Tropical marine climate

Sauyin yanayi na ruwa na wurare masu zafi yanayi ne na wurare masu zafi wanda teku ke yin tasiri da farko. Yawanci yana fuskantar tsibirai da yankunan bakin teku 10° zuwa 20° arewa da kudancin equator. Akwai manyan yanayi guda biyu a cikin yanayin yanayin ruwa na wurare masu zafi: lokacin damina da lokacin rani. Ruwan sama na shekara-shekara shine 1000 zuwa sama da 1500 mm (inci 39 zuwa 59). Yanayin zafin jiki ya bambanta daga 20 zuwa 35 ° C (68 zuwa 95 ° F). A ƙarƙashin rarrabuwar yanayi na Köppen, "yanayin ruwa na wurare masu zafi" zai faɗi ƙarƙashin Af ko Am, dazuzzukan ruwan sama ko yanayin damina mai zafi. Iskar cinikin tana kadawa duk shekara kuma tana da ɗanshi, yayin da suke wucewa ta kan tekuna masu dumi[1]. Ana samun waɗannan yanayi na yanayi, alal misali, a ko'ina cikin Caribbean, Gabashin Gabas na Brazil, Madagascar da Queensland; da tsibirai da yawa a cikin ruwan zafi.Wilson, Mark (2016). The Caribbean Environment for CSEC Geography (fifth ed.). Oxford University Press. pp. 114ff. ISBN 9780198374565. OCLC 957691086.Filho, Walter Leal (2017-11-23). Climate Change Impacts and Adaptation Strategies for Coastal Communities. Springer. ISBN 9783319707037. Fiji has a tropical marine climate, with average daily temperatures at Suva ranging from 20.4–26.5 °C in July to 23.8–31.0 °C in FebruarySheppard, Charles (2013-03-14). Coral Reefs of the United Kingdom Overseas Territories. Springer Science & Business Media. ISBN 9789400759657. The climate of the Cayman Islands is influenced by their location in the western Caribbean Basin. The islands have a tropical marine climate with two distinct seasons

 Lokaci 
A lokacin rani ana samun ƙarancin ruwan sama fiye da lokacin damina, amma akwai ɗan bambanci a yanayin zafi tsakanin yanayi biyu. Yankunan ruwa na wurare masu zafi suna samun tasirin anticyclones a lokacin rani da raƙuman ruwa na wurare masu zafi a lokacin damina.

 Daidaita yanayin muhalli 
Yanayin yanayin yanayin ruwa na wurare masu zafi dole ne ya dace da lokacin rani. Tsirrai a lokacin rani dole ne su kiyaye ruwa/danshi. Koyaya, girman daidaitawar ya dogara da yawan ruwan sama na shekara-shekara.

Tsarin muhalli na hygrophytic yana faruwa lokacin da akwai ɗan gajeren lokacin bushewa tare da ƴan ruwan sama. Ƙasar da ke cikin wannan yanayin tana ɗaukar isasshen ruwa don girma shuka. Yawancin yanayin yanayin ruwa na wurare masu zafi suna kusa da gandun daji na gaskiya.London, Norrel A.; Senior, Michael W. (1991). Principles of geography for CXC (second ed.). London: Longman. ISBN 9780582039896. OCLC 26351362

 Mesophytic muhalli 
Tsarin yanayi na mesophytic kuma ana san shi da gandun daji mai shuɗi mai duhu. Ana samun shi inda akwai dogon lokacin rani wanda ba shi da ƙarancin ruwan sama. Akwai ƙarancin ciyayi fiye da cikin dajin damina. Labarun bishiya ne kawai; bishiyoyi suna zubar da ganye ko kuma suna da ƙananan ganye. Wannan yana ba da tsire-tsire hanya don adana danshi.

Akwai ƙarancin epiphytes fiye da dajin ruwan sama kamar yadda alfarwar ta bushe. A lokacin rani ƙasa tana rufe da ganye waɗanda ba za su ruɓe ba har sai ƙasa ta yi laushi. Bishiyoyin kan yi fure a lokacin rani kuma suna fara girma a lokacin damina. Kasa yawanci latasol ne.

 Tsarin muhalli na Xerophytic 
An kuma san yanayin yanayin xerophytic da busasshiyar itace. Ana samunsa a wuraren inuwar ruwan sama a cikin yanayi na wurare masu zafi na ruwa. Wannan yanayin yanayin sau da yawa yana tasowa ƙasa mai zubewa da sauri.

Busasshiyar gandun daji ya sha bamban da dajin damina. Halittar halittu ta yi ƙasa da gandun daji da yawa saboda ƙarancin ruwan sama. Mafi tsayin bishiyoyin suna da tsayin mita 15 zuwa 25 kawai a busasshiyar gandun daji. Busassun bishiyoyi ko dai suna da ƙananan ganye ko kuma suna zubar da ganye. Itatuwan suna da kauri sosai, kuma kututtukan sun kasance karkatattu.Wilson, Mark (2016). The Caribbean Environment for CSEC Geography (fifth ed.). Oxford University Press. pp. 114ff. ISBN 9780198374565. OCLC 957691086.

Filho, Walter Leal (2017-11-23). Climate Change Impacts and Adaptation Strategies for Coastal Communities. Springer. ISBN 9783319707037. Fiji has a tropical marine climate, with average daily temperatures at Suva ranging from 20.4–26.5 °C in July to 23.8–31.0 °C in February

Sheppard, Charles (2013-03-14). Coral Reefs of the United Kingdom Overseas Territories. Springer Science & Business Media. ISBN 9789400759657. The climate of the Cayman Islands is influenced by their location in the western Caribbean Basin. The islands have a tropical marine climate with two distinct seasons

London, Norrel A.; Senior, Michael W. (1991). Principles of geography for CXC (second ed.). London: Longman. ISBN 9780582039896. OCLC 26351362

 Bambance-bambance 
Mangroves suna girma a cikin dausayi na bakin teku, waɗanda ake kira hydrophytic ecosystems. Tsire-tsire a bakin teku yawanci sun dace da ƙasa mai yashi. Dazuzzukan montane da gandun daji na elfin suna girma a kan sanyi, damshi, yankuna masu tsaunuka.

 Duba kuma 
Tropics

Yanayin yanayi na wurare masu zafi na savanna

Yanayin damina mai zafi

Yanayin dajin na wurare masu zafi

Dazuzzukan dazuzzukan wurare masu zafi da na wurare masu zafi

Tsarin yanayi na Köppen

 Manazarta