Physics of Flow and Transport in Urban Canopy Layers

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Biosphere/Hydrosphere/Land–Atmosphere Interactions".

Deadline for manuscript submissions: closed (25 December 2020) | Viewed by 1957

Special Issue Editors


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Guest Editor
Department of Meteorology, University of Reading, Reading RG6 6BB, UK
Interests: urban climate; hydrometeorology

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Guest Editor
Geography and Environmental Sciences, University of Colorado Denver, Denver, CO 80204, USA
Interests: urban climate; surface–atmosphere interactions; biogeochemical cycles; air quality; sensor networks; surface energy balance; renewable energy
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Special Issue Information

Dear Colleagues,

Today, human activities, especially those in urban areas, are transforming the global environment at an unpreceded rate and scale. Urban centers feature high population density, a heavily modified landscape, burgeoning anthropogenic stress, and on top of that, novel challenges of urban environmental issues, the urban heat island being a well-known example. Urban dynamics underlies a complex interplay between humans and nature, the understanding of which requires process-level knowledge augmented by system-level modeling, of which the urban atmosphere is a critical element. This Special Issue of Atmosphere focuses on the flow and transport of energy, water, greenhouse gases, and pollutants in urban canopy layers. We invite you to contribute to this Special Issue with your state-of-the-art research endeavors to further our fundamental understanding of the physics and thermodynamics of flow over complex built terrains, and more importantly, to inform and foster sustainable urban environment management and policy-making processes in the long run. We solicit original research papers, reviews, and perspectives on all topics related to urban atmospheric studies, with an impact on local hydrometeorological changes as well as regional and global environment–health–climate repercussions. Specific topics include but are not limited to observations and numerical simulations of urban flow field, exchange of energy, water, and scalars in the land–atmosphere continuum, and the underlying dynamics of the urban heat island, air pollution, and hydroclimate changes.

Dr. Ting Sun
Dr. Benjamin Crawford
Guest Editors

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Keywords

  • atmospheric transport
  • greenhouse gas and air pollution
  • heat island and mitigation
  • urban canopy layer processes
  • urban hydrometeorology
  • urban fluid dynamics

Published Papers (1 paper)

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Research

14 pages, 764 KiB  
Article
Temperature Response from the Change of Surface Heat Flux and Vertical Diffusivity by Urbanization
by Shuzhan Ren and Craig A. Stroud
Atmosphere 2020, 11(9), 978; https://doi.org/10.3390/atmos11090978 - 12 Sep 2020
Cited by 3 | Viewed by 1586
Abstract
A 1-D diffusion model of temperature is employed to understand important features of temperature response to the changes of surface heat flux (SHF) and vertical diffusivity shown in 3-D model simulations. Analytical results show that the temperature response to the SHF change is [...] Read more.
A 1-D diffusion model of temperature is employed to understand important features of temperature response to the changes of surface heat flux (SHF) and vertical diffusivity shown in 3-D model simulations. Analytical results show that the temperature response to the SHF change is the convolution of the SHF change and Green’s function (GF). Because the GF is inversely proportional to the square root of diffusion coefficient near the surface, weak/strong diffusivity in the early morning/noontime tends to generate a large/small temperature response by slowing/accelerating heat flow from surface to the atmosphere. The modulation effect of the GF and the convolution effect explain very different temperature responses to the SHF change during each period. Analytical results also show that the temperature response to the change of DF is equal to the convolution of the product of diffusion coefficient change, vertical gradients of reference temperature and the GF. Because the vertical gradient of the GF is negative below 80 m, enhanced/reduced diffusivity would enhance/weaken the urban temperature, if the vertical gradient of reference temperature is negative/positive. Numerical results with typical values of the changes of SHF and diffusivity suggest that the changes of SHF has the dominant contribution to the temperature response. Full article
(This article belongs to the Special Issue Physics of Flow and Transport in Urban Canopy Layers)
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