Xinjiang Tianshan inversion?

In the mountainous area of Tianshan Mountain, especially in the west of Tianshan Mountain, obvious inversion stratification often occurs in winter. /kloc-reversed in October and disappeared in April of the following year. In June 5438+ 10, the stratification was the largest, reaching about 3000 meters.

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The temperature in Tianshan Mountain is changeable, mainly depending on the altitude. The foothills are hot in summer: the average temperature in Fergana Valley in July can reach 27℃ (81℉); Yili basin can reach 23℃(73℉), and Turpan basin in the east can reach 34℃(93℉), which belongs to continental climate. At an altitude of about 3200m (10500ft) in the hinterland of Tianshan Mountain, the temperature drops to 5℃(4 1℉) in July, and there may be frost all summer. The average temperature in Fergana Valley was-4℃ (25 ℉) in June+10/October, 5438. The temperature in Yili basin is-10℃ (14 ℉); The temperature in the hinterland of Tianshan Mountain dropped to -23℃(-9℉), and the low temperature in some places (especially in the Aksai Valley) reached -50℃(-58℉).

Mountain climate is obviously divided into cold and warm seasons in the middle of the year. How sunny it is in the cold season. The mountains, basins and valleys below 3000 meters are covered with deep snow, foggy and frosty. In warm season (summer), it is rainy and snowy above 3000 meters above sea level. The climate is cool below 3000 meters. The difference of humidity in different places is controlled by altitude. In the mountainous area of Tianshan Mountain, especially in the west of Tianshan Mountain, obvious inversion stratification often occurs in winter. /kloc-reversed in October and disappeared in April of the following year. In June 5438+ 10, the stratification was the largest, reaching about 3000 meters.