Draft:Subtropical monsoon climate

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Last edited by Uness232 (talk | contribs) 19 days ago. (Update)

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Also known as Subtropical desiccation winter climate Cw: Dry-winter subtropical， a: hottestThe month Average temperature Above 22℃.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)

References[edit]

^ "Pure tabular statistics". ArcGIS Experience Builder. China Meteorological Data Service Center. Retrieved 2 August 2023.

[1] "Pure tabular statistics". ArcGIS Experience Builder. China Meteorological Data Service Center. Retrieved 2 August 2023.

[1]