Abstract
This article approaches some of the current rainfall derivatives pricing and operational challenges through an empirical application to Comunidad Valenciana, Spain. Regarding the former, two different issues are addressed. First, we examine the rightness of suggesting the Gamma distribution to price rainfall contracts, which is the alternative chosen by previous authors applying the Index Value Simulation technique. This is done for the purpose of determining whether the consideration and comparison of other alternatives may lead to more accurate valuation results. Concretely, two different distributions, in addition to the Gamma, are proposed: the exponential and the mixed exponential, whose fits are assessed through the Kolmogorov–Smirnov/Lilliefors test and graphical analyses. The outcomes attained indicate that this selection process leads indeed to a precise generation of the rainfall index’s moments. Next, we examine the viability of using a unique distribution to model the rainfall risk of regions located nearby, since this would considerably decrease valuation complexity. Our analysis shows that the most convenient choice depends on the period and location considered, although the mixed exponential appears as a reasonable option in most cases. Finally, a relevant operational challenge related to geographical basis risk is approached. Concretely, an evaluation of this type of risk among the locations studied is conducted. The results attained indicate that, given the insufficient degree of correlation between nearby locations, rainfall risk hedging measures may rely on compound derivatives referred to several neighbor stations.
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Notes
The KS test requires that the parameters of the theoretical distribution have not been estimated from the same bunch of data used to apply this test (Blain 2014, p. 193). As in this case this requirement is not fulfilled, the probability of accepting a false H0 becomes high and a change in the original KS test needs to be implemented. The corrected test is called KS/Lilliefors and relies on Monte Carlo simulations to attain more accurate p-values. First, many samples (in this case, 4999) of the same size than the observed sample are generated. For that purpose, the MLE parameters of the observed sample are used. After that, the MLE parameters of the distribution of each of the random samples are estimated. Then, the KS test is applied to each of the samples, using their estimated parameters. Finally, the p-value is computed as the proportion of test statistics D equal or higher than the test statistic obtained from the KS test applied to the observed sample. A value of one is included in numerator and denominator to allow the observed sample to be represented within the null distribution (Manly 2007, pp. 4–9).
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Acknowledgements
The Project which has generated these results has been supported by a grant of Fundación Bancaria “la Caixa” (ID 100010434), whose code is LCF/BQ/ES16/11570002. The authors are thankful to Professor Joan Montllor-i-Serrats (UAB) for interesting insights on previous stages of this research. They are also grateful to the anonymous referee and Gurdip Bakshi (the editor) for providing helpful comments.
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Martínez Salgueiro, A., Tarrazon-Rodon, MA. Approaching rainfall-based weather derivatives pricing and operational challenges. Rev Deriv Res 23, 163–190 (2020). https://doi.org/10.1007/s11147-019-09161-0
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DOI: https://doi.org/10.1007/s11147-019-09161-0