Traditional Culture Encyclopedia - Travel guide - What is the altitude of Yulong Snow Mountain in Yunnan?

What is the altitude of Yulong Snow Mountain in Yunnan?

Yulong Snow Mountain in Yunnan is 5596 meters above sea level.

Longxueshan is located in Lijiang City, Yunnan Province, with Li (Jiang)-Ming Highway in the east, Tiger Leaping Gorge in the west, Yuhu Lake in the south and Tiger Leaping Gorge in the big giant gorge in the north. It is located at1004' 2 "-10016' 30 east longitude and 27 3 north latitude.

Yulong Snow Mountain is a group of snow-capped mountains in Lijiang City, Yunnan Province. It is about 0/5 km north of Lijiang, with a total length of 75 km. It is the closest equatorial snow mountain in the northern hemisphere, juxtaposed with Zhongdian Snow Mountain across Jiangxi and Mianmian Mountain in the east, starting from Sanjiangkou in the north and 27 north latitude in the south, just like a fan facing the ancient city.

The plants in Yulong Snow Mountain area are distributed from low altitude to high altitude, including warm valley shrubs, wet evergreen broad-leaved forests in mountainous areas, deciduous broad-leaved forests in mountainous areas, warm coniferous forests, hard-leaved oak forests in mountainous areas, cold coniferous forests, cold temperate shrubs, sparse meadows in alpine riparian beaches and so on.

Yulong Snow Mountain area is located in the southeast edge of Qinghai-Tibet Plateau, which is controlled by westerly circulation, southwest monsoon and southeast monsoon alternately, and the climate in this area is obviously different between dry and wet seasons.

The dry season 165438+ 10 to April of the following year is mainly controlled by the south branch of the westerly circulation and the winter wind on the Qinghai-Tibet Plateau, with little rain. May-10 is the wet season, which is mainly controlled by the southwest and southeast monsoon, and the precipitation accounts for more than 90% of the annual precipitation. From June 65438 to March of the following year, it was mainly controlled by the jet stream of the south branch of the upper westerly circulation, with less precipitation and less glacier recharge; In April, the south branch jet weakened, and the hot and humid southwest monsoon entered the area northward, and the wet season began.