AN AIRCRAFT OBSERVED THERMAL INTERNAL BOUNDARY LAYER ALONG THE CAPE SOUTH COAST

Aircraft observations offer a unique meteorological perspective of coastal internal boundary layers along the Cape south coast. One case study near the Gourits River mouth on 22 June 1989 is analysed using aircraft-derived wind, temperature and turbulence data collected every 800 m over a 25 km cros...

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Main Author: M. Jury
Format: Article
Language:English
Published: National Association for Clean Air 1990-06-01
Series:Clean Air Journal
Online Access:https://journals.assaf.org.za/index.php/caj/article/view/7192
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author M. Jury
author_facet M. Jury
author_sort M. Jury
collection DOAJ
description Aircraft observations offer a unique meteorological perspective of coastal internal boundary layers along the Cape south coast. One case study near the Gourits River mouth on 22 June 1989 is analysed using aircraft-derived wind, temperature and turbulence data collected every 800 m over a 25 km cross section. A weak coastal low pressure cell imposed a shallow easterly flow and weather conditions were stable and humid. The speed of surface easterly winds halved from the coast to the river under the influence of surface friction. Surface temperatures, measured by an infrared sensor, increased from ITC at the sea to 250C over the River valley. Upward sensible heat fluxes caused a westward tilted thermal internal boundary layer in the first 100 m. Convergence and river channelling forced the thermal internal boundary layer to become vertically aligned above 100 m. Vertical velocity fluctuations were more vigourous in the internal boundary layer. Implications for the dispersion of air pollutants from proposed petroleum refineries and nuclear power stations ate discussed.
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spelling doaj.art-72cfb841cc3b417ca9b6a3e48ec9cc8c2022-12-21T23:20:17ZengNational Association for Clean AirClean Air Journal2410-972X1017-17031990-06-018110.17159/caj/1990/8/1.7192AN AIRCRAFT OBSERVED THERMAL INTERNAL BOUNDARY LAYER ALONG THE CAPE SOUTH COASTM. Jury0Oceanography Dept, Univ Cape TownAircraft observations offer a unique meteorological perspective of coastal internal boundary layers along the Cape south coast. One case study near the Gourits River mouth on 22 June 1989 is analysed using aircraft-derived wind, temperature and turbulence data collected every 800 m over a 25 km cross section. A weak coastal low pressure cell imposed a shallow easterly flow and weather conditions were stable and humid. The speed of surface easterly winds halved from the coast to the river under the influence of surface friction. Surface temperatures, measured by an infrared sensor, increased from ITC at the sea to 250C over the River valley. Upward sensible heat fluxes caused a westward tilted thermal internal boundary layer in the first 100 m. Convergence and river channelling forced the thermal internal boundary layer to become vertically aligned above 100 m. Vertical velocity fluctuations were more vigourous in the internal boundary layer. Implications for the dispersion of air pollutants from proposed petroleum refineries and nuclear power stations ate discussed.https://journals.assaf.org.za/index.php/caj/article/view/7192
spellingShingle M. Jury
AN AIRCRAFT OBSERVED THERMAL INTERNAL BOUNDARY LAYER ALONG THE CAPE SOUTH COAST
Clean Air Journal
title AN AIRCRAFT OBSERVED THERMAL INTERNAL BOUNDARY LAYER ALONG THE CAPE SOUTH COAST
title_full AN AIRCRAFT OBSERVED THERMAL INTERNAL BOUNDARY LAYER ALONG THE CAPE SOUTH COAST
title_fullStr AN AIRCRAFT OBSERVED THERMAL INTERNAL BOUNDARY LAYER ALONG THE CAPE SOUTH COAST
title_full_unstemmed AN AIRCRAFT OBSERVED THERMAL INTERNAL BOUNDARY LAYER ALONG THE CAPE SOUTH COAST
title_short AN AIRCRAFT OBSERVED THERMAL INTERNAL BOUNDARY LAYER ALONG THE CAPE SOUTH COAST
title_sort aircraft observed thermal internal boundary layer along the cape south coast
url https://journals.assaf.org.za/index.php/caj/article/view/7192
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