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The major influences on Thailand's climate are its location in the tropical monsoon zone of mainland Southeast Asia and certain topographic features that affect the distribution of precipitation.
In the monsoon zone, surface circulation reverses every half year and features two opposing gyres (i.e., semi-closed current systems exhibiting spiral motion) that are separated by the Indian subcontinent.
In this study, the temporal trends and magnitudes of key climatic variables and the accompanying effects on ET0 during 1956 2015 were evaluated at 200 meteorological stations across the temperate continental zone (TCZ), temperate monsoon zone (TMZ), mountain plateau zone (MPZ), and subtropical monsoon zone (SMZ) of China.
This study conducted a national-scale assessment of different models for pan evaporation (Epan) estimation at 178 meteorological stations across different climatic zones of China, including the temperate continental zone (TCZ), temperate monsoon zone (TMZ), mountain plateau zone (MPZ) and subtropical monsoon zone (SMZ).
Generally, it can be divided into three climate zones, including the monsoon zone, the arid zone, and the highland zone.
Each zone can be further divided into several regions, such as the tropical, subtropical, and midlatitude monsoon regions within the monsoon zone.
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Where they extend into regions of seasonal rainfall, such as monsoon zones, they become less truly evergreen, holding many trees that stand leafless during the short dry seasons.
The Gushan River catchment is located in the Eastern-Asia Monsoon climate zone, which is generally arid to semi-arid.
The Gushan River catchment is in the East Asia Monsoon climate zone and is characterized by low precipitation and high potential evaporation.
2. Meteorology and hydrology Situated in the subtropical humid monsoon climate zone, Zunyi shows an annual mean precipitation of 1167.3 mm.
It belongs to the plateau type of the tropical monsoon climate zone, with cool summers and warm winters, and a mean annual temperature of 16 °C.
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