Tropospheric ozone in the Lower Fraser Valley, British Columbia and the threat of injury to forest plants

During the summers of 2001 and 2002 ambient ozone levels were measured as hourly averages in parts per billion (ppb) at four sites of differing elevation (200, 400, 600 and 1200 m) in the Lower Fraser Valley (LFV), British Columbia. A l l sites were located in forest clearings and experienced hourly...

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Main Author: Krzyzanowski, Judi
Format: Others
Language:English
Published: 2009
Online Access:http://hdl.handle.net/2429/14390
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spelling ndltd-UBC-oai-circle.library.ubc.ca-2429-143902018-01-05T17:37:17Z Tropospheric ozone in the Lower Fraser Valley, British Columbia and the threat of injury to forest plants Krzyzanowski, Judi During the summers of 2001 and 2002 ambient ozone levels were measured as hourly averages in parts per billion (ppb) at four sites of differing elevation (200, 400, 600 and 1200 m) in the Lower Fraser Valley (LFV), British Columbia. A l l sites were located in forest clearings and experienced hourly averages as low as Oppb, and >70ppb. Mean seasonal concentrations show an increase in ambient ozone with elevation due to consistently high nocturnal concentrations and lack of diurnal variation at higher altitudes. Diurnal patterns are in agreement with previous studies showing a peak in concentration in the late afternoon, and a morning increase due to photochemical production and residual layer down mixing. The occurrence of an upper level ridge coinciding with a thermal trough along the coast, cause above average ozone levels to occur, and may cause the National Ambient Air Quality Objective of 82ppb to be exceeded. Cumulative ozone exposures were measured with height in a forest canopy using OGAWA passive samplers mounted to a 10.5m tower. A strong power-law increase in ozone with height was found due to a number of potential processes including deposition and chemical destruction at the surface, uptake by vegetation, and dynamic stability inhibiting down mixing. This relationship shows plants in the LFV may be acting as an effective ozone sink. Plants uptake ozone direcdy through leaf stomates where the pollutant may directly injure foliage. A preliminary survey of native shrubs exhibiting visible ozone injury symptoms suggests that current concentrations of tropospheric ozone in the LFV may be high enough to cause injury to forest species, however more research is required in order to determine the threat of ozone to these economically and culturally important forests. Arts, Faculty of Geography, Department of Graduate 2009-10-29T19:13:55Z 2009-10-29T19:13:55Z 2003 2003-11 Text Thesis/Dissertation http://hdl.handle.net/2429/14390 eng For non-commercial purposes only, such as research, private study and education. Additional conditions apply, see Terms of Use https://open.library.ubc.ca/terms_of_use. 38933611 bytes application/pdf
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language English
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description During the summers of 2001 and 2002 ambient ozone levels were measured as hourly averages in parts per billion (ppb) at four sites of differing elevation (200, 400, 600 and 1200 m) in the Lower Fraser Valley (LFV), British Columbia. A l l sites were located in forest clearings and experienced hourly averages as low as Oppb, and >70ppb. Mean seasonal concentrations show an increase in ambient ozone with elevation due to consistently high nocturnal concentrations and lack of diurnal variation at higher altitudes. Diurnal patterns are in agreement with previous studies showing a peak in concentration in the late afternoon, and a morning increase due to photochemical production and residual layer down mixing. The occurrence of an upper level ridge coinciding with a thermal trough along the coast, cause above average ozone levels to occur, and may cause the National Ambient Air Quality Objective of 82ppb to be exceeded. Cumulative ozone exposures were measured with height in a forest canopy using OGAWA passive samplers mounted to a 10.5m tower. A strong power-law increase in ozone with height was found due to a number of potential processes including deposition and chemical destruction at the surface, uptake by vegetation, and dynamic stability inhibiting down mixing. This relationship shows plants in the LFV may be acting as an effective ozone sink. Plants uptake ozone direcdy through leaf stomates where the pollutant may directly injure foliage. A preliminary survey of native shrubs exhibiting visible ozone injury symptoms suggests that current concentrations of tropospheric ozone in the LFV may be high enough to cause injury to forest species, however more research is required in order to determine the threat of ozone to these economically and culturally important forests. === Arts, Faculty of === Geography, Department of === Graduate
author Krzyzanowski, Judi
spellingShingle Krzyzanowski, Judi
Tropospheric ozone in the Lower Fraser Valley, British Columbia and the threat of injury to forest plants
author_facet Krzyzanowski, Judi
author_sort Krzyzanowski, Judi
title Tropospheric ozone in the Lower Fraser Valley, British Columbia and the threat of injury to forest plants
title_short Tropospheric ozone in the Lower Fraser Valley, British Columbia and the threat of injury to forest plants
title_full Tropospheric ozone in the Lower Fraser Valley, British Columbia and the threat of injury to forest plants
title_fullStr Tropospheric ozone in the Lower Fraser Valley, British Columbia and the threat of injury to forest plants
title_full_unstemmed Tropospheric ozone in the Lower Fraser Valley, British Columbia and the threat of injury to forest plants
title_sort tropospheric ozone in the lower fraser valley, british columbia and the threat of injury to forest plants
publishDate 2009
url http://hdl.handle.net/2429/14390
work_keys_str_mv AT krzyzanowskijudi troposphericozoneinthelowerfraservalleybritishcolumbiaandthethreatofinjurytoforestplants
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