Humid Subtropical Climate
Template:Short description Template:Climate classification Humid subtropical climate is a type of climate characterized by hot, humid summers and generally mild to cool winters. This climate typically lies on the east coast of continents between latitudes 20° and 40° north and south of the equator.
Characteristics[edit | edit source]
Humid subtropical climates are noted for high temperatures in summer, with humidity levels that can make it feel even hotter. During winter, temperatures are cooler but generally mild compared to other climate types, with rare occurrences of frost or snow in many regions. Rainfall is typically distributed throughout the year, often with a peak in the summer months due to thunderstorms and tropical weather patterns.
Köppen classification[edit | edit source]
In the Köppen climate classification system, the humid subtropical climate is categorized as Cfa or Cwa:
- Cfa: Humid subtropical climates with hot summers and no significant dry season.
- Cwa: Humid subtropical climates with hot summers and a noticeable dry winter season.
Geographic distribution[edit | edit source]
Humid subtropical climates are found in many parts of the world, including the southeastern United States, southeastern South America, southern China, South Korea, Japan, and eastern Australia. The climate is also found in coastal regions of India, particularly in West Bengal, Assam, and parts of the Northeast.
Vegetation and wildlife[edit | edit source]
Humid subtropical climates support diverse vegetation, including evergreen forests, deciduous trees, and grasslands. Due to the high humidity and mild winter temperatures, these regions are often rich in flora and fauna. Agriculture is also prominent, with many humid subtropical areas growing crops such as rice, cotton, and tobacco.