Our study finds that during the wet season, Rossby waves play a significant role, contributing to the formation of high-pressure systems that intensify heat extremes. However, in the dry season, the signal is less clear, with noticeable differences between ERA5 data and AM4 model outputs. The warming scenarios (SSP5-8.5) indicate that future heatwaves could become more intense and longer-lasting, largely due to greater soil moisture depletion and reduced evaporative cooling.
These findings point to the need for better model simulations, particularly for the dry season. Future work could involve refining the calculation methods, exploring additional metrics like heat index or wet bulb temperature, and integrating coupled ocean simulations to better understand the dynamics at play. This research is crucial for improving our understanding of heatwave behavior in an understudied region like Eritrea, with significant implications for public health, agriculture, and ecosystems.
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