Draft:Subtropical monsoon climate
Also known as Subtropical desiccation winter Cw: Dry-winter subtropical Cwa is a monsoonal influenced version of the humid subtropical climate, having the classic dry winter–wet summer pattern associated with tropical monsoonal climates. They are found at similar latitudes as the Cfa climates, except in regions where monsoons are more prevalent. These regions are in the Southern Cone of South America, the Gangetic Plain of South Asia, southeastern Africa, and parts of East Asia and Mexico.
Examples
- Antananarivo, Madagascar (Cwa, bordering on Cwb)
- Busan, South Korea (Cwa)
- Chengdu, Sichuan, China (Cwa)
- Córdoba, Argentina (Cwa)
- Delhi, India (Cwa, bordering on BSh)
- Guadalajara, Jalisco, Mexico (Cwa)
- Guangzhou, Guangdong, China (Cwa)[1]
- Guwahati, India (Cwa)
- Hanoi, Vietnam (Cwa)
- Hong Kong (Cwa)
- Islamabad, Pakistan (Cwa)
- Kathmandu, Nepal (Cwa)
- Lilongwe, Malawi (Cwa)
- Lubumbashi, Democratic Republic of Congo (Cwa)
- Lucknow, Uttar Pradesh, India (Cwa)
- Lusaka, Zambia (Cwa)
- Macau (Cwa)
- Mackay, Queensland, Australia (Cwa)
- Pretoria, Gauteng, South Africa (Cwa)
- Rangpur, Bangladesh (Cwa)
- Sialkot, Pakistan (Cwa)
- Siguatepeque, Honduras (Cwa)
- Taunggyi, Myanmar (Cwa)
- Tucumán, Argentina (Cwa)
- Yeosu, South Korea (Cwa)
- Zapopan, Mexico (Cwa)
- Zhengzhou, Henan, China (Cwa)
- ^ "Pure tabular statistics". ArcGIS Experience Builder. China Meteorological Data Service Center. Retrieved 2 August 2023.