Stratospheric–Tropospheric Exchange of Ozone during February–April 2008 at Eureka University of Western Ontario Environment Canada University of Dalhousie.

Slides:



Advertisements
Similar presentations
LONG-TERM VARIATION OF VERTICAL TURBULENT DIFFUSIVITY IN THE TROPOSPHERE AND LOWER STRATOSPHERE P. Bencze and S. Cseh Geodetic and Geophysical Research.
Advertisements

Meteo 3: Chapter 7 Analyzing weather above Earth’s surface Read: pp (ignore confluence)
ARC-IONS Workshop, U of T – 7-8/01/ ARC-IONS - First results from a North American Strategic Network David W. Tarasick Experimental Studies, Air.
Holger Vömel NCAR Science Day 17 April 2015 Exploration of the tropical tropopause region during Strateole-2.
Variability in Ozone Profiles at TexAQS within the Context of an US Ozone Climatology Mohammed Ayoub 1, Mike Newchurch 1 2, Brian Vasel 3 Bryan Johnson.
Atmospheric conditions associated with high and low summer ozone levels in the lower troposphere over the eastern Mediterranean and ship borne observations.
Validation of Tropospheric Emission Spectrometer (TES) nadir stare ozone profiles using ozonesonde measurements during Arctic Research on the Composition.
Assimilation of TES O 3 data in GEOS-Chem Mark Parrington, Dylan Jones, Dave MacKenzie University of Toronto Kevin Bowman Jet Propulsion Laboratory California.
Distribution of H 2 O and SO 2 in the atmosphere of Venus Yung Y. 1, Zhang X. 1, Liang M.-C. 2 and Parkinson C. 3 1 California Institute of Technology.
Impact of Seasonal Variation of Long-Range Transport on the Middle Eastern O 3 Maximum Jane Liu, Dylan B. Jones, Mark Parrington, Jay Kar University of.
Upper-Level Frontogenesis Cliff Mass University of Washington.
The OQ-Net radar VHF wind profiler network: Comparisons with radiosondes and NWP models Zheng Qi Wang, Mathew Corkum, Shama Sharma, Lisa Alexander, Peter.
Lessons 22,23,24 Upper Level Winds
Wave-critical layer interactions observed using GPS data Bill Randel, NCAR.
Large-scale influences during ACTIVE – Rossby waves and their effects on tropical convection Grant Allen 1 G. Vaughan 1 P. May 2 D. Brunner 3, W. Heyes.
Experiments with WACCM: A sensitivity study. OUTLINE Why is a parameterization of gravity waves important? Middle atmosphere (stratosphere + mesosphere)
Upper-Level Frontogenesis Cliff Mass University of Washington.
Upper-Level Frontogenesis Cliff Mass University of Washington.
Reassessment of Tropospheric Ozone due to Fires/Pollution Stephan Gallagher.
Investigating Stratosphere-Troposphere-Intrusion by Ozonesonde and TES data Huixia He, D.W. Tarasick, W. Hocking Environment Canada University of Western.
This project has been funded with support from the European Commission. IES José Saramago Majadahonda, Spain Menntaskólinn í Kópavogi Kópavogur, Iceland.
Methods Results Abstract Materials References Contributors: Aviance Carter, Marlon Doyle, AveriSeelig, AyannaStukes Dr. Shermane Austin, Dr. Leon Johnson.
Using GPS data to study the tropical tropopause Bill Randel National Center for Atmospheric Research Boulder, Colorado “You can observe a lot by just watching”
Water vapour soundings in the upper troposphere Geraint Vaughan University of Wales, Aberystwyth With thanks to: Clare Cambridge, Alan Phillips, Les Dean,
Vertical Ozone Profiles at TEXAQS 2000 Mike Newchurch 1 2, Mohammed Ayoub 1, Brian Vasel 3 Bryan Johnson 3, Sam Oltmans 3, Richard McNider 1 1. Department.
Boundary layer temperature profile observations using ground-based microwave radiometers Bernhard Pospichal, ISARS 2006 Garmisch-Partenkirchen AMMA - Benin.
AOS 101 Weather and Climate Lisha M. Roubert University of Wisconsin-Madison Department of Atmospheric & Oceanic Sciences.
In Situ Measurements of Ozone during Hibiscus 2004 Contributions through provision of data and discussions: Niels Larsen (DMI ozonesondes) Gerhard Held,
Assessment of SBUV Profile Algorithm Using High Vertical Resolution Sensors Assessment of SBUV Profile Algorithm Using High Vertical Resolution Sensors.
Acoustic-gravity wave monitoring for global atmospheric studies Elisabeth Blanc 1 Alexis Le Pichon 1 Lars Ceranna 2 Thomas Farges 1 2- BGR / B3.11, Hannover,
COST 723 WORKSHOP – SOFIA, BULGARIA MAY 2006 USE OF RADIOSONDE DATA FOR VALIDATION OF REGIONAL CLIMATE MODELLING SIMULATIONS OVER CYPRUS Panos Hadjinicolaou.
Ko pplung von Dy namik und A tmosphärischer C hemie in der S tratosphäre total ozone fluctuations related to different influences Global Maps Mechanisms.
The lower tropospheric ozone increase over the eastern edge of the Indochina Peninsula revealed by ozonesondes at Hanoi, Vietnam Shin-Ya OGINO, Masatomo.
Stratosphere-Troposphere Analyses of Regional Transport (START) Experiment Investigators: Laura Pan (PI) Andy Weinheimer (Integration and Payload) Rushan.
 The atmosphere is a layer of gases that are held in place by earths gravity – called air.  Atmosphere is 78% nitrogen and 21% oxygen.  The atmosphere.
Science applications for EISCAT-3D: possibilities for atmospheric research from the mesosphere down to the troposphere Evgenia Belova, Sheila Kirkwood.
Model evolution of a START08 observed tropospheric intrusion Dalon Stone, Kenneth Bowman, Cameron Homeyer - Texas A&M Laura Pan, Simone Tilmes, Doug Kinnison.
5.32 Estimating regions of tropopause folding and clear-air turbulence with the GOES water vapor channel Tony Wimmers, Wayne Feltz Cooperative Institute.
Infrasound Technology WS – Bermuda, November 6 th, Microbarom signals recorded in Antarctica - a measure for sudden stratospheric warming? L. Ceranna,
Jim Angell’s contributions to understanding the QBO.
Dynamical Impacts of Antarctic Stratospheric Ozone Depletion on the Extratropical Circulation of the Southern Hemisphere Kevin M. Grise David W.J. Thompson.
Mesoscale energy spectra for a simulated squall line Fuqing Zhang Rich Rotunno Y. Qiang Sun Groupmeeting
Inertia-Gravity waves and their role in mixing Geraint Vaughan University of Manchester, UK.
Mesoscale processes in the polar atmosphere – the context Suzanne Gray University of Reading February 2013.
Influence of Lightning-produced NOx on upper tropospheric ozone Using TES/O3&CO, OMI/NO2&HCHO in CMAQ modeling study M. J. Newchurch 1, A. P. Biazar.
ATMOSPHERE OBJECTIVE 1 1.What are the structural components of the
Layers of the Atmosphere 1.  The atmosphere is divided into layers according to major changes in its temperature.  Gravity holds the layers of the atmosphere.
Exercise.04 Receiver functions will be determined Receiver functions will be inverted Receiver functions and surface-wave dispersion will be inverted jointly.
Ch. 1 Review games Quia web Name : firstlast876 Password: student I.D. #
Jonathan Pleim NOAA/ARL* RTP, NC A NEW COMBINED LOCAL AND NON-LOCAL PBL MODEL FOR METEOROLOGY AND AIR QUALITY MODELING * In Partnership with the U.S. Environmental.
UTLS Workshop, NCAR – 20/10/ STT and Tropopause Changes from Radar Windprofilers and Ozonesondes David W. Tarasick Air Quality Research Division,
Atmosphere-ocean interactions Exchange of energy between oceans & atmosphere affects character of each In oceans –Atmospheric processes alter salinity.
Effects of January 2010 stratospheric sudden warming in the low-latitude ionosphere L. Goncharenko, A. Coster, W. Rideout, MIT Haystack Observatory, USA.
Jean-François Lamarque, Peter Hess, Louisa Emmons, and John Gille Figure 2 Days since June CO Mixing ratio (ppbv) See description above. AsiaNorth.
GEO Turbulence Detection: Tropopause Folds and Clear Air Turbulence Tony Wimmers Cooperative Institute for Meteorological Satellite Studies (CIMSS), UW-Madison.
QUANTIFYING BOREAL FIRE & POLLUTION ENHANCEMENT OF THE FREE TROPOSPHERIC OZONE COLUMN DURING THE 2008 ARC-IONS CAMPAIGN Alaina Luzik, Stephan Gallagher,
Andy Delcloo and Hugo De Backer
Static Stability in the Global UTLS Observations of Long-term Mean Structure and Variability using GPS Radio Occultation Data Kevin M. Grise David W.
Seasonal variability of the tropical tropopause dehydration
A New Tropopause Definition for Use in Chemistry-Transport Models
Stratosphere Issues in the CFSR
Constant Pressure Maps
Double tropopauses during idealized baroclinic life cycles
Tony Wimmers, Wayne Feltz
Upper-Level Frontogenesis
Changes in the Free Atmosphere
Lower Tropospheric Frontogenesis
Upper-Level Frontogenesis
Department of Physics and Astronomy, University of Louisville, KY, USA
Comparison of ozone profiles from Broadmeadows and Macquarie Island,
Presentation transcript:

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