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Floods in Thailand are regular natural disasters in Thailand which happen nearly every year during the monsoon season. The monsoon seasons in the country are distinct by region, the southern part mirrors the Malay Peninsula and monsoon begins in October and ends in March. The rest of the nation has monsoons and/or frequent thundershowers from ...
Monk at Vassa. Vassa (Pali: vassa-, Sanskrit: varṣa-, both "rain") is the three-month annual retreat observed by Theravada Buddhists. Taking place during the wet season, Vassa lasts for three lunar months, usually from July (the Burmese month of Waso, ဝါဆို) to October (the Burmese month of Thadingyut, သီတင်းကျွတ်).
A travellers’ guide to the Thai weather seasons from north to south
A hot season runs from mid-February to May. The rainy season is from mid-May to October, the rainiest month. The annual average rainfall is 1,350 millimetres (53 in) with average humidity of 71 percent and 104 rain days. Highest average wind speeds are observed in December with 3.73 knots (6.9 km/h). [5]
The rainy season begins with the arrival of the southwest monsoon around mid-May. September is the wettest month, with an average rainfall of 335.9 millimetres (13.22 in). The rainy season lasts until October, when the dry and cool northeast monsoon takes over until February. The hot season is generally dry, but also sees occasional summer ...
Tropical monsoon climates have monthly mean temperatures above 18 °C (64 °F) in every month of the year and a dry season. [ 1 ] : 200–1 The tropical monsoon climate is the intermediate climate between the wet Af (or tropical rainforest climate ) and the drier Aw (or tropical savanna climate ).
Detailed map of Thailand. Thailand is in the middle of mainland Southeast Asia. It has a total size of 513,120 km 2 (198,120 sq mi) which is the 50th largest in the world. The land border is 4,863 km (3,022 mi) long with Myanmar, Cambodia, Laos and Malaysia. The nation's axial position influenced many aspects of Thailand's society and culture. [1]
The rainy season occurs from September to February and it is a major source of energy for the Hadley circulation during boreal winter. It is associated with the development of the Siberian High and the movement of the heating maxima from the Northern Hemisphere to the Southern Hemisphere.