The Use of Critical Levels for Determining Plant Response to Ozone in Europe and in North America

Critical levels to determine plant response to ozone (O3) have been used in Europe since the 1980s, utilizing the concentration-based AOT40 to relate plant response to ambient O3 exposure. More recently, there has been progress in Europe toward utilizing flux-based critical levels, because plant res...

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Main Authors: Robert C. Musselman, Allen S. Lefohn
Format: Article
Language:English
Published: Hindawi Limited 2007-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1100/tsw.2007.24
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spelling doaj-67ca1810304348b08ae74989ab27b0152020-11-25T02:15:34ZengHindawi LimitedThe Scientific World Journal1537-744X2007-01-017152110.1100/tsw.2007.24The Use of Critical Levels for Determining Plant Response to Ozone in Europe and in North AmericaRobert C. Musselman0Allen S. Lefohn1USDA Forest Service, Rocky Mountain Research Station, Fort Collins, CO, USAA.S.L. and Associates, Helena, MT, USACritical levels to determine plant response to ozone (O3) have been used in Europe since the 1980s, utilizing the concentration-based AOT40 to relate plant response to ambient O3 exposure. More recently, there has been progress in Europe toward utilizing flux-based critical levels, because plant response is more closely related to O3 uptake than to the amount of O3 in ambient air. Flux-based critical levels are plant species specific; data for parameterization of flux-based critical levels models are lacking for most plant species. Although flux-based critical levels are now being used for a limited number of agricultural crops and tree species where data are available, the use of flux-based critical levels is limited by the lack of adequate consideration and incorporation of plant internal detoxification mechanisms in flux modeling. Critical levels have not been used in North America; however, recent interest in the U.S. and Canada for using critical loads for nitrogen and sulfur has generated interest in using critical levels for O3. A major obstacle for utilization of critical levels in North America is that ambient air quality standards for O3 in the U.S. and Canada are concentration based. It appears that cumulative exposure-based metrics, particularly when implemented with a quantification of peak concentrations and environmental variables, such as a drought index, are currently the most useful to relate O3 to vegetation response. Because data are unavailable to quantify detoxification potential of vegetation, effective flux models are not available to determine plant response to O3.http://dx.doi.org/10.1100/tsw.2007.24
collection DOAJ
language English
format Article
sources DOAJ
author Robert C. Musselman
Allen S. Lefohn
spellingShingle Robert C. Musselman
Allen S. Lefohn
The Use of Critical Levels for Determining Plant Response to Ozone in Europe and in North America
The Scientific World Journal
author_facet Robert C. Musselman
Allen S. Lefohn
author_sort Robert C. Musselman
title The Use of Critical Levels for Determining Plant Response to Ozone in Europe and in North America
title_short The Use of Critical Levels for Determining Plant Response to Ozone in Europe and in North America
title_full The Use of Critical Levels for Determining Plant Response to Ozone in Europe and in North America
title_fullStr The Use of Critical Levels for Determining Plant Response to Ozone in Europe and in North America
title_full_unstemmed The Use of Critical Levels for Determining Plant Response to Ozone in Europe and in North America
title_sort use of critical levels for determining plant response to ozone in europe and in north america
publisher Hindawi Limited
series The Scientific World Journal
issn 1537-744X
publishDate 2007-01-01
description Critical levels to determine plant response to ozone (O3) have been used in Europe since the 1980s, utilizing the concentration-based AOT40 to relate plant response to ambient O3 exposure. More recently, there has been progress in Europe toward utilizing flux-based critical levels, because plant response is more closely related to O3 uptake than to the amount of O3 in ambient air. Flux-based critical levels are plant species specific; data for parameterization of flux-based critical levels models are lacking for most plant species. Although flux-based critical levels are now being used for a limited number of agricultural crops and tree species where data are available, the use of flux-based critical levels is limited by the lack of adequate consideration and incorporation of plant internal detoxification mechanisms in flux modeling. Critical levels have not been used in North America; however, recent interest in the U.S. and Canada for using critical loads for nitrogen and sulfur has generated interest in using critical levels for O3. A major obstacle for utilization of critical levels in North America is that ambient air quality standards for O3 in the U.S. and Canada are concentration based. It appears that cumulative exposure-based metrics, particularly when implemented with a quantification of peak concentrations and environmental variables, such as a drought index, are currently the most useful to relate O3 to vegetation response. Because data are unavailable to quantify detoxification potential of vegetation, effective flux models are not available to determine plant response to O3.
url http://dx.doi.org/10.1100/tsw.2007.24
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