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Prevailing wind patterns interact with local topographic conditions to produce significant variations in rainfall throughout the archipelago. In general, western and northern parts of Indonesia experience the most precipitation, since the north- and westward-moving monsoon clouds are heavy with moisture by the time they reach these more distant regions.
Indonesian Institute of Sciences building in Jakarta. Among the main research and development institutions in the country, are: The Ministry of Education, Culture, Research and Technology (Indonesian: Kementerian Pendidikan, Kebudayaan, Riset dan Teknologi Republik Indonesia, or Kemendikbudristek), is a government ministry that has the task of conducting affairs in the field of research ...
These areas usually see some snowfall during the winter, though snowfall is much lower than at locations at similar latitudes with more humid climates. [ citation needed ] Areas featuring cold semi-arid climates tend to have higher elevations than areas with hot semi-arid climates, and tend to feature major temperature swings between day and ...
Mangga Dua is a shopping district at Pademangan subdistrict of North Jakarta, in Indonesia The area is bordered by Jalan Gajah Mada in the west and Jalan Gunung Sahari in the east, while in the middle is Jalan Pangeran Jayakarta and Jalan Mangga Dua Raya.
Nuclear winter is a severe and prolonged global climatic cooling effect that is hypothesized [1] [2] to occur after widespread firestorms following a large-scale nuclear war. [3] The hypothesis is based on the fact that such fires can inject soot into the stratosphere, where it can block some direct sunlight from reaching the surface of the Earth.
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A cold front is the leading edge of a cooler mass of air at ground level that replaces a warmer mass of air and lies within a pronounced surface trough of low pressure.It often forms behind an extratropical cyclone (to the west in the Northern Hemisphere, to the east in the Southern), at the leading edge of its cold air advection pattern—known as the cyclone's dry "conveyor belt" flow.