Banjarnegara is a town in Central Java , Indonesia and the seat of Banjarnegara Regency . It is 55 km from the Dieng Plateau region and a centre for ceramic arts.
5-566: Banjarnegara has a tropical rainforest climate (Af) with moderate rainfall from June to September and heavy to very heavy rainfall from October to May. It is one of the wettest towns in Indonesia. 7°23′46″S 109°41′42.58″E / 7.39611°S 109.6951611°E / -7.39611; 109.6951611 This Central Java location article is a stub . You can help Misplaced Pages by expanding it . Tropical rainforest climate A tropical rainforest climate or equatorial climate
10-453: Is a tropical climate sub-type usually found within 10 to 15 degrees latitude of the equator . There are some other areas at higher latitudes, such as the coast of southeast Florida, United States, and Okinawa, Japan that fall into the tropical rainforest climate category. They experience high mean annual temperatures, small temperature ranges, and rain that falls throughout the year. Regions with this climate are typically designated Af by
15-480: Is high throughout the months. One day in a tropical rainforest climate can be very similar to the next, while the change in temperature between day and night may be larger than the average change in temperature during the year. When tropical rainforest climates are more dominated by the Intertropical Convergence Zone (ITCZ) than the trade winds (and with no or rare cyclones), so usually located near
20-454: The Köppen climate classification . A tropical rainforest climate is typically hot, very humid, and wet with no dry season . Tropical rainforests have a type of tropical climate (at least 18 C or 64.4 F in their coldest month) in which there is no dry season —all months have an average precipitation value of at least 60 mm (2.4 in). There are no distinct wet or dry seasons as rainfall
25-519: The equator, they are also called equatorial climates. Otherwise, when they are more dominated by the trade winds than the ITCZ, they are called tropical trade-wind climates. In pure equatorial climates, the atmospheric pressure is almost constantly low so the horizontal pressure gradient is low. Consequently, the winds are rare and usually weak (except sea and land breezes in coastal areas) while in tropical trade-wind climates, often located at higher latitudes than
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