Middle East Geography & Climate

The Arabian Peninsula (Saudi Arabia, UAE, Qatar, Bahrain, Oman, Yemen) is dominated by vast desert, including the Rub' al Khali (Empty Quarter), one of the largest continuous sand deserts on Earth, ringed by a long Gulf and Red Sea coastline and, in Oman specifically, dramatic mountains and fjord-like coastal inlets.

The Levant (Jordan, Lebanon, Syria, Israel) is geographically compact but varied — Lebanon's own mountains rise directly from the Mediterranean coast, Jordan's desert holds Petra's rock-cut city and the otherworldly landscape of Wadi Rum, and the Dead Sea (bordering Jordan and Israel) is the lowest point on Earth's land surface.

Iran is a large, geographically diverse country spanning the Zagros and Alborz mountain ranges, the Caspian Sea coast, and a substantial arid central plateau. Iraq is defined by the Tigris and Euphrates rivers and the fertile plain between them. Turkey spans both European and Asian territory across the Bosphorus, ranging from Istanbul's straits to Anatolia's central plateau and Cappadocia's distinctive volcanic rock formations.

Most of the Arabian Peninsula (Saudi Arabia, UAE, Qatar, Bahrain, Yemen) has a hot desert climate with extreme summer heat (often exceeding 40°C/104°F) and mild, far more comfortable winters; Oman's own mountainous regions offer some relief from the coastal heat.

The Levant (Jordan, Lebanon, Syria, Israel) has a Mediterranean climate along the coast — mild, wet winters and hot, dry summers — transitioning to desert conditions further inland and east.

Iran and Iraq both have significant continental climate variation: hot, dry summers and cold winters across much of the interior, with Iran's own mountain regions considerably cooler than its arid plateau and coastal areas.

Turkey has a genuine four-season climate, Mediterranean along its southern and western coasts and increasingly continental (colder winters, hot summers) moving into its central Anatolian interior.