What is causing high ozone at Summit, Greenland?

Causes for the unusually high and seasonally anomalous ozone concentrations at Summit, Greenland were investigated. Surface data from continuous monitoring, ozone sonde data, tethered balloon vertical profiling data, correlation of ozone with the radionuclide tracers 7Be and 210Pb, and synoptic tran...

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Published in:Atmospheric Environment
Main Authors: Helmig, D, Oltmans, S J, Morse, Thomas O, Dibb, Jack E.
Format: Text
Language:unknown
Published: University of New Hampshire Scholars' Repository 2007
Subjects:
Online Access:https://scholars.unh.edu/earthsci_facpub/242
https://doi.org/10.1016/j.atmosenv.2006.05.084
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spelling ftuninhampshire:oai:scholars.unh.edu:earthsci_facpub-1241 2023-05-15T13:41:56+02:00 What is causing high ozone at Summit, Greenland? Helmig, D Oltmans, S J Morse, Thomas O Dibb, Jack E. 2007-08-01T07:00:00Z text/html https://scholars.unh.edu/earthsci_facpub/242 https://doi.org/10.1016/j.atmosenv.2006.05.084 unknown University of New Hampshire Scholars' Repository https://scholars.unh.edu/earthsci_facpub/242 http://dx.doi.org/10.1016/j.atmosenv.2006.05.084 Copyright © 2007 Published by Elsevier Ltd. Earth Sciences Scholarship Tropospheric ozone Snowpack-atmosphere gas exchange Snow photochemistry Synoptic transport Atmospheric Sciences text 2007 ftuninhampshire https://doi.org/10.1016/j.atmosenv.2006.05.084 2023-01-30T21:34:30Z Causes for the unusually high and seasonally anomalous ozone concentrations at Summit, Greenland were investigated. Surface data from continuous monitoring, ozone sonde data, tethered balloon vertical profiling data, correlation of ozone with the radionuclide tracers 7Be and 210Pb, and synoptic transport analysis were used to identify processes that contribute to sources and sinks of ozone at Summit. Northern Hemisphere (NH) lower free troposphere ozone mixing ratios in the polar regions are ∼20 ppbv higher than in Antarctica. Ozone at Summit, which is at 3212 m above sea level, reflects its altitude location in the lower free troposphere. Transport events that bring high ozone and dry air, likely from lower stratospheric/higher tropospheric origin, were observed ∼40% of time during June 2000. Comparison of ozone enhancements with radionuclide tracer records shows a year-round correlation of ozone with the stratospheric tracer 7Be. Summit lacks the episodic, sunrise ozone depletion events, which were found to reduce the annual, median ozone at NH coastal sites by up to ∼3 ppbv. Synoptic trajectory analyses indicated that, under selected conditions, Summit encounters polluted continental air with increased ozone from central and western Europe. Low ozone surface deposition fluxes over long distances upwind of Summit reduce ozone deposition losses in comparison to other NH sites, particularly during the summer months. Surface-layer photochemical ozone production does not appear to have a noticeable influence on Summit's ozone levels. Text Antarc* Antarctica Greenland University of New Hampshire: Scholars Repository Greenland Atmospheric Environment 41 24 5031 5043
institution Open Polar
collection University of New Hampshire: Scholars Repository
op_collection_id ftuninhampshire
language unknown
topic Tropospheric ozone
Snowpack-atmosphere gas exchange
Snow photochemistry
Synoptic transport
Atmospheric Sciences
spellingShingle Tropospheric ozone
Snowpack-atmosphere gas exchange
Snow photochemistry
Synoptic transport
Atmospheric Sciences
Helmig, D
Oltmans, S J
Morse, Thomas O
Dibb, Jack E.
What is causing high ozone at Summit, Greenland?
topic_facet Tropospheric ozone
Snowpack-atmosphere gas exchange
Snow photochemistry
Synoptic transport
Atmospheric Sciences
description Causes for the unusually high and seasonally anomalous ozone concentrations at Summit, Greenland were investigated. Surface data from continuous monitoring, ozone sonde data, tethered balloon vertical profiling data, correlation of ozone with the radionuclide tracers 7Be and 210Pb, and synoptic transport analysis were used to identify processes that contribute to sources and sinks of ozone at Summit. Northern Hemisphere (NH) lower free troposphere ozone mixing ratios in the polar regions are ∼20 ppbv higher than in Antarctica. Ozone at Summit, which is at 3212 m above sea level, reflects its altitude location in the lower free troposphere. Transport events that bring high ozone and dry air, likely from lower stratospheric/higher tropospheric origin, were observed ∼40% of time during June 2000. Comparison of ozone enhancements with radionuclide tracer records shows a year-round correlation of ozone with the stratospheric tracer 7Be. Summit lacks the episodic, sunrise ozone depletion events, which were found to reduce the annual, median ozone at NH coastal sites by up to ∼3 ppbv. Synoptic trajectory analyses indicated that, under selected conditions, Summit encounters polluted continental air with increased ozone from central and western Europe. Low ozone surface deposition fluxes over long distances upwind of Summit reduce ozone deposition losses in comparison to other NH sites, particularly during the summer months. Surface-layer photochemical ozone production does not appear to have a noticeable influence on Summit's ozone levels.
format Text
author Helmig, D
Oltmans, S J
Morse, Thomas O
Dibb, Jack E.
author_facet Helmig, D
Oltmans, S J
Morse, Thomas O
Dibb, Jack E.
author_sort Helmig, D
title What is causing high ozone at Summit, Greenland?
title_short What is causing high ozone at Summit, Greenland?
title_full What is causing high ozone at Summit, Greenland?
title_fullStr What is causing high ozone at Summit, Greenland?
title_full_unstemmed What is causing high ozone at Summit, Greenland?
title_sort what is causing high ozone at summit, greenland?
publisher University of New Hampshire Scholars' Repository
publishDate 2007
url https://scholars.unh.edu/earthsci_facpub/242
https://doi.org/10.1016/j.atmosenv.2006.05.084
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
genre_facet Antarc*
Antarctica
Greenland
op_source Earth Sciences Scholarship
op_relation https://scholars.unh.edu/earthsci_facpub/242
http://dx.doi.org/10.1016/j.atmosenv.2006.05.084
op_rights Copyright © 2007 Published by Elsevier Ltd.
op_doi https://doi.org/10.1016/j.atmosenv.2006.05.084
container_title Atmospheric Environment
container_volume 41
container_issue 24
container_start_page 5031
op_container_end_page 5043
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