2010
DOI: 10.1007/s10546-010-9550-8
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Thermal Energy Balance Analysis of the Tokyo Metropolitan Area Using a Mesoscale Meteorological Model Incorporating an Urban Canopy Model

Abstract: The summer climate around the Tokyo metropolitan area has been analysed on an urban scale, and the regional characteristics of the thermal energy balance of a bayside business district in the centre of Tokyo (Otemachi) have been compared with an inland residential district (Nerima), using a mesoscale meteorological model incorporating an urban canopy model. From the results of the analysis, the mechanism of diurnal change in air temperature and absolute humidity in these areas is quantitatively demonstrated, w… Show more

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Cited by 14 publications
(7 citation statements)
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References 18 publications
(14 reference statements)
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“…The first group looked at the effect of urban climate and heat island effects on buildings [117][118][119][120][121][122][123][124][125][126] and the second looked at a larger district scale [127][128][129][130][131][132][133], including street cross-sections [134][135][136][137][138][139] or raster grid of several hundred meters [140,141].…”
Section: Urban Climatementioning
confidence: 99%
“…The first group looked at the effect of urban climate and heat island effects on buildings [117][118][119][120][121][122][123][124][125][126] and the second looked at a larger district scale [127][128][129][130][131][132][133], including street cross-sections [134][135][136][137][138][139] or raster grid of several hundred meters [140,141].…”
Section: Urban Climatementioning
confidence: 99%
“…The building surface temperature is strongly related to the urban surface condition, which is determined by the energy balance between: 1) the sensible and latent heat fluxes transferred to the air, 2) the received net radiation (short-wave and long-wave), 3) the heat storage into the building materials and the ground, and 4) anthropogenic heat sources [91][92][93], as shown in Fig. 10(a).…”
Section: A C C E P T E D Accepted Manuscriptmentioning
confidence: 99%
“…Concept of heat balance in urban environment: (a) Heat balance of urban surface layer (Mainly from: Ooka et al[93]); (b) Heat balance in thermal environment around buildings (Revised from: Li et al[97]). …”
mentioning
confidence: 99%
“…The synoptic wind speed and direction have an essential impact on the strength of wind effect [35,36]. For the buoyancy effect, one inducement is the difference between indoor and outdoor temperature, the other one can be the thermal plume along the high-temperature walls heated by the solar radiation during the daytime, especially in windless or breezy sunny day [37]. Fan et al [38] measured boundary layer structure along the sunward surface of a sixteen-storey building in Guangzhou, and concluded that the maximum velocity in the boundary layer at a height of 50 m is about 1.0-1.5 m/s with absent wind and a wall/air temperature difference of 14-20 K. Such strong thermal flow should not be neglected since the most common wind speed in the urban environment is in the range of 1.0-2.0 m/s [39].…”
Section: Introductionmentioning
confidence: 99%