Tide wave. The water flow. Monsoon season is the khoikuan sea water flows will help reduce water deficiency and allows oxygen to water by. In the Gulf of Thailand is a semi-closed Bay. Waves and tides if there is insufficient circulation, especially in the rainy season. Fresh water flowing into the sea will bring down more than normal food, Tu phatha, including fresh water, sun-burnt, temperature rise, making fresh water floating on the surface of the water, press the water salty colder down. Which have a very already the phytoplankton into more depth in the water mass more Hypoxia hypoxia. Fish and smaller organisms that cannot escape has died. The more severe Hypoxia and hypoglycaemia is important Bioturbation processes of living organisms, oxygen facial area normal sludge sludge sludge which still face deep down to 10 cm when the sediment is stirred up by Bioturbation processes, oxygen is taken up m.Use the oxygen in the sediment, making lower down than the original. In doing so, to analyze the amount of oxygen in that part of the sea with the sludge. Furthermore, this phenomenon is also related to the typhoon, which is influenced by the Gulf of Thailand from two monsoon wind is southwest monsoon and North East monsoon winds. The southwest monsoon will begin approximately may through early October, to the eastern side of the Gulf of Thailand rows, e.g., Chonburi, Rayong, and North-East monsoons start approximately November through February is the West side of the Gulf of Thailand rows from Chumphon to Pattani. The typhoon caused this will cause the water in the Gulf of Thailand with the stumps of the turnover must be studied on both sides of the Gulf of Thailand on the seasonal.
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