Gidan shakatawa na Ujung Kulon, BantenRinca, Ƙananan Tsibirin SundaGidan shakatawa na Danau Sentarum, Yammacin KalimantanTaron Dutsen RinjaniGili Meno Beach, Lombo
Yanayi na Indonesia kusan gaba ɗaya ne na wurare masu zafi. Ruwan da ke da zafi wanda ya kai kashi 81% na yanayin Indonesia ya tabbatar da cewa yanayin zafi a ƙasa ya kasance daidai, tare da filayen bakin teku da ke da matsakaicin 28°C (82°F) ° C (82 ° F), yankunan ciki da tsaunuka da ke da Matsakaicin 26°C (79°F) ° C (79 ° F), da yankunan tsaunuka mafi girma, 23°C (73°F) ° C (73 ° F). Yanayin zafi ya bambanta kadan daga kakar zuwa kakar, kuma Indonesia tana fuskantar ɗan canji kaɗan a cikin tsawon sa'o'in hasken rana daga kakar wasa ɗaya zuwa na gaba; bambancin tsakanin rana mafi tsawo da rana mafi ƙanƙanta a shekara minti arba'in da takwas ne kawai. Wannan yana ba da damar shuka amfanin gona a duk shekara.[1]
Babban canji na yanayin Indonesia ba zafin jiki ko matsin iska ba ne, amma ruwan sama. Yanayin zafi na yankin yana tsakanin 70 zuwa 90%. Iska tana da matsakaici kuma gabaɗaya ana iya hangowa, tare da ruwan sama yawanci yana hurawa daga kudu da gabas a watan Yuni zuwa Satumba kuma daga arewa maso yamma a watan Disamba zuwa Maris. Typhoons da manyan hadari suna haifar da ƙananan haɗari ga masu jirgin ruwa a cikin ruwan Indonesiya; babban haɗari ya fito ne daga saurin ruwa a cikin tashoshi, kamar Lombok da Sape.
Indonesia tana fuskantar yanayi da yawa, galibi gandun daji na wurare masu zafi (mafi girman ruwan sama), sannan kuma ruwan sama na wurare masu wurare masu zafi da savanna na wurare masu sanyi (mafi ƙarancin ruwan sama). [lower-alpha 1] Koyaya, Yanayin yanayi na teku da yanayin tsaunuka masu zafi ana samun su a yankuna masu tsawo a Indonesia, galibi tsakanin mita 1,500 da 3,500 (4,900 da 11,500 sama da matakin teku. Yankunan da ke sama da wannan matakin (yawanci a cikin tsaunuka na Papuan) sun fada cikin Yanayin yanayi na tundra da kuma yankin teku na subpolar.[2]
Bambance-bambance a cikin ruwan sama yana da alaƙa da Ruwan sama na Australiya da Indonesia. Gabaɗaya, akwai lokacin bushewa (Afrilu zuwa Satumba), wanda tasirin iska na Australiya ya rinjayi, da kuma lokacin ruwan sama (Oktoba zuwa Maris) wanda Asiya da Pacific Ocean suka haifar. Tsarin iska na gida, duk da haka, na iya canza waɗannan tsarin iska gaba ɗaya, musamman a tsibirin tsakiyar Maluku - Seram, Ambon, da Buru. Wannan tsarin shekara-shekara na iska da ruwan sama yana da alaƙa da wurin ƙasa na Indonesia a matsayin isthmus tsakanin manyan nahiyoyi biyu. A watan Satumba da Mayu, matsin lamba a kan hamadar Gobi yana motsa iskõki daga wannan nahiyar zuwa arewa maso yamma. Yayin da iskõki suka isa ma'auni, juyawa na Duniya yana sa su karkatar da hanyarsu ta asali a arewa maso gabas zuwa yankin kudu maso gabashin Asiya. A cikin Janairu da Fabrairu, tsarin matsin lamba mai dacewa a kan Asiya yana haifar da tsarin juyawa. Sakamakon shi ne ruwan sama wanda aka kara da iska mai laushi daga Tekun Indiya, yana samar da ruwan sama mai yawa a sassa da yawa na Malay Archipelago. Dubi kuma kwandon ruwan sama.
Hanyoyin iska da ke ci gaba da yin mu'amala da yanayin yanayi na gida don samar da sauye-sauye a cikin ruwan sama a ko'ina cikin tsibiran. Gabaɗaya, yankunan yammaci da arewacin Indonesiya sun fi samun hazo, tunda gajimaren damina da ke tafiya arewa da yamma suna da ɗanshi a lokacin da suka isa waɗannan yankuna masu nisa. Sumatra ta Yamma, Java, Bali, da ke cikin Kalimantan, Sulawesi, da Papua sune yankunan da ake hasashen dassuka na Indonesia, tare da auna ruwan sama sama da milimita 2,000 (78.7 in) a kowace shekara. A wani bangare, wannan danshi ya samo asali ne daga kololuwar tsaunin da ke damun iska. Birnin Bogor, kusa da Jakarta, ya yi iƙirarin samun mafi yawan adadin ranakun tsawa a duniya a kowace shekara—322. A gefe guda kuma, tsibiran da suka fi kusa da Ostiraliya—ciki har da Nusa Tenggara da ƙwanƙolin gabas na Java—suna iya zama bushe, tare da wasu wuraren da ke fuskantar ƙasa da milimita 1,000 (39.4 in) a kowace shekara. Don dagula lamarin, wasu tsibiran na kudancin Malukus suna fuskantar yanayin ruwan sama da ba a iya faɗi ba, ya danganta da iskar gida..
Ko da yake yanayin zafin iska yana canzawa kaɗan daga yanayi zuwa yanayi ko daga wannan yanki zuwa na gaba, yanayin sanyi yana yin rinjaye a mafi girma. Gabaɗaya, yanayin zafi yana faɗuwa kusan 1 ° C a kowace mita 90 a tsayi daga matakin teku tare da wasu yankuna masu tsayin tsayi na ciki suna fuskantar sanyin dare. Tsawon tsaunuka mafi tsayi a Papua suna cike da dusar ƙanƙara ta dindindin..
↑The tropical monsoon climate predominantly lies along Java's coastal north, Sulawesi's coastal south and east, and Bali, while the tropical savanna climate lies in isolated parts of Central Java, lowland East Java, coastal southern Papua and smaller islands to the east of Lombok.
