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The Great Salt Lake Desert, located near the northeast corner of the Great Basin desert, is an excellent example of a cold desert climate. Although still arid, it is worthy to note that this portion of the desert receives more precipitation than the similar playas and salt pans on the western edge of the Great Basin desert.
It is noted for both its arid climate and the basin and ... Most Great Basin precipitation ... The next group to live in the area was the Great Basin Desert Archaic ...
The Ladakh region and the city of Leh in the Great Himalayas in India also have a cold desert climate. In North America, the cold desert climate occurs in the drier parts of the Great Basin Desert and the Bighorn Basin in Big Horn and Washakie County in Wyoming. The Hautes Plaines, located in the northeastern section of Morocco and in Algeria ...
There are three main deserts in California: the Mojave Desert, the Colorado Desert, and the Great Basin Desert. [5]: 408 The Mojave Desert is bounded by the Tehachapi Mountains on the northwest, the San Gabriel and San Bernardino Mountains on the south, and extends eastward to California's borders with Arizona and Nevada; it also forms portions of northwest Arizona.
Death Valley is a desert valley in Eastern California, in the northern Mojave Desert, bordering the Great Basin Desert. It is thought to be the hottest place on Earth during summer. [3] Death Valley's Badwater Basin is the point of lowest elevation in North America, at 282 feet (86 m) below sea level. [1]
The high desert of Oregon is located in the central and southeastern parts of the state. It covers approximately 24,000 square miles (62,000 km 2), extending approximately 200 miles (320 km) from central Oregon east to the Idaho border and 130 miles (210 km) from central Oregon south to the Nevada border. [1]
Nelson Peak is set within the Great Basin Desert which has hot summers and cold winters. [6] The desert is an example of a cold desert climate as the desert's elevation makes temperatures cooler than lower elevation deserts.
The drier areas are the Desert Southwest, Great Basin, valleys of northeast Arizona, eastern Utah, and central Wyoming. [4] [5] Increased warming within urban heat islands leads to an increase in rainfall downwind of cities. [6]
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