Stratospheric–Tropospheric Exchange of Ozone during February–April 2008 at Eureka University of Western Ontario Environment Canada University of Dalhousie ARC-IONS Workshop 7-8 January 2009 ARC-IONS M. Osman, W. Hocking, D.Tarasick, J.Drummond
Outline Background and Motivation Methods Results Future Work ARC-IONS
Background and Motivation Photochemistry is the major source of ozone in the lower troposphere The stratosphere–troposphere exchange of ozone Health issues Economic issues- crop production Global warming ARC-IONS
Detection of Ozone intrusion Source: Hocking et al. (2007)- NATURE Simultaneous radar and ozonesonde measurements from the Montreal Campaign of April–May 2005 This talk examines the detection of stratospheric ozone leakage from the stratosphere to the troposphere Particularly highlighting noticeable differences between February-March and April ARC-IONS
Methods Ozonesondes combined with windprofiler radars Radar analysis software and MATLAB 1 Ozone sensor Styrofoam casing 2 Radiosonde 3 Ozonesonde Interface Board OIF11 4 Ozone sensor Windprofiler radar at Eureka ARC-IONS
Ozone campaign 24 Feb – 18 April 2008 Eureka Ozone variation with height Time series of ozone concentration between ground & 0.5km as well as 0.5km & 1.0km Results ARC-IONS
Ozone plot Red transition to softer colors …noticeable Smeared out A lot more ozone in the upper and middle troposphere High gradients of ozone Sharp cut off ARC-IONS
Was the difference due to ozone concentration just above the tropopause? Was it stratospheric ozone? What happened to tropopause during those periods of time? Wind and turbulence strengths Motivated questions… ARC-IONS
Was the leakage due to high concentration of ozone immediately above the tropopause ? No! ARC-IONS
Was the ozone really stratospheric? Low RH used as a partial indicator of ozone originated from stratosphere Weak gradients of ozone Low humidity… ARC-IONS
Smoothed humidity… ARC-IONS
Ozone & Humidity … Low humidity? Is there a correlation? High tropospheric ozone ARC-IONS
Smoothed one… ARC-IONS
Was the tropopause poorly defined? Gradient of temperature around tropopause is not that weak in Feb – Mar… ARC-IONS
Cont… Gradient of temperature around tropopause is not that weak… ARC-IONS
Turbulence No obvious distinction between the two periods! ARC-IONS
Proxy for gravity wave SD of vertical component of wind Nothing distinct statistically between the two periods! ARC-IONS
Vertical Wind (1-5km) No obvious difference between the two periods!
ARC-IONS Vertical Wind (5-10km) No difference!
Horizontal Wind (1 – 5km) ARC-IONS
Horizontal Wind (5 – 10km) During April 1–13 the wind was blowing northward!
Daily Horizontal Wind (1 – 5km) ARC-IONS
Daily Horizontal Wind (5 – 10km) During the 1 st two weeks of April northward blowing wind quite dominant
Future Work To further analyze the wind and turbulent strengths To simulate the situation using FLEXPART To run photochemical models like GEM- MACH To apply the same procedure for other radar stations and campaigns ARC-IONS
Acknowledgements Prof. Wayne Hocking Prof. David Tarasick University of Western Ontario Environment Canada ARC-IONS Thank you!
Horizontal Wind (5 – 10km) ARC-IONS
Daily Horizontal Wind (5 – 10km) ARC-IONS From 04/01 – 04/13 the wind was blowing northward
Turbulence km ARC-IONS
Turbulence up to 15km ARC-IONS
Horizontal Wind (1 – 5km) Although it isn’t quite dominant the wind was blowing northward!
ARC-IONS Daily Horizontal Wind (1 – 5km) The wind was blowing northward!
Vertical Wind (1-5km) ARC-IONS
Vertical Wind (5-10km) ARC-IONS
Vertical Wind (1-10km) ARC-IONS
Horizontal Wind (1 – 10km) ARC-IONS
Daily Horizontal Wind (1 – 10km) ARC-IONS
Horizontal Wind From 04/01 – 04/13 the wind was blowing northward ARC-IONS
Horizontal Wind… During the 1 st two weeks April northward blowing wind quite dominant Before coming to conclusion we need to look at in more detail ARC-IONS