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Dantes View
Dante's View is a viewpoint terrace at 1,669 m height, on the north side of Coffin Peak, along the crest of the Black Mountains overlooking the Badwater Basin salt flats.
Rec Temp: Aug. 17, 2020 - 130 degrees (54.4 degrees Celsius)
Why so hot?
The depth and shape of Death Valley influences its summer temperatures. The valley is a long, narrow basin that reaches down to 282 feet (86 m) below sea level, yet is walled by high, steep mountain ranges. The clear, dry air and sparse plant cover allow sunlight to heat the desert surface. Heat radiates back from the rocks and soil, then becomes trapped in the valley's depths. Summer nights provide little relief as overnight lows may only dip into the 85°F to 95°F (30°C to 35°C) range. Heated air rises, yet is trapped by the high valley walls, is cooled and recycled back down to the valley floor. These pockets of descending air are only slightly cooler than the surrounding hot air. As they descend, they are compressed and heated even more by the low elevation air pressure. These moving masses of super heated air blow through the valley creating extreme high temperatures.
Dantes View
Dante's View is a viewpoint terrace at 1,669 m height, on the north side of Coffin Peak, along the crest of the Black Mountains overlooking the Badwater Basin salt flats.
Rec Temp: Aug. 17, 2020 - 130 degrees (54.4 degrees Celsius)
Why so hot?
The depth and shape of Death Valley influences its summer temperatures. The valley is a long, narrow basin that reaches down to 282 feet (86 m) below sea level, yet is walled by high, steep mountain ranges. The clear, dry air and sparse plant cover allow sunlight to heat the desert surface. Heat radiates back from the rocks and soil, then becomes trapped in the valley's depths. Summer nights provide little relief as overnight lows may only dip into the 85°F to 95°F (30°C to 35°C) range. Heated air rises, yet is trapped by the high valley walls, is cooled and recycled back down to the valley floor. These pockets of descending air are only slightly cooler than the surrounding hot air. As they descend, they are compressed and heated even more by the low elevation air pressure. These moving masses of super heated air blow through the valley creating extreme high temperatures.