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Corrections to a description of turbulence in a trafficked street canyon in Manchester [An article from: Atmospheric Environment]
Book Details
Author(s)I. Longley
PublisherElsevier
ISBN / ASINB000RR1F64
ISBN-13978B000RR1F61
AvailabilityAvailable for download now
Sales Rank99,999,999
MarketplaceUnited States 🇺🇸
Description
This digital document is a journal article from Atmospheric Environment, published by Elsevier in 2004. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.
Description:
A paper previously published in Atmospheric Environment (Longley et al. (Atmos. Environ 38 (2004) 69) contained a model describing turbulence data measured in the field. Subsequent re-analysis of the data has uncovered fundamental and irreparable errors in the raw data from one anemometer. This dataset covered measurements by a mobile anemometer at a height of 2m above a road surface within a street canyon. Some key conclusions concerning the influence of traffic upon turbulence were dependent upon this dataset and are no longer valid. New data has been captured from the original street canyon to correct and replace this erroneous data. This new data indicates that the weak positive gradient in turbulent intensity higher in the canyon described in the original paper is consistent down to 2m and that the sharp enhancement at this height originally reported was not observed in the replacement data.
Description:
A paper previously published in Atmospheric Environment (Longley et al. (Atmos. Environ 38 (2004) 69) contained a model describing turbulence data measured in the field. Subsequent re-analysis of the data has uncovered fundamental and irreparable errors in the raw data from one anemometer. This dataset covered measurements by a mobile anemometer at a height of 2m above a road surface within a street canyon. Some key conclusions concerning the influence of traffic upon turbulence were dependent upon this dataset and are no longer valid. New data has been captured from the original street canyon to correct and replace this erroneous data. This new data indicates that the weak positive gradient in turbulent intensity higher in the canyon described in the original paper is consistent down to 2m and that the sharp enhancement at this height originally reported was not observed in the replacement data.
