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dc.date.accessioned2022-12-27T23:14:35Z
dc.date.available2022-12-27T23:14:35Z
dc.date.copyright8/17/2022 12:00:00 AM
dc.date.issued2022
dc.identifier.issn2642-6641
dc.identifier.otherjesbc_3_2_020201.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4288195
dc.description.abstractTropical environments cover a large part of the Earth: almost all the portion of the planetary surface included between latitudes 23.43 North (Tropic of Cancer) and 23.43 South (Tropic of Capricorn) [1]. Tropical climates can be divided in three subclimates: rainforest, monsoon, and savannah [2]. All these climates imply high humidity values and average temperatures of the coldest month greater to 18 °C [3]. In such environments, buildings and cities must face overheating for large periods of the year. Moreover, almost the 40% of humanity is living in these environments [4], and the number is expected to grow to the 50% by the 2050 [5]. Many megalopolises with more than 10.000.000 of inhabitants are placed there: Calcutta (India), Lagos (Nigeria), Rio de Janeiro (Brazil), Canton (China), and Manila (Philippines) are just a few examples.
dc.publisherThe American Society of Mechanical Engineers (ASME)
dc.titleAdvancing Climate Change Adaptation and Mitigation Strategies in the Tropics
dc.typeJournal Paper
dc.journal.volume3
dc.journal.issue2
dc.journal.titleASME Journal of Engineering for Sustainable Buildings and Cities
dc.identifier.doi10.1115/1.4055138
dc.journal.fristpage20201
dc.journal.lastpage20201_2
dc.page2
dc.treeASME Journal of Engineering for Sustainable Buildings and Cities:;2022:;volume( 003 ):;issue: 002
dc.contenttypeFulltext


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