Is it cold in Hanzhong in winter? What are the climatic characteristics of Hanzhong?

Hanzhong is a good tourist city. In spring, you can enjoy all kinds of beautiful mountains and rivers, and in winter, you can play, ski, play and enjoy the snow, so that tourists can enjoy themselves.

Is it cold in Hanzhong in winter? Winter in Hanzhong is not cold. The temperature is generally not lower than zero. Compared with the north of Qinling Mountains, it is unusually warm here. But because Hanzhong is at the southern foot of Qinling Mountains, there is no central heating, so northerners think Hanzhong is colder in winter.

Hanzhong belongs to the tropical climate zone of North Asia. There are two barriers, Qinling Mountain in the north and Daba Mountain in the south.

The geographical distribution of temperature in this area is mainly influenced by topography. The annual average temperature14 c is slightly lower in the west than in the east, and lower in the north and south mountains than in the flat dams and hills. Annual average temperature in Pingba area below 600 meters above sea level14.2 ~14.6℃; The annual average temperature in areas above 1000m is generally lower than12℃; The annual average temperature in Jiaqianling River Basin is higher than 65438 03℃.

? Climate characteristics of Hanzhong area Hanzhong area is located in the mid-latitude area of the northern hemisphere. The warm and humid air of perennial precipitation mainly comes from the Bay of Bengal in the Indian Ocean, followed by the western Pacific Ocean. In summer, under the influence of the subtropical high, the water vapor in the Bay of Bengal moves northward along the southwest monsoon at the lower part of the southwest vortex, passes through Tibet, Yunnan and northwest Sichuan, and reaches over this area. Water vapor from the western Pacific enters the region with the southeast airflow at the edge of subtropical high.

Winter is controlled by the polar continental cold air mass (mainly Mongolian high pressure), with more northwest monsoon and cold, dry and little rain. Spring and autumn are transitional seasons, with warm and little rain in spring, cool and rainy in autumn and humid climate. The water vapor evaporated from vegetation, reservoirs, rivers and pastoral areas rarely participates in precipitation.

The warm and humid airflow from the southwest and southeast is blocked by Bashan and Qinling Mountains, which makes the region abundant in rainfall. However, due to the fact that the two mountains are located on the southwest airflow path, the water vapor system in the middle and lower layers converges, and the topographic uplift and the vertical influence of mountains make the water vapor in the north and south of the water area different, and the precipitation distribution is very different. The average annual precipitation is between 700- 1700mm, of which Micang Mountain in the south is the most abundant and the highest in Shaanxi.