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Where is the climate and temperature in Germany similar to that in China?

Most parts of Germany belong to temperate maritime climate. According to latitude and longitude, German and China Heilongjiang belong to almost the same latitude, even to Russian territory, but the climate is quite different. The coastal cities of China, such as Tianjin, Qingdao and Shanghai, belong to temperate monsoon climate, which is quite different from temperate maritime climate. Therefore, there is no temperate maritime climate city not only in China, but also in Asia as a whole.

Germany is located in the warm and humid westerly belt, which belongs to the transitional climate between the maritime climate in western Europe and the continental climate in eastern Europe. Northwest China has a maritime climate, which is neither hot in summer nor cold in winter, making it more comfortable. The continental climate in the east and southeast is remarkable. In winter, Leng Xia is hot, with the lowest temperature reaching-10 degrees and the highest temperature exceeding 30 degrees.

Stable and mild climate is the general feature of Germany, and the temperature is relatively stable. The average temperature in winter is between 1.5 degrees (lowlands) and -6 degrees (mountains), and the average temperature in summer is about 18 degrees (plains) and 20 degrees (southern valleys). Usually April is the most unpredictable month of climate change in Germany, with rainstorm, hurricane and snow hail appearing alternately, so it is best to take rain gear when going out during this time; May, June, September, 65438+1October,165438+1October are good seasons for Germans to engage in various exchange activities, and various activities are generally arranged in these five months; July and August are the holiday season for Germans and the tourist season in Germany. In winter in Germany, the sun sets early and it rains and snows.

China is located in the southeast of Eurasia, the largest continent on earth. Due to the difference of physical properties between land and sea, especially the difference of thermal action, the Asian continent is the source of cold air in winter, forming a cold high pressure, and the cold air diverges from the mainland to the periphery; In summer, the land heats up rapidly, forming a hot low pressure, and warm and humid air blows from Zhou Haiyang to the center of the low pressure. This change in the prevailing wind direction, which is opposite in winter and summer, has brought about obvious seasonal changes in the climate, and this change has formed the monsoon climate in China.

The cold high pressure on the winter monsoon continent was formed in September, and its center is located in Mongolia. The cold and dry northwest or northeast monsoon blows, first reaching the north of China, and then rapidly advancing southward to the Jianghuai Basin and its south area. The winter wind intensifies month by month with the change of seasons, and it is strongest in 5438+1October and June. Every 7 ~ 10 days, cold air bursts southward, and the temperature in South China can be reduced by 12 ~ 16℃ for 24 hours, sometimes accompanied by moderate to heavy rain. Hainan Island can also cool down by more than 8℃. When cold air reaches the southern coastal areas, it often forms low clouds, accompanied by Mao Mao rain. When the winter wind is strong, it can blow to northern Australia, which is the southernmost limit of the winter wind. Cold and warm air in the northern and southern hemispheres is often mixed in this convergence zone or intertropical convergence zone. At this time, the winter wind blowing from the Asian continent meets the cool and humid airflow blowing from the western Pacific subtropical high, forming a north-south convergence line, and these convergence zones are rich in precipitation. Winter winds only prevail at low altitudes (below 3,000m). The average altitude of the Qinghai-Tibet Plateau in southwest China is above 4,000m, so it is difficult for cold air to cross the Qinghai-Tibet Plateau. Winter winds flow to the eastern part of China along the eastern side of the Plateau and its east. Cold air often goes south with the cold front, and the north is sunny and sunny, and slowly runs to Jianghuai and its south; The Yunnan-Guizhou Plateau often forms a stationary front, which shows a wide range of rainy weather.

In April and May of the summer monsoon, the Asian continent heats up rapidly, forming a thermal depression, the center of which is located in the western part of the Qinghai-Tibet Plateau. However, the warm and humid airflow dispersed by the Pacific subtropical high goes deep into the north and Hetao area from the southeast coast in the form of southeast or south monsoon, and its climate is characterized by hot and humid and thunderstorms.

There are three sources of summer monsoon affecting China: 1 The southwest monsoon originates in the South Indian Ocean, forms a low-level jet in the Arabian Sea, passes through the Indian Peninsula, and affects southwest and south China; The second southeast trade wind originated in northern Australia, crossed the equator, passed through Indonesia or Malay Peninsula, and merged with the 1 airflow in the northern hemisphere and the northeast trade wind to form the equatorial convergence zone. The third airflow comes from the subtropical high in the North Pacific, which is the southeast monsoon and the south monsoon that mainly affect the eastern part of China. They go deep into the northwest of northeast China and the north of Inner Mongolia, which is the northern boundary of China summer monsoon. When they meet the cold air from the northwest, they form a rainstorm belt, which brings abundant precipitation. This rainstorm zone is usually used to indicate the activity of summer monsoon. The advance and retreat of the East Asian summer monsoon have two sharp advances and one sharp retreat. Generally, summer monsoon prevails in South China in early May, which is the beginning of monsoon rainfall in South China. Prevalent in southwest China at the end of May or early June; In June, the midsummer monsoon suddenly prevailed in the Jianghuai Basin, which was the beginning of the rainy season in the Jianghuai Basin. In July, the midsummer monsoon jumps northward to North China and Northeast China again, which is the beginning of the rainy season in North China and the end of the meiyu period in Central China. Mid-to-late August is the peak of summer monsoon, when it advances to the northernmost and westernmost borders of China. Therefore, it takes about four months for summer monsoon activities to reach the northern part of North China from South China. Its retreat was a sudden change. Generally, the cold air in the north begins to strengthen in early September, that is, the winter wind begins to establish. It takes only 1 month for winter winds to reach South China or coastal areas from north to south. In another famous monsoon region, the advance and retreat speed of China summer monsoon is just the opposite to that of Indian monsoon. The arrival of Indian summer monsoon is explosive, and it only takes 1 month from south to north, while its retreat takes 4 ~ 5 months.