Is there still snow in Yulong Snow Mountain?

In July, there was snow in Yulong Snow Mountain, but there was not much snow, only a little on the top of the mountain. But if the weather is bad, tourists may not be able to see it even if they take the cableway. The whole Yulong Snow Mountain is surrounded by fog. Yulong Snow Mountain is a group of snow-capped mountains 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 north. It is located at1004' 2 "-10016' 30" east longitude and 27 3' 2 "~ 27" north latitude. It is the closest mountain range to the equator in the northern hemisphere, with snow all year round. It is adjacent to Zhongdian Snow Mountain in Jiangxi, and Mianmian Mountain is in the east. It starts from Sanjiangkou in the north and reaches 27 north latitude in the south, like a fan facing the ancient city. The whole mountain 13 peaks are vertically arranged from south to north, and the highest peak is 5596 meters above sea level, showing a steep fan shape. There is snow all year round, and the height of the snow line is between 4800 and 5000 meters. Asia and Europe have temperate marine glaciers closest to the equator. Climate Characteristics Yulong Mountain belongs to the monsoon climate zone of the southern temperate plateau, and has unique characteristics of mountain monsoon. Due to the large height difference between the valley and the peak, there are warm, warm, warm, cool north subtropical zone, cold warm zone and other mountain vertical climatic zones from the valley to the peak. Yulong mountain area is located on the southeast edge of Qinghai-Tibet Plateau, which is controlled by westerly circulation, southwest monsoon and southeast monsoon alternately. The climate in this area is clearly divided into dry season and rainy season. The dry season is 1 1 to April of the following year, which 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 rainy 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 5438 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 jet weakened, and the hot and humid southwest monsoon entered the area northward, and the rainy season began. /0eb 30 f 2442 a 7d 933 f 05 a 70 12 BD 4d 1 1372 f 00 1 E4？ x-BCE-process = image % 2f resize % 2Cm _ lfit % 2Cw _ 600% 2Ch _ 800% 2c limit _ 1% 2f quality % 2Cq _ 85% 2f format % 2Cf _ auto