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在副热带气候带内由于大洋上副热带高压东西侧的不同影响,因而在大陆东、西岸及内陆形成了不同类型的副热带气候。东岸是季风气候和副热带潮湿气候,西岸是副热带夏干气候,介于东西岸之间的中部则是副热带干燥气候。 地中海式气候是副热带西岸型气候,也即副热带夏干气候,它是所有气候类型中占有陆地面积最小的类型(约占1.7％),大约位于南北纬度30°—40°之间的地带,包括地中海沿岸、北美加利福尼亚沿岸、南美智利中部海岸、南非南端以及澳大利亚南缘和西南沿岸(见附图)。地中海式气候处于热带半干旱气候与温带海洋性气候间的过渡地带,它的气候主要特征表现为:
In the subtropical climatic zone, due to the different impacts on the east and west sides of the subtropical high in the ocean, different types of subtropical climates are formed in the east, west and inland areas of the mainland. The east coast is a monsoon climate and a subtropical humid climate. The West Bank is a subtropical summer dry climate, while the middle between the east and west coasts is a subtropical dry climate. The Mediterranean climate is a subtropical West Coast climate, ie, the subtropical summer climate, which is the smallest of all climate types (about 1.7% of the total land area), about 30 ° -40 ° north-south latitude, including The Mediterranean coast of North America, the coast of Central America in South America and Chile, the southern end of South Africa, and the south and southwestern coasts of Australia (see photo). Mediterranean climate in tropical semi-arid climate and temperate climate of the transitional zone between the climate, its main features are as follows: