Climate change is also felt in Thailand, because the monsoon largely determined the weather in Thailand a very important concept for monsoon ITCZ is (= Inter Tropical Convergence Zone or Inner Tropical Convergence Zone) The monsoon translated, Season, a yearly, large-scale circulation of air currents, which significantly changes the lives of the population in the affected parts of the world beeinflusst.Die direction of the monsoons is every six months. Formation of a monsoon can be explained simply and banal --- is much more complicated, but I still try to make explicable. There are over the Indian subcontinent, two types of monsoons: the summer and winter monsoon. summer monsoon The summer monsoon blows about in the months of July to October. It is caused by the fact that over the Indian Ocean, southwest of India, a high pressure area has developed as has developed north of the Himalayas of Nepal and Bhutan are a large low pressure area. The resulting summer monsoon is warm and rainy, blowing from the southwest. winter monsoon 
The winter monsoon blows approximately in the period from November to February. It is caused by the fact that China has over the edge of the Tibetan highlands, a cold high pressure in India and developed a deep equatorial heat. The resulting wind blows from the northeast, and is cold and dry. what is a monsoon? 
The monsoon is a two-tier system of wind. Sun is blowing in the summer months the wind constantly from one direction, in the winter months, but just as consistently accurate from the Gegenrichtung.Für Thailand, this means that blows during the winter months, a steady wind from the northeast of the country because the Chinese mainland is essentially the monsoon Climate Change in Southeast Asia determined. In the summer months the wind comes allegedly from the opposite direction, ie from the southwest. This means that the regions in central, northern and northeastern Thailand can only be gotten extensive rain, when the southwest monsoon coming from the Andaman Sea of the Indian Ocean, where he was charged with moisture kann.Der northeast monsoon, which in the November to April of China blows can arrive in the same regions therefore only dry as the land masses offer him no opportunity to recharge with moisture. 
In trade winds meant the easterly winds north and south of the ITCZ (Inter Tropical Convergence Zone or = Inner Tropical Convergence Zone). At the ITCZ increases to air and moves to more air. This aspirated air is deflected by the Coriolis force to the west. Therefore, these winds are easterly winds to. In the southern hemisphere the trade winds blow from the southeast, north-easterly direction to the northern hemisphere. Crossing the equator, these winds, so the trade winds are deflected to the other hemisphere to the east. The northeast trade wind is in the southern hemisphere to the north-west trade winds and the southeast trade winds to the southwest trade winds. The southwest summer monsoon determines the Passat in India. The Inter Tropical Convergence Zone (ITC) "(German: Inner Tropical Convergence Zone) is a zone around the equator, where strong convection upgrade (the heated Air masses takes place). reason for the strong convection warming by the sun. The ITCZ follows the vertical position of the sun with a delay of up to 4 weeks. The sun then developed their strongest heat effect, where it is at noon vertically from the ground. The ITCZ is limited by the trade wind zones of both hemispheres of the Tropic of Cancer 23.5 N and the Tropic of Capricorn 23.5 S in between the tropical zone. fall day in the ITCZ heavy rainfall (thunderstorms). continue leading sources and sources used are as follows http://www.agenda21-treffpunkt.de/lexikon/Klimawandelfolgen.htm http://klima-der-gerechtigkeit.de/archiv/bali-dossier/thailand/ http://www.weather.gov.sg/wip/web/ASMC/Regional_Weather/Monthl y_Weather_and_Haze_Outlook http://www.raonline.ch/pages/edu/cli2/monsun001.html --------------------------- should enlarge with --------------------------------------- video on climate here is one See really! ----------------------------------------------- -------------------
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