Show simple item record

dc.contributor.authorNazarian, Negin
dc.contributor.authorMartilli, Alberto
dc.contributor.authorNorford, Leslie Keith
dc.contributor.authorKleissl, Jan
dc.date.accessioned2019-08-28T14:53:45Z
dc.date.available2019-08-28T14:53:45Z
dc.date.issued2018-03
dc.date.submitted2016-04
dc.identifier.issn0006-8314
dc.identifier.issn1573-1472
dc.identifier.urihttps://hdl.handle.net/1721.1/122021
dc.description.abstractUrban morphology and inter-building shadowing result in a non-uniform distribution of surface heating in urban areas, which can significantly modify the urban flow and thermal field. In Part I, we found that in an idealized three-dimensional urban array, the spatial distribution of the thermal field is correlated with the orientation of surface heating with respect to the wind direction (i.e. leeward or windward heating), while the dispersion field changes more strongly with the vertical temperature gradient in the street canyon. Here, we evaluate these results more closely and translate them into metrics of “city breathability,” with large-eddy simulations coupled with an urban energy-balance model employed for this purpose. First, we quantify breathability by, (i) calculating the pollutant concentration at the pedestrian level (horizontal plane at z≈ 1.5 –2 m) and averaged over the canopy, and (ii) examining the air exchange rate at the horizontal and vertical ventilating faces of the canyon, such that the in-canopy pollutant advection is distinguished from the vertical removal of pollution. Next, we quantify the change in breathability metrics as a function of previously defined buoyancy parameters, horizontal and vertical Richardson numbers (Rih and Riv, respectively), which characterize realistic surface heating. We find that, unlike the analysis of airflow and thermal fields, consideration of the realistic heating distribution is not crucial in the analysis of city breathability, as the pollutant concentration is mainly correlated with the vertical temperature gradient (Riv) as opposed to the horizontal (Rih) or bulk (Rib) thermal forcing. Additionally, we observe that, due to the formation of the primary vortex, the air exchange rate at the roof level (the horizontal ventilating faces of the building canyon) is dominated by the mean flow. Lastly, since Rih and Riv depend on the meteorological factors (ambient air temperature, wind speed, and wind direction) as well as urban design parameters (such as surface albedo), we propose a methodology for mapping overall outdoor ventilation and city breathability using this characterization method. This methodology helps identify the effects of design on urban microclimate, and ultimately informs urban designers and architects of the impact of their design on air quality, human health, and comfort.en_US
dc.language.isoen
dc.publisherSpringer Natureen_US
dc.relation.isversionofhttp://dx.doi.org/10.1007/s10546-018-0346-6en_US
dc.rightsCreative Commons Attribution-Noncommercial-Share Alikeen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/en_US
dc.sourceOther repositoryen_US
dc.titleImpacts of Realistic Urban Heating. Part II: Air Quality and City Breathabilityen_US
dc.typeArticleen_US
dc.identifier.citationNazarian, Negin et al. "Impacts of Realistic Urban Heating. Part II: Air Quality and City Breathability." Boundary-Layer Meteorology 168, 2 (March 2018): 321-341 © 2018 Springer Natureen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Architectureen_US
dc.relation.journalBoundary-Layer Meteorologyen_US
dc.eprint.versionOriginal manuscripten_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/NonPeerRevieweden_US
dc.date.updated2019-08-07T16:31:21Z
dspace.date.submission2019-08-07T16:31:22Z
mit.journal.volume168en_US
mit.journal.issue2en_US


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record