An ozone episode in the Philadelphia metropolitan area. Kleinman, L., I., Ryan, W., F., Daum, P., H., Springston, S., R., Lee, Y., N., Nunnermacker, L., J., & Weinstein-Lloyd, J. Journal of Geophysical Research-Atmospheres, 109(D20):-, 2004. Website abstract bibtex [1] In July and August 1999 a Northeast Oxidant and Particle Study field campaign was conducted in the Philadelphia metropolitan area to determine causes for episodically high levels of O-3 and particulate matter less than or equal to 2.5 mum in aerodynamic diameter. We report emission estimates, weather information, surface O-3 monitoring data, and aircraft observations, with a focus on 31 July, the last day of an O-3 episode in which concentrations in Philadelphia reached 165 ppb, the highest level observed there in the past 11 years. As is common in the northeastern states, this O-3 episode started with the development of a broad ridge over the central United States and ended with the northeast corridor under the influence of an Appalachian lee trough with airflow from the SW in an along-corridor direction. For a portion of the morning of 31 July, winds were nearly stagnant, allowing local emissions to accumulate. In contrast to typical O-3 episodes in the northeast, transport on 31 July was limited, and O-3 hot spots occurred close to NOx and volatile organic compound (VOC) emission sources. High O-3 was observed downwind of Baltimore and Philadelphia, both major urban areas. High O-3 was also observed in a less likely region near the Delaware-Pennsylvania border, downwind of Wilmington, Delaware, but near utility and industrial emission sources. Surface O-3 monitoring data and morning aircraft observations show that the residual layer aloft contained 80 - 100 ppb of O-3 but almost no O-3 precursors. Same-day photochemistry on 31 July caused surface O-3 concentrations to increase by 60 - 80 ppb. Photochemical model calculations indicate O-3 production rates in excess of 20 ppb h(-1) in regions with NOx > 5 ppb. High NOx concentrations are a consequence of poor ventilation. Peroxide observations and calculations indicate that O-3 production is VOC limited in the high-NOx portions of the Philadelphia urban plume. Our results are contrasted against a severe O-3 episode that occurred in 1995. While the 1999 episode had stagnation conditions leading to local O-3 hot spots, there were mesoscale meteorological features in 1995 that favored interregional transport.
@article{
title = {An ozone episode in the Philadelphia metropolitan area},
type = {article},
year = {2004},
identifiers = {[object Object]},
keywords = {chemistry,hydrocarbons,nashville,northeastern united-states,o-3 formation,ozone,ozone episode,photochemistry,southern oxidants,stagnation episode,tennessee,transport,urban},
pages = {-},
volume = {109},
websites = {<Go to ISI>://000224876600005},
id = {5dd587e7-6c25-356b-b1a3-933fd00cd1e5},
created = {2015-02-12T02:07:30.000Z},
file_attached = {false},
profile_id = {81af7548-db00-3f00-bfa0-1774347c59e1},
group_id = {63e349d6-2c70-3938-9e67-2f6483f6cbab},
last_modified = {2015-02-12T20:20:27.000Z},
read = {false},
starred = {false},
authored = {false},
confirmed = {true},
hidden = {false},
source_type = {Journal Article},
language = {English},
notes = {<m:note>867XQ<m:linebreak/>Times Cited:5<m:linebreak/>Cited References Count:32</m:note>},
abstract = {[1] In July and August 1999 a Northeast Oxidant and Particle Study field campaign was conducted in the Philadelphia metropolitan area to determine causes for episodically high levels of O-3 and particulate matter less than or equal to 2.5 mum in aerodynamic diameter. We report emission estimates, weather information, surface O-3 monitoring data, and aircraft observations, with a focus on 31 July, the last day of an O-3 episode in which concentrations in Philadelphia reached 165 ppb, the highest level observed there in the past 11 years. As is common in the northeastern states, this O-3 episode started with the development of a broad ridge over the central United States and ended with the northeast corridor under the influence of an Appalachian lee trough with airflow from the SW in an along-corridor direction. For a portion of the morning of 31 July, winds were nearly stagnant, allowing local emissions to accumulate. In contrast to typical O-3 episodes in the northeast, transport on 31 July was limited, and O-3 hot spots occurred close to NOx and volatile organic compound (VOC) emission sources. High O-3 was observed downwind of Baltimore and Philadelphia, both major urban areas. High O-3 was also observed in a less likely region near the Delaware-Pennsylvania border, downwind of Wilmington, Delaware, but near utility and industrial emission sources. Surface O-3 monitoring data and morning aircraft observations show that the residual layer aloft contained 80 - 100 ppb of O-3 but almost no O-3 precursors. Same-day photochemistry on 31 July caused surface O-3 concentrations to increase by 60 - 80 ppb. Photochemical model calculations indicate O-3 production rates in excess of 20 ppb h(-1) in regions with NOx > 5 ppb. High NOx concentrations are a consequence of poor ventilation. Peroxide observations and calculations indicate that O-3 production is VOC limited in the high-NOx portions of the Philadelphia urban plume. Our results are contrasted against a severe O-3 episode that occurred in 1995. While the 1999 episode had stagnation conditions leading to local O-3 hot spots, there were mesoscale meteorological features in 1995 that favored interregional transport.},
bibtype = {article},
author = {Kleinman, L I and Ryan, W F and Daum, P H and Springston, S R and Lee, Y N and Nunnermacker, L J and Weinstein-Lloyd, J},
journal = {Journal of Geophysical Research-Atmospheres},
number = {D20}
}
Downloads: 0
{"_id":"dKtGwuFZo2S4wZa8k","bibbaseid":"kleinman-ryan-daum-springston-lee-nunnermacker-weinsteinlloyd-anozoneepisodeinthephiladelphiametropolitanarea-2004","downloads":0,"creationDate":"2017-01-12T21:32:07.268Z","title":"An ozone episode in the Philadelphia metropolitan area","author_short":["Kleinman, L., I.","Ryan, W., F.","Daum, P., H.","Springston, S., R.","Lee, Y., N.","Nunnermacker, L., J.","Weinstein-Lloyd, J."],"year":2004,"bibtype":"article","biburl":null,"bibdata":{"title":"An ozone episode in the Philadelphia metropolitan area","type":"article","year":"2004","identifiers":"[object Object]","keywords":"chemistry,hydrocarbons,nashville,northeastern united-states,o-3 formation,ozone,ozone episode,photochemistry,southern oxidants,stagnation episode,tennessee,transport,urban","pages":"-","volume":"109","websites":"<Go to ISI>://000224876600005","id":"5dd587e7-6c25-356b-b1a3-933fd00cd1e5","created":"2015-02-12T02:07:30.000Z","file_attached":false,"profile_id":"81af7548-db00-3f00-bfa0-1774347c59e1","group_id":"63e349d6-2c70-3938-9e67-2f6483f6cbab","last_modified":"2015-02-12T20:20:27.000Z","read":false,"starred":false,"authored":false,"confirmed":"true","hidden":false,"source_type":"Journal Article","language":"English","notes":"<m:note>867XQ<m:linebreak/>Times Cited:5<m:linebreak/>Cited References Count:32</m:note>","abstract":"[1] In July and August 1999 a Northeast Oxidant and Particle Study field campaign was conducted in the Philadelphia metropolitan area to determine causes for episodically high levels of O-3 and particulate matter less than or equal to 2.5 mum in aerodynamic diameter. We report emission estimates, weather information, surface O-3 monitoring data, and aircraft observations, with a focus on 31 July, the last day of an O-3 episode in which concentrations in Philadelphia reached 165 ppb, the highest level observed there in the past 11 years. As is common in the northeastern states, this O-3 episode started with the development of a broad ridge over the central United States and ended with the northeast corridor under the influence of an Appalachian lee trough with airflow from the SW in an along-corridor direction. For a portion of the morning of 31 July, winds were nearly stagnant, allowing local emissions to accumulate. In contrast to typical O-3 episodes in the northeast, transport on 31 July was limited, and O-3 hot spots occurred close to NOx and volatile organic compound (VOC) emission sources. High O-3 was observed downwind of Baltimore and Philadelphia, both major urban areas. High O-3 was also observed in a less likely region near the Delaware-Pennsylvania border, downwind of Wilmington, Delaware, but near utility and industrial emission sources. Surface O-3 monitoring data and morning aircraft observations show that the residual layer aloft contained 80 - 100 ppb of O-3 but almost no O-3 precursors. Same-day photochemistry on 31 July caused surface O-3 concentrations to increase by 60 - 80 ppb. Photochemical model calculations indicate O-3 production rates in excess of 20 ppb h(-1) in regions with NOx > 5 ppb. High NOx concentrations are a consequence of poor ventilation. Peroxide observations and calculations indicate that O-3 production is VOC limited in the high-NOx portions of the Philadelphia urban plume. Our results are contrasted against a severe O-3 episode that occurred in 1995. While the 1999 episode had stagnation conditions leading to local O-3 hot spots, there were mesoscale meteorological features in 1995 that favored interregional transport.","bibtype":"article","author":"Kleinman, L I and Ryan, W F and Daum, P H and Springston, S R and Lee, Y N and Nunnermacker, L J and Weinstein-Lloyd, J","journal":"Journal of Geophysical Research-Atmospheres","number":"D20","bibtex":"@article{\n title = {An ozone episode in the Philadelphia metropolitan area},\n type = {article},\n year = {2004},\n identifiers = {[object Object]},\n keywords = {chemistry,hydrocarbons,nashville,northeastern united-states,o-3 formation,ozone,ozone episode,photochemistry,southern oxidants,stagnation episode,tennessee,transport,urban},\n pages = {-},\n volume = {109},\n websites = {<Go to ISI>://000224876600005},\n id = {5dd587e7-6c25-356b-b1a3-933fd00cd1e5},\n created = {2015-02-12T02:07:30.000Z},\n file_attached = {false},\n profile_id = {81af7548-db00-3f00-bfa0-1774347c59e1},\n group_id = {63e349d6-2c70-3938-9e67-2f6483f6cbab},\n last_modified = {2015-02-12T20:20:27.000Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n source_type = {Journal Article},\n language = {English},\n notes = {<m:note>867XQ<m:linebreak/>Times Cited:5<m:linebreak/>Cited References Count:32</m:note>},\n abstract = {[1] In July and August 1999 a Northeast Oxidant and Particle Study field campaign was conducted in the Philadelphia metropolitan area to determine causes for episodically high levels of O-3 and particulate matter less than or equal to 2.5 mum in aerodynamic diameter. We report emission estimates, weather information, surface O-3 monitoring data, and aircraft observations, with a focus on 31 July, the last day of an O-3 episode in which concentrations in Philadelphia reached 165 ppb, the highest level observed there in the past 11 years. As is common in the northeastern states, this O-3 episode started with the development of a broad ridge over the central United States and ended with the northeast corridor under the influence of an Appalachian lee trough with airflow from the SW in an along-corridor direction. For a portion of the morning of 31 July, winds were nearly stagnant, allowing local emissions to accumulate. In contrast to typical O-3 episodes in the northeast, transport on 31 July was limited, and O-3 hot spots occurred close to NOx and volatile organic compound (VOC) emission sources. High O-3 was observed downwind of Baltimore and Philadelphia, both major urban areas. High O-3 was also observed in a less likely region near the Delaware-Pennsylvania border, downwind of Wilmington, Delaware, but near utility and industrial emission sources. Surface O-3 monitoring data and morning aircraft observations show that the residual layer aloft contained 80 - 100 ppb of O-3 but almost no O-3 precursors. Same-day photochemistry on 31 July caused surface O-3 concentrations to increase by 60 - 80 ppb. Photochemical model calculations indicate O-3 production rates in excess of 20 ppb h(-1) in regions with NOx > 5 ppb. High NOx concentrations are a consequence of poor ventilation. Peroxide observations and calculations indicate that O-3 production is VOC limited in the high-NOx portions of the Philadelphia urban plume. Our results are contrasted against a severe O-3 episode that occurred in 1995. While the 1999 episode had stagnation conditions leading to local O-3 hot spots, there were mesoscale meteorological features in 1995 that favored interregional transport.},\n bibtype = {article},\n author = {Kleinman, L I and Ryan, W F and Daum, P H and Springston, S R and Lee, Y N and Nunnermacker, L J and Weinstein-Lloyd, J},\n journal = {Journal of Geophysical Research-Atmospheres},\n number = {D20}\n}","author_short":["Kleinman, L., I.","Ryan, W., F.","Daum, P., H.","Springston, S., R.","Lee, Y., N.","Nunnermacker, L., J.","Weinstein-Lloyd, J."],"urls":{"Website":"<Go to ISI>://000224876600005"},"bibbaseid":"kleinman-ryan-daum-springston-lee-nunnermacker-weinsteinlloyd-anozoneepisodeinthephiladelphiametropolitanarea-2004","role":"author","keyword":["chemistry","hydrocarbons","nashville","northeastern united-states","o-3 formation","ozone","ozone episode","photochemistry","southern oxidants","stagnation episode","tennessee","transport","urban"],"downloads":0},"search_terms":["ozone","episode","philadelphia","metropolitan","area","kleinman","ryan","daum","springston","lee","nunnermacker","weinstein-lloyd"],"keywords":["chemistry","hydrocarbons","nashville","northeastern united-states","o-3 formation","ozone","ozone episode","photochemistry","southern oxidants","stagnation episode","tennessee","transport","urban"],"authorIDs":[]}