Influence of mountains on Arctic tropospheric ozone
Tropospheric ozone was measured above Ellesmere Island in the Canadian Arctic during spring of 2008 using a differential absorption lidar. The observations were carried out at Eureka Weather Station, which is located between various mountain ranges. Analysis of the observations revealed that mountai...
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| Published in: | Journal of geophysical research. Atmospheres Vol. 121; no. 4; pp. 1935 - 1942 |
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| Language: | English |
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27-02-2016
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| Abstract | Tropospheric ozone was measured above Ellesmere Island in the Canadian Arctic during spring of 2008 using a differential absorption lidar. The observations were carried out at Eureka Weather Station, which is located between various mountain ranges. Analysis of the observations revealed that mountains had a significant effect on the vertical distribution of ozone. Ozone depletion events were observed when air that had spent significant time near to the frozen surface of the Arctic Ocean reached Eureka. This air arrived at Eureka by flowing over the surrounding mountains. Surface level ozone depletions were not observed during periods when mountains blocked the flow of air from over the sea ice. In the case of blocking there was an enhancement in the amount of ozone near the surface as air from the midtroposphere descended in the lee of the mountains. Three case studies from spring of 2008 are described.
Key Points
Differential absorption lidar (DIAL) measurements of Arctic tropospheric ozone
Measurements provide an unprecedented view of variations in arctic ozone near the surface
Mountain blocking of airflow had a significant impact on the vertical distribution of ozone |
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| AbstractList | Tropospheric ozone was measured above Ellesmere Island in the Canadian Arctic during spring of 2008 using a differential absorption lidar. The observations were carried out at Eureka Weather Station, which is located between various mountain ranges. Analysis of the observations revealed that mountains had a significant effect on the vertical distribution of ozone. Ozone depletion events were observed when air that had spent significant time near to the frozen surface of the Arctic Ocean reached Eureka. This air arrived at Eureka by flowing over the surrounding mountains. Surface level ozone depletions were not observed during periods when mountains blocked the flow of air from over the sea ice. In the case of blocking there was an enhancement in the amount of ozone near the surface as air from the midtroposphere descended in the lee of the mountains. Three case studies from spring of 2008 are described. Key Points Differential absorption lidar (DIAL) measurements of Arctic tropospheric ozone Measurements provide an unprecedented view of variations in arctic ozone near the surface Mountain blocking of airflow had a significant impact on the vertical distribution of ozone Tropospheric ozone was measured above Ellesmere Island in the Canadian Arctic during spring of 2008 using a differential absorption lidar. The observations were carried out at Eureka Weather Station, which is located between various mountain ranges. Analysis of the observations revealed that mountains had a significant effect on the vertical distribution of ozone. Ozone depletion events were observed when air that had spent significant time near to the frozen surface of the Arctic Ocean reached Eureka. This air arrived at Eureka by flowing over the surrounding mountains. Surface level ozone depletions were not observed during periods when mountains blocked the flow of air from over the sea ice. In the case of blocking there was an enhancement in the amount of ozone near the surface as air from the midtroposphere descended in the lee of the mountains. Three case studies from spring of 2008 are described. Differential absorption lidar (DIAL) measurements of Arctic tropospheric ozone Measurements provide an unprecedented view of variations in arctic ozone near the surface Mountain blocking of airflow had a significant impact on the vertical distribution of ozone Tropospheric ozone was measured above Ellesmere Island in the Canadian Arctic during spring of 2008 using a differential absorption lidar. The observations were carried out at Eureka Weather Station, which is located between various mountain ranges. Analysis of the observations revealed that mountains had a significant effect on the vertical distribution of ozone. Ozone depletion events were observed when air that had spent significant time near to the frozen surface of the Arctic Ocean reached Eureka. This air arrived at Eureka by flowing over the surrounding mountains. Surface level ozone depletions were not observed during periods when mountains blocked the flow of air from over the sea ice. In the case of blocking there was an enhancement in the amount of ozone near the surface as air from the midtroposphere descended in the lee of the mountains. Three case studies from spring of 2008 are described. Key Points Differential absorption lidar (DIAL) measurements of Arctic tropospheric ozone Measurements provide an unprecedented view of variations in arctic ozone near the surface Mountain blocking of airflow had a significant impact on the vertical distribution of ozone |
| Author | Whiteway, James Seabrook, Jeffrey |
| Author_xml | – sequence: 1 givenname: Jeffrey surname: Seabrook fullname: Seabrook, Jeffrey organization: York University – sequence: 2 givenname: James surname: Whiteway fullname: Whiteway, James organization: York University |
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| Cites_doi | 10.1016/j.jqsrt.2009.02.013 10.2151/jmsj.81.339 10.1029/GL013i002p00113 10.1029/JD091iD04p05229 10.5194/acp-10-7775-2010 10.1364/AO.46.002269 10.1038/334138a0 10.5194/acp-9-4545-2009 10.1029/2011JD016335 10.5194/acp-7-4375-2007 10.5194/acp-13-6023-2013 10.1364/AO.38.004639 |
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| Snippet | Tropospheric ozone was measured above Ellesmere Island in the Canadian Arctic during spring of 2008 using a differential absorption lidar. The observations... |
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| SubjectTerms | Absorption Air Air flow Arctic Arctic ozone Blocking Brackish Case studies Climatology Depletion Differential absorption lidar Distribution Emission measurements Frozen Geophysics Lidar Marine Mountains Ozone Ozone depletion Ozone measurements Sea ice Spring Surface chemistry Troposphere Tropospheric ozone Vertical distribution Weather Weather stations |
| Title | Influence of mountains on Arctic tropospheric ozone |
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