Description

The huge Chinese territory is subject to different climates, mostlytemperate or subtropical. In the Northwest (Mongolia Region andXinjiang), summer is scorching (47 ° C) with violent thunderstormsand very cold winter (as low as -40 ° C) and very dry. On theTibetan Plateau and north-east, the sun is omnipresent throughoutthe year with cold winters and mild summers yet. On the coast is anoceanic climate prevails, while the South China is marked by asubtropical climate, mild and humid in winter, hot and rainy insummer. Huge differences in latitude, longitude and altitude canlead to sudden changes in temperature and precipitation in thecountry. Although most temperate countries are located such asChina, the climate model of the country is complex. Northern Chinais in the temperate zone, while the southern end has a tropicalclimate. Differences in temperature in winter are great, but thesedifferences are smaller in the summer. For example, northernHeilongjiang province can have an average below 0 ° C in January aslow as minus 30 ° C, while the average in July and in the samearea, can exceed 20 ° C . In contrast, central and southernGuangdong province may experience an average January temperatureabove 10 ° C, while the average in July is about 28 ° C.Precipitation can vary from one region to another, even fortemperatures. In southern China, with a subtropical climate, QinLing knows abundant precipitation, most of them come with thesummer monsoons. Spring is the best time to visit this region. Tothe north and west, however, rainfall is uncertain. Northwestern isthe low annual rainfall region in the country, sometimes with noprecipitation in these desert areas. The clear skies and dry air ofautumn make pleasant visits this season.