Anti-cyclone weather in China

The answer is D. The anticyclone (high pressure) that can control most parts of China refers to the Asian high (also known as Mongolia-Siberia high), that is, the winter half year in the northern hemisphere. Because Eurasia is the largest continent in the world, the thermal properties of land and ocean are significantly different from those of the largest ocean Pacific in the world. The Eurasian continent is colder, forming a strong cold high, the center of which is located in Mongolia-Siberia, and the Asian high can control most parts of China. Since it is winter, it is of course cold weather.

About Option A: The dry weather in summer occurs in July and August every year. Although the dry weather in summer is formed under the control of the western Pacific subtropical high (which belongs to anticyclone), the location is limited to the middle and lower reaches of the Yangtze River, so option A is wrong.

Option B: Meiyu weather occurs from mid-June to mid-July every year and is formed under the control of quasi-static front. The rainy weather has nothing to do with anticyclone (bringing sunny weather). And the location is limited to the plain in the middle and lower reaches of the Yangtze River, so option B is wrong.

About option C: Typhoon appears in summer and autumn every year, which is a tropical cyclone (low pressure) with strong development and has nothing to do with anticyclone (bringing sunny weather). Moreover, the geographical location is limited to the southeast coastal areas of China, so option C is wrong.