Yanayin yankin Curaçao

Yanayin yankin Curaçao
	geography of geographic location (en)
Bayanai
Fuskar	Curacao
Ƙasa	Curacao
Wuri
	12°11′N 68°59′W / 12.18°N 68.98°W

Curaçao, da sauran tsibirai na ABC da Trinidad da Tobago, suna kan iyakar nahiyar Amurka ta Kudu. Yana da tsibiri mai laushi tare da yanayin tuddai gabaɗaya; mafi girman batu shine Christoffelberg 372 metres (1,220 ft) a arewa maso yamma.^[1] Bayanan bakin teku, hanyoyin shiga da maɓuɓɓugar ruwa masu zafi suna ba da tushen ma'adanai na halitta, yanayin zafi, da ruwan teku da aka yi amfani da shi a cikin hydrotherapy da mesotherapy, yana mai da tsibirin ɗaya daga cikin yankuna masu yawa a yankin. A gefen kudu maso gabas akwai karamin tsibirin Klein Curaçao.^[2]

Tsire-tsire

Furen Curacao ya bambanta da tsibiran tsibiri na wurare masu zafi. Guajira-Barranquilla xeric scrub shine mafi shahara, tare da nau'ikan cacti iri-iri, ciyayi masu ƙaya, tsire-tsire, da bishiyar watapana (Libidibia coriaria; wanda ake kira divi-divi akan Aruba), waɗanda sune halayen tsibiran ABC da alamar ƙasa ta Aruba. Brassavola nodosa wani nau'in jure fari ne na Brassavola, ɗaya daga cikin 'yan orchids da ke cikin tsibiran ABC. Cacti sun haɗa da Melocactus da nau'in Opuntia kamar Opuntia stricta.

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Yanayi

Curaçao yana da yanayi mai zafi, mai raɗaɗi (Köppen yanayin yanayi na BS) tare da lokacin rani daga Janairu zuwa Satumba da lokacin rigar daga Oktoba zuwa Disamba. Ruwan sama ya yi karanci, kawai milimita 450 (inci 18) a kowace shekara; musamman lokacin damina ya fi bushewa fiye da yadda ake yi a yanayin zafi; a lokacin rani, kusan ba ya yin ruwan sama. Sakamakon karancin ruwan sama, yanayin Curaçao yana da bushewa; musamman a arewacin gabar tekun tsibirin. Yanayin zafi yana da ɗanɗano kaɗan, tare da ƙananan bambance-bambancen da aka auna a cikin shekara. Iskar cinikin tana sanyaya tsibirin da rana kuma tana dumi da dare. Watan mafi sanyi shine Janairu tare da matsakaicin zafin jiki na 26.6 °C (80 °F); mafi zafi shine Satumba tare da matsakaicin zafin jiki na 29.1 °C (84 °F). Matsakaicin matsakaicin matsakaicin zafin shekara shine 31.4 °C (89 °F). Matsakaicin zafin jiki na shekara shine 25.7 °C (78 °F). Ruwan ruwan tekun da ke kusa da Curacao yana kusan 27 °C (81 °F) kuma yana da sanyi (matsayin 25.9 °C (78.6 °F)) daga Fabrairu zuwa Maris, kuma mafi zafi (mafi 28.2 °C (82.8 °F)) daga Satumba zuwa Oktoba.

Saboda Curaçao yana arewacin yankin Intertropical Convergence Zone kuma a cikin wani yanki na ƙananan bambance-bambance inda iskõki ke gudana a layi daya zuwa gabar teku, yanayin sa ya bushe sosai fiye da yadda ake tsammani ga gefen arewa maso gabashin nahiyar a latitude. Ruwan sama kuma yana da matukar bambanci daga shekara zuwa shekara, yana da alaƙa da El Niño Southern Oscillation. Kadan kamar 200 millimeters ko 8 inci na iya faɗuwa a cikin shekara mai ƙarfi ta El Niño, amma kusan 1,150 millimeters o 45 inci ba a sani ba a cikin shekaru masu ƙarfi na La Niña.

Curaçao tana waje da Babban Yankin Ci Gaban Guguwa na Tropical na Atlantic, amma har yanzu suna shafar su a wasu lokuta, Kaisar yadda Guguwar Hazel a 1954, Anna a 1961, Felix a 2007, da Omar a 2008. Guguwar Hazel ta haifar da ambaliyar ruwa a Curaçao, ta lalata gada da madatsar ruwa da yawa. Ya haifar da asarar $ 350,000 (1954 USD). ^[3] Babu wata guguwa da ta sauka a Curaçao tun lokacin da Cibiyar Guguwa ta Amurka ta fara bin diddigin guguwa. Curaçao, duk da haka, guguwa ta shafi kai tsaye ta hanyar guguwa mai zafi sau da yawa; na baya-bayan nan shine Guguwar Tomas 2010, Cesar a cikin 1996, Joan a cikin 1988, Cora da Greta a cikin 1978, Edith da Irene a cikin 1971, da Francelia a cikin 1969. Tomas ya wuce Curaçao a matsayin guguwa mai zafi, ya sauka har zuwa 265 millimetres (10.4 in) in) na ruwan sama a tsibirin, kusan rabin ruwan sama na shekara-shekara a rana ɗaya.^[4] Wannan ya sanya Tomas daya daga cikin abubuwan da suka fi ruwan sama a tarihin tsibirin, da kuma daya daga cikin mafi muni; ambaliyar ta kashe mutane biyu kuma ta haifar da lalacewa sama da NAƒ50 miliyan (US $ 28 miliyan). ^[5]^[6]^[7]

Dangane da Emissions Database for Global Atmospheric Research, matsakaicin hayakin carbon dioxide ga kowane mutum a tsibirin ya kai tan 52 a cikin 2018, na biyu mafi girma a duniya.

Climate data for {{{location}}}
Watan	Janairu	Fabrairu	Maris	Afrilu	Mayu	Yuni	Yuli	Ogusta	Satumba	Oktoba	Nuwamba	Disamba	Shekara
^{[Ana bukatan hujja]}

Canjin yanayi

Matsakaicin yanayin zafi ya tashi sosai a cikin shekaru 40 da suka gabata a cikin Caribbean Netherlands kuma Curaçao ya sami kwanakin da suka fi zafi da ƙananan dare masu sanyi.^[8] Kwamitin Intergovernmental kan Canjin Yanayi ya yi hasashen cewa idan yanayin iska ya karu da digiri 1.4, za a sami raguwar 5% zuwa 6% a cikin ruwan sama, karuwar mitar da tsananin abubuwan da suka faru na matsanancin yanayi (gami da karuwar 66% a cikin ƙarfin guguwa), da kuma hauhawar matakin teku na mita 0.5- zuwa 0.6 a cikin Caribbean Netherlands.^[8]

Yankin teku na arewa yana sauka sosai a cikin 60 metres (200 ft) m (200 na bakin tekun Curaçaoan. Wannan raguwa an san shi da "blue edge".

A Curaçao, ana iya samun manyan tsarin ilimin ƙasa guda huɗu: tsarin lava, tsarin Knip, tsarin Mid-Curaçao da tsarin dutse.^[9]

Curaçao yalaka-linkid="304" href="./Mega-annum" id="mw0Q" rel="mw:WikiLink" title="Mega-annum">Na cikin babban lardin Caribbean (CLIP) tare da mahimman bayyanar waɗancan lavas da ke cikin tsibirin wanda ya kunshi Curaçao Lava Formation (CLF). CLF ya kunshi kilomita 5 na lavas na matashin kai tare da wasu intrusions na basalt. Shekaru na waɗannan duwatsu sun haɗa da 89 Ma don lavas da 75 Ma don sills na poikilitic, kodayake wasu jerin na iya fashewa har zuwa 62-66 Ma, suna sanya su a cikin lokacin Cretaceous. Abubuwan da suka hada sun hada da matashin Picrite a tushe, sannan kuma lavas na tholeiitic, sannan hyaloclastites, sannan sills na poikilitic. An ɗaga CLF a hankali har sai an Kafawa ƙuƙwalwar dutse na Eocene-Miocene, kafin bayyanar ƙarshe sama da matakin teku. Christoffelberg da ɓangaren Zevenbergen (Seven Hills) na tsibirin suna da bayyanar Tsarin Knip. Wannan tsari ya haɗa da ajiyar ruwa mai zurfi na yashi mai laushi da yumɓu mai kyau, wanda aka rufe shi da siliceous chert wanda ke dauke da radiolarians. Tsakiyar Curaçao ta ƙunshi ƙasa mai laushi daga CLF da dutse mai laushi.^[10]^[11]

Curaçao tana da rairayin bakin teku da yawa. Yawancin suna gefen kudu na tsibirin. Mafi sanannun sune:

Bayanan da aka ambata

↑ "The World Factbook – Central Intelligence Agency". cia.gov. Retrieved 28 November 2017.
↑ "CIA World Factbook- Curaçao". Retrieved 15 July 2019.
↑ "Hurricanes and Tropical Storms in the Netherlands Antilles and Aruba" (PDF). Meteorological Service Netherlands Antilles and Aruba. 2010. pp. 18, 29. Archived from the original (PDF) on April 25, 2012. Retrieved 2011-11-08.
↑ "Doden door noodweer op Curaçao" (in Holanci). Netherlands National News Agency. 1 November 2010. Retrieved 1 November 2010.
↑ "Damdoorbraken in Curaçao door storm Tomas" (in Holanci). Nieuws.nl. 2 November 2010. Archived from the original on 18 June 2011. Retrieved 2 November 2010.
↑ Elisa Koek (6 November 2010). "50 miljoen schade" (in Holanci). versgeperst.com. Archived from the original on 8 July 2011.
↑ Redactie Aworaki (2 November 2010). "Twee doden op Curaçao door Tropische Storm Tomas". Aworaki.nl.
↑ ^8.0 ^8.1 "Climate change becomes an existential crisis on the islands". Curacao Chronicle. 2021-11-15. Retrieved 2022-07-15.
↑ "CARMABI Research Station Curaçao". researchstationcarmabi.org.
↑ Loewen, M.W.; Duncan, R.A.; Krawl, K.; Kent, A.J.; Sinton, C.W.; Lackey, J. (2011). "Prolonged volcanic history for the Curaçao Lava Formation inferred from new 40Ar-39Ar ages and trace phase geochemistry". American Geophysical Union, Fall Meeting 2011, Abstract Id. V51D-2542. 2011: V51D–2542. Bibcode:2011AGUFM.V51D2542L.
↑ van Buurt, Gerard (2010). "A Short Natural History of Curaçao. In: Crossing Shifting Boundaries, Language and Changing Political status in Aruba, Bonaire and Curaçao" (PDF). Proceedings of the ECICC-conference, Dominica 2009. I: 229–256. Archived from the original (PDF) on 19 May 2019. Retrieved 3 September 2018.

[1] "The World Factbook – Central Intelligence Agency". cia.gov. Retrieved 28 November 2017.

[CIA_World_Factbook-_Curaçao-2] "CIA World Factbook- Curaçao". Retrieved 15 July 2019.

[3] "Hurricanes and Tropical Storms in the Netherlands Antilles and Aruba" (PDF). Meteorological Service Netherlands Antilles and Aruba. 2010. pp. 18, 29. Archived from the original (PDF) on April 25, 2012. Retrieved 2011-11-08.

[4] "Doden door noodweer op Curaçao" (in Holanci). Netherlands National News Agency. 1 November 2010. Retrieved 1 November 2010.

[5] "Damdoorbraken in Curaçao door storm Tomas" (in Holanci). Nieuws.nl. 2 November 2010. Archived from the original on 18 June 2011. Retrieved 2 November 2010.

[6] Elisa Koek (6 November 2010). "50 miljoen schade" (in Holanci). versgeperst.com. Archived from the original on 8 July 2011.

[7] Redactie Aworaki (2 November 2010). "Twee doden op Curaçao door Tropische Storm Tomas". Aworaki.nl.

[:2-8] 8.0 ^8.1 "Climate change becomes an existential crisis on the islands". Curacao Chronicle. 2021-11-15. Retrieved 2022-07-15.

[9] "CARMABI Research Station Curaçao". researchstationcarmabi.org.

[10] Loewen, M.W.; Duncan, R.A.; Krawl, K.; Kent, A.J.; Sinton, C.W.; Lackey, J. (2011). "Prolonged volcanic history for the Curaçao Lava Formation inferred from new 40Ar-39Ar ages and trace phase geochemistry". American Geophysical Union, Fall Meeting 2011, Abstract Id. V51D-2542. 2011: V51D–2542. Bibcode:2011AGUFM.V51D2542L.

[11] van Buurt, Gerard (2010). "A Short Natural History of Curaçao. In: Crossing Shifting Boundaries, Language and Changing Political status in Aruba, Bonaire and Curaçao" (PDF). Proceedings of the ECICC-conference, Dominica 2009. I: 229–256. Archived from the original (PDF) on 19 May 2019. Retrieved 3 September 2018.

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