Arabian Gulf | The growth of the tropical air rise in the coming period and the beginning of a rise in temperatures

Written By هشام جمال on 2023/05/07

This article was written originally in Arabic and is translated using a 3rd party automated service. ArabiaWeather is not responsible for any grammatical errors whatsoever.

<p style=";text-align:left;direction:ltr"><strong>Arab Weather -</strong> Weather forecasters at the Arab Regional Weather Center said that the latest outputs of the processed numerical models indicate a growth of the tropical air rise over the Arab Gulf countries during the coming period, which leads to an increase in air heating near the surface of the earth, which is reflected in temperatures.</p><p style=";text-align:left;direction:ltr"></p><p style=";text-align:left;direction:ltr"><br /> In the details, it is expected, God willing, that the impact of the tropical air rise will increase on the Arab Gulf countries during the coming period, especially Qatar, Bahrain, the Emirates and the Sultanate of Oman, where a rise in temperatures will occur in the coming period to be in forty levels even in capitals, including the capital, Riyadh, and hot to very hot weather prevails. During the daytime hours, while the weather becomes warm to relatively hot at night.</p><p style=";text-align:left;direction:ltr"></p><h2 style=";text-align:left;direction:ltr"><br /> <strong>What is the Tropical High and how does it contribute to the rise in temperatures?</strong></h2><p style=";text-align:left;direction:ltr"></p><p style=";text-align:left;direction:ltr"> The tropical atmospheric elevation is that belt of high atmospheric pressure that extends transversely (east-west) centered around latitude 30 north and south, and the reason for the existence of this pressure is due to the fall of large masses of air in the upper part of the variable atmosphere (tropoposphere), but this belt It is characterized by its non-continuity, as it is divided into compartments as a result of the overlapping of land and water masses, and the different surface appearances. Subtropical high pressure compartments in the hemispheres form the source of the trade winds and reverse winds (the westerlies of the middle latitudes).</p><p style=";text-align:left;direction:ltr"></p><p style=";text-align:left;direction:ltr"> The tropical air rise contributes to the process of heating the layers of the atmosphere close to the surface of the earth. The subtropical air rise (the rise in the geofencing values) contributes to the occurrence of what is known as the &quot;heat dome&quot; phenomenon, which would increase the values of the sinking air - As it compresses the air in the lower layers of the atmosphere, causing a rise in temperatures.</p><p style=";text-align:left;direction:ltr"></p><p style=";text-align:left;direction:ltr"><br /> God knows.</p>

This article was written originally in Arabic and is translated using a 3rd party automated service. ArabiaWeather is not responsible for any grammatical errors whatsoever.


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