Summary
Not much is known about the extreme conditions of urban temperature in tropical cities. Also, the concept, heat-island has been hardly related to the other climatic parameters that have some links with temperature. In view of the points mentioned above, this study examined the maximum temperature records as well as the conditions of temperature at 1000 and 1600 Local Zone Time (LZT). The results revealed that for the humid tropical city of Ibadan, heat islands was best indicated by the minimum temperature. Also, some level of relationship was found to exist between heat island and urban/rural difference in potential evaporation.
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References
Adebayo, Y. R., 1987: Land-use approach to the spatial analysis of urban “heat island” in Ibadan, Nigeria.Weather 42, No. 9, 273–280.
Jauregui, E., 1986: Tropical urban climates: review. Urban climatology and its applications with special regard to tropical areas. Proc. of Technical Conference WMO 652, WMO, Geneva.
Nakamura, K., 1966: City temperature of Nairobi.J. Geogr. 75, 316–325.
Oke, T. R., 1979: Review of urban climatology 1973–76. WMO Technical Note 169, WMO, Geneva.
Okoola, R. E., 1980: The Nairobi heat island.Kenya J. Sci. Techn. 1, 53–65.
Padmanabhamarty, B., Bahl, H. D., 1984: Isothermal and isoyetal patterns of Delhi as a sequal of urbanization.Mansam, 35, No. 4.
WMO, 1986: Conclusions and recommendations. Urban climatology and its applications with special regard to tropical areas. Proc. Technical Conf. WMO/WHO Mexico City 1984. WMO No. 652, WMO, Geneva.
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Adebayo, Y.R. “Heat island” in a humid tropical city and its relationship with potential evaporation. Theor Appl Climatol 43, 137–147 (1991). https://doi.org/10.1007/BF00867471
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DOI: https://doi.org/10.1007/BF00867471