Dinamika Siklon Tropis di Asia Tenggara Menggunakan Data Penginderaan Jauh  

Oleh:

Zubaidah, Any ; Haryani, Nanik Suryo

Jenis: Article from Journal - ilmiah nasional - tidak terakreditasi DIKTI
Dalam koleksi: Widya: Majalah Ilmiah vol. 27 no. 324 (Oct. 2012), page 54-58.
Topik: Siklon Tropis; Penginderaan Jauh
Fulltext: 54-58-Bernard.pdf (3.5MB)

Isi artikel

Tropical cyclone is the form of extreme weather disturb. The growth of tropical cyclone is originated by tropical depression or the center of an intensive low pressure above the ocean, triggering convection process and the intensive forming of cloud. The aim of the research is to obtain the information of the extreme weather condition in the form of tropical depression and tropical cyclones particularly the movement location of tropical cyclones and the influence coverage area in Indonesia. This method used observation and analyzing the impact of tropical cyclones in Indonesia area, and mapping its position based on latitude and longitude of cyclone Centrum. The result of tropical cyclone monitoring in 2010 shows that tropical cyclone in Southern Indonesian area or Indian Ocean lasted in January, part of March and December 2010. Meanwhile, the tropical cyclone in Northern Indonesian area on South China Sea and West Pacific was lasted in April , May, July, August, September, October, November and part of March 2010. Tropical cyclone on March 2010 did not show an orderly pattern. On May 2010, the tropical cyclones are simultaneously happen in the northern and southern of Indonesia. In 2010 the concentration of tropical cyclone is heavily taken place in northern part of Indonesia.

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