Published July 2, 2009 | Version v1

A climatology of flow and turbulence at 190 m above central London

Description

The structure of the surface layer over homogeneous terrain is quite well understood, however there is not thorough knowledge of the corresponding structure over urban areas. The aim of this work is to study turbulent fluxes and variances in the framework of local similarity theory. A sonic anemometer and Vaisala weather station were mounted atop BT tower (at 190 m) from 2003 onwards. Implications include understanding local urban climates for weather prediction and pollutant dispersion purposes. [This work will be submitted to Boundary-Layer Meteorology for peer-review in late 2009.]

Notes

Previously curated at: http://cedadocs.ceda.ac.uk/358/ Event type: conference. The publish date on this item was its original submitted date. This item was not refereed before the publication Main files in this record: Wood_etal_2009_LondonTurbulence.pdf Item originally deposited with Centre for Environmental Data Analysis (CEDA) document repository by Dr Curtis R Wood. Transferred to CEDA document repository community on Zenodo on 2022-11-24

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