Qatar | Haqban clouds strongly affect Doha and a number of areas, and their impact is expected to continue in the coming hour

<p style=";text-align:left;direction:ltr">Arab Weather - The latest satellite images show large amounts of cumulonimbus clouds forming to the north and northeast of Qatar, <strong><u>causing moderate to heavy rains to fall on Al Rayyan, Al Wakra and Al Khor, in addition to the capital Doha, while some interior parts are witnessing descending winds that raise dust and dirt.</u></strong></p><p style=";text-align:left;direction:ltr"></p><p style=";text-align:left;direction:ltr"> <a href="https://www.arabiaweather.com/ar/%D8%B5%D9%88%D8%B1-%D8%A7%D9%84%D8%A3%D... the movement of thunderstorm clouds in the Qatari sky from here</a><br /><br /></p><p style=";text-align:left;direction:ltr"> The latest weather forecasts indicate that the clouds known locally as Haqban clouds will continue to develop in these areas, and will begin to recede starting in the afternoon hours, and God knows best.</p><p style=";text-align:left;direction:ltr"></p><p style=";text-align:left;direction:ltr"> <strong>What are the drawdowns?</strong></p><p style=";text-align:left;direction:ltr"></p><p style=";text-align:left;direction:ltr"> Al-Haqban clouds are medium to high altitude clouds that appear in the sky during the pre-Wasmi period. They are clouds that indicate that the region is entering a transitional phase between the hot and dry summer and the fall season, when the weather begins to gradually change with a decrease in temperatures and an increase in humidity levels.</p><p style=";text-align:left;direction:ltr"></p><p style=";text-align:left;direction:ltr"> <a href="https://www.arabiaweather.com/ar/content/%D9%85%D8%A7-%D9%87%D9%8A-%D8%B... details about withdrawing the two eras from here</a></p><p style=";text-align:left;direction:ltr"></p><p style=";text-align:left;direction:ltr"> The clouds are characterized by their sometimes bright white color, and they are often of the cumulus or stratus type. These clouds are formed by the meeting of cold northwesterly winds with warm southeasterly air masses, which leads to the lifting of moist air, and the formation of these cloud formations.</p>