During the dry season, the region experiences semi-desert conditions with much less rainfall. The desert region of South Asia is located east of the Caspian Sea and Northwest of the Himalayan Mountains; this region experiences warm to high temperatures and little rainfall. The desert region is home to cacti and similar plants that can tolerate the arid conditions. Central to South India experiences a Savanna climate; the temperatures are warm to high rising in summer months up to 50 degrees Celsius.
This region only experiences rainfall during the summer months. The Thai climate is controlled by tropical monsoons and the weather in Thailand is generally hot and humid across most of the country throughout most of the year. The weather in central, northern, and northeastern Thailand the landlocked provinces is determined by three seasons, whereas the southern, coastal regions of Thailand feature only two, making the weather in Thailand quite easy to understand and plan a trip around.
The other inland season, the rainy season, lasts from May to November and is dominated by the southwest monsoon, during which time rainfall in most of Thailand is at its heaviest. The southern, coastal region of Thailand really has only two seasons — rainy season and dry season.
The weather in Thailand around the central, northern, and northeastern regions is mostly cool and dry between November and February, consequently these are the most popular months to visit Thailand. The weather in Thailand classified as the hot season lasts from March to June when higher relative temperatures and occasional rain are the norm. Around the inland areas, including Bangkok and Ayutthaya, this often means punishing heat and high humidity.
The temperatures in the hot season begin climbing in February and by April the unrelenting heat makes many residents eager for the upcoming rains, which begin sporadically falling around mid-April. The season lasts from July to October and is dominated by the southwest monsoon, during which time rainfall in most of Thailand is at its heaviest.
Overall, the southern parts of Thailand, particularly the Andaman Coast, get the most rain: around 2, millimeters every year, compared with the central and northern regions of Thailand, both of which get around 1, millimeters.
The best travelling period is in the dry season between May and September. The sun shines 12 hours per day, as Sumatra lis situated around the equator.
The raining season on Java is from October till March, but it is possible to go to Java all year around. Only in the wet season is the chance of rain bigger than at other times of the year. Bali has a similar climate to East Java and has therefore, apart from the mountainous regions, low rainfall during the dry season, which is from April to November. The best time to travel to Sulawesi depends on the area you wish to visit.
Sulawesi lies on the separation line between the monsoons; the Southern part of the island has the opposite season of the Northern-east part. Rainy season is from October till March. The temperature on Sulawesi is between the 25 and 34 degrees. The sun shines 12 hours per day, because Sulawesi lies on the equator.
In the mountains in the middle of Sulawesi it is possible to have rain during the summer months. The mountains catch the clouds and you will often have rain in the late afternoon for one or two hours.
The Northern part of Sulawesi has its wettest season during the summer months. The coastal areas have oppressive heat the whole year around — only a little sea breeze will cool you down.
In the mountains it is more pleasant and in the evening it can be very cold. Xie, P. Global precipitation: a year monthly analysis based on gauge observations, satellite estimates and numerical model outputs. Bulletin of the American Meteorological Society , 78 : — Yanai, M. Seasonal heating of the Tibetan Plateau and its effects on the evolution of the Asian summer monsoon. Ye, D. Yeh, T. Science Press: Beijing in Chinese.
The abrupt change of circulation over the northern hemisphere during June and October. The Atmosphere and the Sea in Motion. New York: Rockefeller Institute, pp. Cross-references 1. Asia, Climate of Southwest Google Scholar. Climate Classification Google Scholar. Intertropical Convergence Zone Google Scholar. Monsoons and Monsoon Climate Google Scholar. Tropical and Equatorial Climates Google Scholar.
Yanai There are no affiliations available. Parts of the Mongolian Plateau make up the semiarid zones of the region. The vegetation of semiarid zones consists mainly of short grasses, which provide food for grazing animals and livestock.
Most of the deserts in the region are found in the west central area of the mainland. The Gobi Desert is located in northern China and southeast Mongolia. The Gobi is a prime area for finding dinosaur fossils, since thousands of these animals roamed through the region millions of years ago. The tropical climate zone in East Asia is fairly small. It includes a small strip of land along China's southeastern coast, the island of Hainan , and the southern tip of Taiwan.
These areas have high temperatures, heavy rainfall, and high humidity every month of the year. The tropical rain forest in these places is made up of tall dense forests of broadleaf trees. In the next section, you will read how human-environment interactions affect the quality of life in rural China and urban Japan.
Asia » Climat » Vegetation geography ». East Asia: Landforms and Resources.
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