What is the Mediterranean climate, temperate monsoon climate, temperate maritime climate and tropical monsoon climate?

The Mediterranean climate is controlled by subtropical high and prevailing westerlies. Summer is hot and dry, and winter is mild and rainy. Mainly distributed in the western mainland, such as the Mediterranean region of Europe.

The temperate monsoon climate is due to the temperature difference between the land and the sea. In summer, the mainland temperature is high and the ocean temperature is low, so the mainland forms a low-pressure ocean and forms a high pressure. In summer, the southeast wind blows from the ocean. On the contrary, the northwest wind blows from the mainland in winter, and the rain and heat are the same (high temperature and rainy in summer), and the winter is cold and dry. The North China Plain and the Northeast Plain in China belong to the temperate monsoon climate zone.

The temperate maritime climate is influenced by a single warm current all the year round, with more precipitation throughout the year, which is not too cold in winter and too hot in summer. Very uniform, Europe is a typical temperate maritime climate zone.

The tropical monsoon climate is influenced by the great difference of ocean thermodynamics and the movement of seasonal pressure zone. When the northern hemisphere welcomes winter, the pressure belt moves south, and the tropical monsoon climate zone will be affected by the northeast trade wind. When the northern hemisphere welcomes summer, the pressure belt moves northward, and this area will be affected by the southwest monsoon of the Indian Ocean. Therefore, the dry season and rainy season of tropical monsoon climate are very obvious. The South Asian subcontinent and Indian zhina Peninsula are typical tropical monsoon climate zones.