Several factors give the summit of Waialeale more potential to create precipitation than the rest of the island chain:
1. Its northern position relative to the main
2. It has a relatively round and regular conica
l shape, exposing all sides of its peak to winds and the moisture that they carry.
3. Its peak lies just below the so-called trade wind inversion layer of 6,000 feet (1,800 m), above which trade-wind-produced clouds cannot rise.
4. And most importantly, the steep cliffs cause the moisture-laden air to rise rapidly - over 3,000 feet (910 m) in less than 0.5 miles (0.80 km) - and drop a large portion of its rain in one spot, as opposed to spreading the rain out over a larger area if the slope were more gradual.
The great rainfall in the area produces the Alaka’i Wilderness Preserve, a large boggy area that is home to many rare plants. The ground is so wet that although trails exist, access by foot to the Waialeale area is extremely difficult.
credited to wikipedia and flickr: anand.shroff,NicBarca, volcantrek8




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