Robert Maisha, T. Ndarana, Francois A. Engelbrecht, M. Thatcher, Mary-Jane M. Bopape, J. van der Merwe, Y. Padayachi, Cecilia Masemola
{"title":"南非德班尼热岛的模拟","authors":"Robert Maisha, T. Ndarana, Francois A. Engelbrecht, M. Thatcher, Mary-Jane M. Bopape, J. van der Merwe, Y. Padayachi, Cecilia Masemola","doi":"10.1175/jamc-d-21-0231.1","DOIUrl":null,"url":null,"abstract":"\nThe study evaluates the performance of the Conformal-Cubic Atmospheric Model (CCAM) when simulating an urban heat island (UHi) over the City of eThekwini, located along the southeast coast of South Africa. The CCAM model is applied at a grid length of 1 km on the panel with eThekwini, in a stretched grid mode. The CCAM is coupled to the urban climate model (UCM) called the Australian Town Energy Budget (ATEB). The ATEB incorporates measured urban parameters including building characteristics, emissions, and albedo. The ATEB incorporates the landcover boundary conditions obtained from the Moderate Resolution Imaging Spectroradiometer (MODIS) satellite. The CCAM configuration applied realistically captured the orientation of the city and landcover types. Simulations of meteorological variables such as temperatures and longwave radiation reproduced the spatial distribution and intensity of the UHi. Results shows that the UHi is stronger during summer and weaker in all other seasons. The UHi developed because of natural factors (i.e., distribution of longwave radiation) and human factors (i.e., urban expansion, an increase in anthropogenic emissions, and additional heating). Due to the city location along the coast, the UHi simulation could be weakened by atmospheric circulation resulting from land and sea breezes. Mitigation methods such as applying reflective paints and revegetation of the city may increase albedo and latent heat fluxes but reduce the sensible heat fluxes and weakens the UHi. However, the UHi may not be completely eliminated since natural factors emissions constantly influence its development.","PeriodicalId":15027,"journal":{"name":"Journal of Applied Meteorology and Climatology","volume":" ","pages":""},"PeriodicalIF":2.6000,"publicationDate":"2023-04-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Simulation of the eThekwini Heat Island in South Africa\",\"authors\":\"Robert Maisha, T. Ndarana, Francois A. Engelbrecht, M. Thatcher, Mary-Jane M. Bopape, J. van der Merwe, Y. Padayachi, Cecilia Masemola\",\"doi\":\"10.1175/jamc-d-21-0231.1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\\nThe study evaluates the performance of the Conformal-Cubic Atmospheric Model (CCAM) when simulating an urban heat island (UHi) over the City of eThekwini, located along the southeast coast of South Africa. The CCAM model is applied at a grid length of 1 km on the panel with eThekwini, in a stretched grid mode. The CCAM is coupled to the urban climate model (UCM) called the Australian Town Energy Budget (ATEB). The ATEB incorporates measured urban parameters including building characteristics, emissions, and albedo. The ATEB incorporates the landcover boundary conditions obtained from the Moderate Resolution Imaging Spectroradiometer (MODIS) satellite. The CCAM configuration applied realistically captured the orientation of the city and landcover types. Simulations of meteorological variables such as temperatures and longwave radiation reproduced the spatial distribution and intensity of the UHi. Results shows that the UHi is stronger during summer and weaker in all other seasons. The UHi developed because of natural factors (i.e., distribution of longwave radiation) and human factors (i.e., urban expansion, an increase in anthropogenic emissions, and additional heating). Due to the city location along the coast, the UHi simulation could be weakened by atmospheric circulation resulting from land and sea breezes. Mitigation methods such as applying reflective paints and revegetation of the city may increase albedo and latent heat fluxes but reduce the sensible heat fluxes and weakens the UHi. 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Simulation of the eThekwini Heat Island in South Africa
The study evaluates the performance of the Conformal-Cubic Atmospheric Model (CCAM) when simulating an urban heat island (UHi) over the City of eThekwini, located along the southeast coast of South Africa. The CCAM model is applied at a grid length of 1 km on the panel with eThekwini, in a stretched grid mode. The CCAM is coupled to the urban climate model (UCM) called the Australian Town Energy Budget (ATEB). The ATEB incorporates measured urban parameters including building characteristics, emissions, and albedo. The ATEB incorporates the landcover boundary conditions obtained from the Moderate Resolution Imaging Spectroradiometer (MODIS) satellite. The CCAM configuration applied realistically captured the orientation of the city and landcover types. Simulations of meteorological variables such as temperatures and longwave radiation reproduced the spatial distribution and intensity of the UHi. Results shows that the UHi is stronger during summer and weaker in all other seasons. The UHi developed because of natural factors (i.e., distribution of longwave radiation) and human factors (i.e., urban expansion, an increase in anthropogenic emissions, and additional heating). Due to the city location along the coast, the UHi simulation could be weakened by atmospheric circulation resulting from land and sea breezes. Mitigation methods such as applying reflective paints and revegetation of the city may increase albedo and latent heat fluxes but reduce the sensible heat fluxes and weakens the UHi. However, the UHi may not be completely eliminated since natural factors emissions constantly influence its development.
期刊介绍:
The Journal of Applied Meteorology and Climatology (JAMC) (ISSN: 1558-8424; eISSN: 1558-8432) publishes applied research on meteorology and climatology. Examples of meteorological research include topics such as weather modification, satellite meteorology, radar meteorology, boundary layer processes, physical meteorology, air pollution meteorology (including dispersion and chemical processes), agricultural and forest meteorology, mountain meteorology, and applied meteorological numerical models. Examples of climatological research include the use of climate information in impact assessments, dynamical and statistical downscaling, seasonal climate forecast applications and verification, climate risk and vulnerability, development of climate monitoring tools, and urban and local climates.