{{\mu }}_t^{\bullet } \), so they enter with positive and negative magnitudes for different countries which average out across the sample. This explains the statistically insignificant mean of the trends in the AMG regressions.

  18. Note that the estimations in Dell et al. (2008) include a dummy variable for poor countries, which is also interacted with temperature and precipitation. The ‘poor dummy’ takes the value of 1 when the country has below-median PPP per-capita GDP in the first year of data—as most African countries fall in this category, the introduction of this dummy is unlikely to affect significantly the comparison with our own results.

  19. Given the different approach used, the estimates in Barrios et al. (2010) are not directly comparable to those presented in this paper. The closest possible counterpart to our results are the long-run estimates from the growth regression in their Table 4, column 2, which, however, includes a number of control variables. In this specification, the coefficient on rainfall is significant but very small (i.e. 0.014), while that on temperature is even smaller and not significant.

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Acknowledgments

The author would like to thank an anonymous Associate Editor of this journal and two anonymous referees for valuable comments and suggestions. The author is also grateful to Markus Eberhardt for many helpful observations. The usual disclaimer applies.

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Correspondence to Matteo Lanzafame.

Appendices

Appendix A

See Tables 5 and 6.

Table 5 \(\Delta \)lnP-models, CCEP and AMG estimations
Table 6 \(\Delta \)lnY-models, CCEP and AMG estimations

 

Appendix B

Bond and Eberhardt (2009) and Eberhardt and Teal (2010) show that the inclusion of the ‘common dynamic process’ \(\hat{{\mu }}_t^{\bullet } \) in the country regressions allows the AMG procedure to account for cross section dependence. In order to see the intuition behind this, consider the following empirical model

$$\begin{aligned} y_{it} ={\beta }^{\prime }_i x_{it} +u_{it} \end{aligned}$$
(B1)
$$\begin{aligned} u_{it} =\alpha _i +{\lambda }^{\prime }_i f_t +\varepsilon _{it} \end{aligned}$$
(B2)

where \(i=1,2,{\ldots },N\) and \(t=1,2,{\ldots },T\), while\(x_{it} \) is a \(k\times 1\) vector of explanatory variables, \(\beta _i \) are the \(k\times 1\) coefficient vectors,\(\alpha _i \) represents the (group-specific) fixed effect and \(f_t \) is a set of unobservable common factors with group-specific factor loading \(\lambda _i \). This is a simplified version of the model setup in Eberhardt and Teal (2010), which abstracts from the potential presence of multiple factors in the observable variables. Using (B2) into (B1) and first-differencing (to control for nonstationarity issues) we obtain

$$\begin{aligned} \Delta y_{it} ={\beta }^{\prime }_i \Delta x_{it} +{\lambda }^{\prime }_i \Delta f_t +\Delta \varepsilon _{it} \end{aligned}$$
(B3)

The AMG approach captures the common (or mean) evolution of unobservables across groups (e.g. countries) and over time via the inclusion of \(T-1\) year dummies \(\left( {\sum _{t=2}^T {\Delta D_t } } \right)\) in a pooled estimation of the model in (B3). Intuitively, if\(f_t \) is truly common across groups, in each year \(t\) the coefficient on the year dummy variable \(D_t \) will provide an average estimate of the common factors across groups in that particular year. Thus, the inclusion of \(T-1\) year dummies produces an estimate of how the common factors \(f_t \) evolve over time—this is the common dynamic process \(\hat{{\mu }}_t^{\bullet } \).

In other words, \(\hat{{\mu }}_t^{\bullet } \) is some function \(h\) of the common factors \(f_t \), i.e. \(\hat{{\mu }}_t^{\bullet } =h\left( {\bar{{\lambda }}f_t } \right)\). As such, \(\hat{{\mu }}_t^{\bullet } \) can be used as a proxy for \(f_t \) in the second stage of the AMG procedure as follows

$$\begin{aligned} y_{it} =\alpha _i +{\beta }^{\prime }_i x_{it} +{\lambda }^{\prime }_i h\left( {\bar{{\lambda }}f_t } \right)_t +\varepsilon _{it} \end{aligned}$$
(B4)

Provided that in (B3) the error term \(\Delta \varepsilon _{it} \) is white noise, the estimated common dynamic process \(\hat{{\mu }}_t^{\bullet } \) can be included in the second-stage AMG regression (B4) to control for the presence of common factors \(f_t \) and their heterogeneous effects on \(y_{it} \). The Monte Carlo simulations in Bond and Eberhardt (2009) provide substantial evidence on the performance of the AMG estimator, indicating that the inclusion of \(\hat{{\mu }}_t^{\bullet } \) in the second-stage regression allows for the separate identification of \(\beta _i \) and \(f_t \), and that the small-sample performance of the AMG approach broadly matches that of the CCEMG and CCEP estimators.

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Lanzafame, M. Temperature, rainfall and economic growth in Africa. Empir Econ 46, 1–18 (2014). https://doi.org/10.1007/s00181-012-0664-3

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