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  1. Alamy. Yazd is said to have the most wind catchers of any city in the world (Credit: Alamy) From ancient Egypt to the Persian Empire, an ingenious method of catching the breeze kept people cool ...

  2. A shamal (Arabic: شمال, 'north') is a northwesterly wind blowing over Iraq and the Persian Gulf states (including Saudi Arabia and Kuwait), often strong during the day, but decreasing at night. This weather effect occurs from once to several times a year, mostly in summer, but sometimes in winter.

  3. en.wikipedia.org › wiki › KhamsinKhamsin - Wikipedia

    Khamsin, chamsin or hamsin (Arabic: خمسين ḫamsīn, meaning "fifty"), more commonly known in Egypt as khamaseen (Egyptian Arabic: خماسين ḫamāsīn, IPA: [xɑmæˈsiːn] ⓘ), is a dry, hot, sandy local wind affecting Egypt and the Levant; similar winds, blowing in other parts of North Africa, the Arabian Peninsula ...

  4. 27 de sept. de 2018 · Wind catchers are tall, chimney-like structures that protrude from the rooftops of older houses in many of Iran’s desert cities. In their simplest form, wind catchers harness the cool breezes...

  5. en.wikipedia.org › wiki › HaboobHaboob - Wikipedia

    Middle East. Haboobs have been observed in the Sahara, Sahel (typically Sudan, where they were named and described), as well as across the Arabian Peninsula, throughout Kuwait, and in the most arid regions of Iraq. Haboob winds in the Arabian Peninsula, Iraq, and Kuwait are frequently created by the collapse of a thunderstorm. North ...

  6. 7 de dic. de 2015 · Abstract The Middle Eastern Shamal is a strong north-northwesterly wind, capable of lifting dust from the Tigris-Euphrates basin and transporting it to the Persian Gulf and Arabian Peninsula. The p...

  7. 19 de sept. de 2022 · Abstract. A new structure is proposed to explain the mechanism governing the summer Shamal wind (SSW) formation in the Middle East (ME). Here, the irreplaceable role of the Zagros Mountains (ZAG) as the primary driver of a localized atmospheric circulation over the ME has been clarified.

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