Arctic Atmospheric Chemistry: the Polar Sunrise Experiments (PSE) Jan W. Bottenheim 1, Paul B. Shepson 2, Jose D. Fuentes 3, Leonard A. Barrie 4 1 Meteorological.

Slides:



Advertisements
Similar presentations
Copyright © 2010 R. R. Dickerson & Z.Q. Li 1 AOSC 620 The Ozone Hole R. Dickerson.
Advertisements

Halogen Oxides in the Troposphere
11 Halogens in the Troposphere AOSC 637 Atmospheric Chemistry Russell R. Dickerson Finlayson-Pitts Chapt. 4,6 Seinfeld Chapt. 6 OUTLINE History & Importance.
3 Dec 2004IUP Heidelberg Reading Group Air-Snow Interactions and Atmospheric Chemistry Florent Domine and Paul B. Shepson, Science, 297, 1506 (2002). Reviewed.
Institute for Climate and Atmospheric Science SCHOOL OF EARTH AND ENVIRONMENT 3D SLIMCAT Studies of Arctic Ozone Loss Wuhu Feng Acknowledgments: Martyn.
Jingqiu Mao, Daniel Jacob, Jenny Fisher, Bob Yantosca, Philippe Le Sager, Claire Carouge Harvard University Bill Brune(Penn State),Ron Cohen(UC Berkeley),
1 Purdue University, West Lafayette IN, USA 2 Meteorological Service of Canada, Toronto, Ontario Canada 3 World Meteorological Organization, Geneva, SW.
Diagnosis of the Ozone Budget in the SH Lower Stratosphere Wuhu Feng and Martyn Chipperfield School of the Environment, University of Leeds, Leeds, UK,
Polar Stratospheric Clouds -Properties and Climate Impacts Haibin Li.
Wuhu Feng and Martyn Chipperfield
METO 621 Lesson 22. Summary of Homogeneous Chemistry.
Atmospheric Heterogeneous Chemistry of HO 2 Joel Thornton and Jonathan Abbatt Department of Chemistry University of Toronto $$ Natural Sciences and Engineering.
METO 637 Lesson 16.
Global 3-D simulation of reactive bromine chemistry T. Canty, Q. Li, R.J. Salawitch Jet Propulsion Laboratory, Caltech, Pasadena CA
1 Global Observations of Sulfur Dioxide from GOME Xiong Liu 1, Kelly Chance 1, Neil Moore 2, Randall V. Martin 1,2, and Dylan Jones 3 1 Harvard-Smithsonian.
Impacts of Climate Change on Physical Systems PPT
This Week—Tropospheric Chemistry READING: Chapter 11 of text Tropospheric Chemistry Data Set Analysis.
CHAPMAN MECHANISM FOR STRATOSPHERIC OZONE (1930) O O 3 O2O2 slow fast Odd oxygen family [O x ] = [O 3 ] + [O] R2 R3 R4 R1.
National Oceanic and Atmospheric Administration Geophysical Fluid Dynamics Laboratory Princeton, NJ Evolution of Stratospheric.
Building a Global Modeling Capability for Mercury with GEOS-CHEM Noelle Eckley Selin, Rokjin J. Park, Daniel J. Jacob Constraining the global budget of.
An Overview Of Arctic Haze And Surface Ozone Depletion At Polar Sunrise Leonard A. Barrie Pacific Northwest National Laboratory
QUESTIONS Based on the major source of OH described last class where do you expect OH formation to be high? 2. The  Chapman mechanism includes a fifth.
Environment Canada Participant Report for IABP-18 Toulouse, June 2008 Edward Hudson Arctic Meteorologist: International Polar Year and Marine.
An overview of mercury speciation measurements and analysis at high latitudes Chris Moore 1, Daniel Obrist 1, Steve Brooks 2, William R. Simpson 3, Peter.
Deriving vertical profiles of free tropospheric trace gases from ground based measurements: Implications for oxidation of atmospheric mercury Sean Coburn.
NEW PERSPECTIVES ON ATMOSPHERIC MERCURY Daniel J. Jacob with Noelle E. Selin and Christopher D. Holmes Supported by NSF, EPA and Sarah Strode and Lyatt.
The polar sea ice covers are large Tens of millions of square kilometers, and empty.
Links between ozone and climate J. A. Pyle Centre for Atmospheric Science, Dept of Chemistry University of Cambridge Co-chair, SAP 7th ORM, Geneva, 19.
QUESTIONS 1.Based on the major source of OH described last class where do you expect OH formation to be high? 2.Why don’t reactions of hydrocarbons deplete.
TRENDS IN ATMOSPHERIC OZONE FROM A LONG-TERM OZONE CLIMATOLOGY Jane Liu 1,2, D. W. Tarasick 3, V. E. Fioletov 3, C. McLinden 3, J. H. Y. Jung 1, T. Zhao.
Global Measurements and Research on Stratospheric Ozone Depletion For The Vienna Convention and Its Protocols: Users, Needs & Requirements Leonard A. Barrie.
ARCTAS BrO Measurements from the OMI and GOME-2 Satellite Instruments
Observations of Formaldehyde and Related Atmospheric Species Using Multi-Axis Spectroscopy Christopher P. Beekman and Dr. Heather C. Allen Department of.
Common ozone depletion myths There is overwhelming evidence that humans are responsible for the Antarctic ozone "hole". And there is strong evidence that.
Global Modeling of Mercury in the Atmosphere using the GEOS-CHEM model Noelle Eckley, Rokjin Park, Daniel Jacob 30 January 2004.
Retrieval and Interpretation of Tropospheric Observations from GOME Randall Martin Daniel Jacob Paul Palmer Sushil Chandra Jerry Ziemke Mian Chin Kelly.
Investigation of air-snow exchanges of mercury: proof of concept for automated gradient sampling of interstitial air at the Summit FLUX facility Xavier.
Research Activities in Japan and other Asian Countries 1. Ground-based observation - AGAGE monitoring stations: China, Korea, and Japan - NDACC stations:
Objective Data  The outlined square marks the area of the study arranged in most cases in a coarse 24X24 grid.  Data from the NASA Langley Research Center.
Jingqiu Mao, Daniel Jacob, Jenny Fisher, Bob Yantosca, Philippe Le Sager, Claire Carouge Harvard University Xinrong Ren(U Miami), Bill Brune(Penn State),
Building a Global Modeling Capability for Mercury with GEOS-CHEM Noelle Eckley Selin EPS Day 12 March 2005.
Why is the photochemistry in Arctic spring so unique? Jingqiu Mao.
1May 14, 2014 Uncertainties in projections of ozone- depleting substances and alternatives Guus Velders The Netherlands (RIVM)
The impact of volcanic aerosols on stratospheric chemistry with implications for geoengineering Simone Tilmes WACCM team, Doug Kinnison,
Model Simulation of tropospheric BrO Xin Yang, J. Pyle and R. Cox Center for Atmospheric Science University of Cambridge 7-9 Oct Frascati, Italy.
GLOBAL MODELING OF MERCURY WITH Br AS ATMOSPHERIC OXIDANT Chris D. Holmes and Daniel J. Jacob and funding from EPRI and NSF.
Oxidant chemistry in the tropical troposphere: role of oxygenated VOCs and halogens, and implications for mercury Daniel J. Jacob with Kevin J. Wecht,
Damaging the Ozone Layer
Halogen Chemistry at NCAR D. Kinnison, J.Orlando, J-F Lamarque, S. Schaffler, G. Brasseur, R. Garcia, et al… NCAR Alfonso Saiz-Lopez and S. Sander JPL.
Climatic implications of changes in O 3 Loretta J. Mickley, Daniel J. Jacob Harvard University David Rind Goddard Institute for Space Studies How well.
Review: Constraining global isoprene emissions with GOME formaldehyde column measurements Shim et al. Luz Teresa Padró Wei-Chun Hsieh Zhijun Zhao.
slide 1 Polar Ozone: Past and present Chapter 4 of WMO 2006 Ozone Assessment Summary Part 1 Polar stratospheric observations update Part 2 Progress.
OCEAN-ATMOSPHERE-ICE (OAII) INTERACTIONS REPORT ARCSS ALL HANDS MEETING SEATTLE FEB L.A. Codispoti and the OAII SSC
Effect of BrO Mixing Height to Ozone Depletion Events Sunny Choi.
OZONE DEPLETION AT POLAR SUNRISE SOURCES AND MECHANISM OF REACTIVE HALOGEN SPECIES EAS6410 Jide & Rita.
Links between ozone and climate 9 th ORM Geneva, 14 May 2014 SAP Co-chairs Ayité-Lô Ajavon (Togo) Paul Newman (USA) John Pyle (UK) A.R. Ravishankara (USA)
The 2003 Wake-up Call: Predictable? “Normal” airmass flow Stagnant airmass flow Jul29-Jul31-Jul 2-Aug 4-Aug 6-Aug8-Aug.
Aerosol Chemical Composition Using Aerosol Mass Spectrometry ASCOS Workshop Landskrona April 9, 2008 R. Chang, J. Abbatt – University of Toronto K. Hayden,
The Collaborative O-Buoy Project: Deployment of a Network of Arctic Ocean Chemical Sensors for the IPY and beyond Patricia Matrai, Bigelow Laboratory for.
Antarctic Ozone Depletion EVSC 1300 Spring Average vertical temperature structure of atmosphere.
Recent achievements and future perspectives in stratospheric research Francesco Cairo, Federico Fierli, Chiara Cagnazzo. Marcel Snels Consiglio Nazionale.
ATS 621 Fall 2012 Lecture 11.
B. Croft1, R. V. Martin1,2, G. R. Wentworth3, W. R. Leaitch4, J. G
Observations of the Arctic boundary layer clouds during ACSE 2014
Ozone.
Anlauf (MSC), Carroll (UM)
North American Hydrocarbon Emissions Measured from Space
Troposphere-to-Stratosphere Transport of VSLS
Ozone.
HO2 O3 NO OH NO2 hv Pyro-convection NOx, RH, CO O3 Visibility
Presentation transcript:

Arctic Atmospheric Chemistry: the Polar Sunrise Experiments (PSE) Jan W. Bottenheim 1, Paul B. Shepson 2, Jose D. Fuentes 3, Leonard A. Barrie 4 1 Meteorological Service of Canada, Toronto, ON, Canada 2 Purdue University, West Lafayette, IN, USA 3 University of Virginia, Charlottesville, VA, USA 4 WMO, Geneva, Switzerland

Chronology of PSEs: 1988: first PSE 1992, 2000: major campaigns Yearly small, dedicated campaigns

Relationship between ozone and bromine From: Barrie et al., 1988

Br +O 3 ->BrO +O 2 BrO +BrO->2 Br +O 2 BrO + BrO limiting BrO +HO 2 ->HOBr HOBr + Br - ->2 Br

From: Foster et al., 2001 From: Hoenninger and Platt, 2002

From: Richter et al., 1998 GOME satellite data

Frequency of depletion episodes is increasing (0.7 % y -1 ), evidence of climate change? Most episodes occur where surface temperature is < C Frost flower growth is efficient over new sea-ice, at a rate inversely proportional to temperature

The HCHO lifetime changes from ~3 months in the dark, to 0.5 days in sunlight From: Sumner and Shepson, 1999

Radical Source HCHO+ h H HO 2 HCHO+ h H HO 2 HO 2 +BrO  HOBr+O 2 HOBr( aq ) + Br - + H +  Br 2 ( aq )  Br 2 ( g ) + h  2 Br Bromine Radical Sink Br+O 3  BrO +O 2 Br+O 3  BrO +O 2 BrO +BrO  2 Br+O 2 Br+ HCHO  HBr+HCO Br+ HCHO  HBr+HCO Role of Formaldehyde in Ozone Destruction

O 3, *20 NO y PAN NO x

Vertical HONO profile at SST, 10:00-14:30, 4/24/ HONO, ppt Height/Depth, cm Courtesy: X. Zhou, SUNYA

Courtesy: Schroeder and Steffen, MSC

Courtesy: Anlauf and Hayden, MSC Similarly, ozone depletion in spring is an annually recurring phenomenon (for a graphic representation contact Dr. K.G. Anlauf at the Meteorological Service of Canada, Toronto, Ontario, Canada)

From: Steffen et al., 2002 TGM at Ice Camp

Height (m) Fuentes, unpublished

From: Albert et al., 2002

Courtesy: Strong and Fuentes

From: Bottenheim et al., 2002

Some future experiments Detailed chemistry profiles of the lower atmosphere (< 100 m) R ole of frost flowers on chemical processing L aboratory experiments devoted to the heterogeneous chemistry on frozen seawater surfaces Other? (discuss at meeting on Saturday evening) Three-dimensional studies to investigate the climate impact of ozone depletion

`