Abstract

The projection of the future climate changes is of paramount importance inasmuch as it contributes to provide useful information for adaptation planning worldwide to local scales. This study investigated the future changes using four temperature related indices based on an ensemble of 14 CORDEX-Africa simulations at 0.44° × 0.44° of resolution under the RCP4.5 and RCP8.5 scenarios. These indices indicate moderate extremes over Côte d’Ivoire. The results show an increase in the warm extreme indices such as the warm spell days index (HWFI), very warm days frequency index (TX90P), and the warm nights frequency index (TN90P) over the entire country under both emission scenarios. The increase in these indices was higher under RCP8.5 and reached 85, 72, and 90% for HWFI, TX90P, and TN90P respectively. In addition, the magnitude of the changes is relevant along the coastal areas in the 2031–2060 and 2071–2100 periods. Moreover, the intra period extreme temperature range (ETR) shows future decrease following a south-north gradient with values in the range [−0.5; 1.5°C] over the country during January–March (JFM) and October–December (OND) seasons whereas an increase (~0.5°C) is projected for April–June (AMJ) and July–September (JAS) seasons, particularly in the central and northern parts. The minimum temperature increases faster than the maximum, except in AMJ and JAS in the central and northern regions. On the other hand, the changes in the indices based on the mean values of the reference period (1976–2005) are in concordance to the expected warming at the end of the twenty-first century with important trends. The projected changes are, however, subject to uncertainties, which are higher under RCP8.5 than under RCP4.5 scenarios. Overall, these changes are meaningful as all the 14 CORDEX-Africa simulations agree to an increase of warm extreme temperature.

Highlights

  • Is agrees with the warming observed over the continent for the past 50–100 years [26]

  • We assessed the future changes in temperature indices describing moderate extreme events as they occur several times per season or per year [74]; such as warm spell days index (HWFI), warm days (TX90P), warm nights (TN90P) frequencies and intra-period extreme temperature range (ETR). is country scale assessment focusing on Côte d’Ivoire uses an ensemble of 14 CORDEX Africa simulations to project modi cations in the near future (2031–2060) and far future (2071–2100) periods under IPCC’s Representative Concentration Pathway scenarios (RCP4.5 and RCP8.5)

  • Our results reveal an increase in warm extreme temperature events in Côte d’Ivoire in the future, leading to a decrease of ETR index, considering both forcing RCP4.5 and RCP8.5 scenarios

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Summary

Coastal Atlantic ocean

1: Map of Côte d’Ivoire including the climatic zones (adapted from [34, 41]). scale in Niamey (Niger) and Abidjan (Côte d’Ivoire) using weather stations in West Africa, and found signi cant warming trends. 1: Map of Côte d’Ivoire including the climatic zones (adapted from [34, 41]). Few works focusing in future changes in temperature have been done at the country level, especially, Côte d’Ivoire. Us, the current study analyses future changes in extreme temperature over Côte d’Ivoire and assesses the associated uncertainties using an ensemble of fourteen CORDEX-Africa simulations under RCP4.5 and RCP8.5 scenarios. E study area is Côte d’Ivoire domain which extends from 9°W to 2.5°W longitude and 4°N to 11°N latitude, with a total landmass of about 322,462 km (Figure 1). TNNi is the minimum of the minimum temperature and TXXi is the maximum of the maximum temperature All these terms are used to calculate the ETR and ETCCDI (HWFI, TX90P and TN90P) indices that are given in bold. Definition Warm spells duration index Intra period extreme temperature range Warm days

Warm nights
Deg C
ETR JFM
Results and Discussion
HWFI OND
Summary and Conclusion
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