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The habagat season is characterized by hot and humid weather, frequent heavy rainfall, and a prevailing wind from the western parts. The main indicator of the switch between the amihan and habagat seasonal patterns is the switch in wind direction. In most years this transition is abrupt and occurs overnight.
Amihan is a genderless deity that is depicted as a bird in the Philippine mythology. According to the Tagalog folklore, Amihan is the first creature to inhabit the universe, along with the gods called Bathala and Aman Sinaya. In the legend, Amihan is described as a bird who saved the first human beings, Malakas and Maganda, from a bamboo plant.
Buran (a wind which blows across eastern Asia. It is also known as Purga when over the tundra); Karakaze (strong cold mountain wind from Gunma Prefecture in Japan); East Asian Monsoon, known in China and Taiwan as meiyu (梅雨), in Korea as jangma (), and in Japan as tsuyu (梅雨) when advancing northwards in the spring and shurin (秋霖) when retreating southwards in autumn.
Monsoons are large-scale sea breezes which occur when the temperature on land is significantly warmer or cooler than the temperature of the ocean. Most summer monsoons or southwest monsoons (Filipino: Habagat) have a dominant westerly component and a strong tendency to ascend and produce copious amounts of rain (because of the condensation of water vapor in the rising air).
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The Habagat season is characterized by hot and humid weather, frequent heavy rainfall, and a prevailing wind from the west. [67] On Boracay, the main indicator of the switch between the Amihan and Habagat seasonal patterns is the switch in wind direction. In most years this transition is abrupt and occurs overnight.
The southwest monsoon (from May to October) is known as the Habagat, and the dry winds of the northeast monsoon (from November to April), the Amihan. Temperatures usually range from 21 °C (70 °F) to 32 °C (90 °F) although it can get cooler or hotter depending on the season.
A monsoon (/ m ɒ n ˈ s uː n /) is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation [1] but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with annual latitudinal oscillation of the Intertropical Convergence Zone (ITCZ) between its limits to the north and south of the equator.