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The continuation of high temperatures and summer weather in parts of the region, despite the approaching end of the summer season astronomically, contributes to increasing the chances of developing weather instability associated with the extension of the Red Sea Low. Warm, moist air interacts with cold air masses coming from upper atmospheric layers, raising the likelihood of cumulus cloud formation and the occurrence of thunderstorm rains. The ongoing warmth can also improve the conditions necessary for cloud growth and the development of unstable weather conditions, promising good prospects for clouds and potential rain in the upcoming period.
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