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The displacement of the latter follows the north-south movement of the sun and its relative position form the earth, in particular from the continents of Asia and Australia, at certain periods of the year.
These factors contribute to the displacement and instensity of the Inter-Tropical Convergence Zone ITCZ which is an equatorial trough of low pressure that produces rain. Thus, the west and east monsoons, or the rainy and dry seasons, are a prevalent feature of the tropical climate. The Main Seasons The climate changes every six months.
The dry season June to September is influenced by the Australian continental air masses; while the rainy season December to March is the result of the Asian and Pacific Ocean air masses. The air contains vapor which precipitates and produces rain in the country. Tropical areas have rains almost the whole year through. However, the climate of Central Maluku is an exception. The rainy season is from June to September and the dry season from December to March. The transitional periods between the two seasons are April to May and October to November.
Temperature and Humidity Due to the large number of islands and mountains in the country, average temperatures may be classified as follows:. Mountains higher than 9, feet are found on the islands of Sumatra Mt. Leuser and Mt. Kerinci , Java Mt. Gede, Mt. Tangkubanperahu, Mt. Ciremai, Mt. Kawi, Mt. Kelud, Mt. Semeru and Mt. Raung , Sulawesi Mt. Lompobatang and Mt. Rantekombala , Bali Mt. Batur and Mt. Agung , Lombok Mt. Rinjani and Sumbawa Mt. The highest mountain is the perpetually snow-capped Mandala Top 15, feet in the Jaya Wijaya mountain range of Irian Jaya.
