Spring 2001 AGU Meeting Peroxy Radical Distribution During TOPSE and Implications for Ozone Photochemistry Christopher Cantrell and TOPSE Science Team.

Slides:



Advertisements
Similar presentations
Atmospheric chemistry
Advertisements

The activation energy of combined reactions
METO 621 CHEM Lesson 2. The Stratosphere We will now consider the chemistry of the troposphere and stratosphere. There are two reasons why we can separate.
CHAPTER 10: STRATOSPHERIC CHEMISTRY. THE MANY FACES OF ATMOSPHERIC OZONE Troposphere Stratosphere: 90% of total In stratosphere: UV shield In middle/upper.
A study of night-time chemistry of HO x radicals in the Northern and Southern Hemisphere R. Sommariva 1, L. Whitehouse 1, M.J. Pilling 1, W.J. Bloss 1,
METO 621 Lesson 21. The Stratosphere We will now consider the chemistry of the troposphere and stratosphere. There are two reasons why we can separate.
METO 621 Lesson 24. The Troposphere In the Stratosphere we had high energy photons so that oxygen atoms and ozone dominated the chemistry. In the troposphere.
Observations of Total Peroxy Nitrates during TOPSE I. Introduction We present in-situ high time resolution measurements of NO 2 and total peroxynitrate.
Next Two Weeks—Stratospheric Chemistry Mid-latitude Ozone Chemistry (and depletion) Polar Ozone Destruction (the Ozone Hole) READING: Chapter 10 of text.
Gregory R. Carmichael Center for Global and Regional Environmental Research, The University of Iowa, Iowa City, USA Climatic Effects & Air Quality: Aerosol/Chemistry.
Observing the Transition From NO x -Limited to NO x -Saturated O 3 Production J. A. Thornton 1, P. J. Wooldridge 1, R. C. Cohen 1, M. Martinez 2, H. Harder.
METO 637 Lesson 9. Man’s impact on the Stratosphere The concern over a loss of stratospheric ozone is that this will lead to an increase in ultraviolet.
This Week—Tropospheric Chemistry READING: Chapter 11 of text Tropospheric Chemistry Data Set Analysis.
STRATOSPHERIC CHEMISTRY. TOPICS FOR TODAY 1.Review of stratospheric chemistry 2.Recent trends in stratospheric ozone and forcing 3.How will stratospheric.
CHAPMAN MECHANISM FOR STRATOSPHERIC OZONE (1930) O O 3 O2O2 slow fast Odd oxygen family [O x ] = [O 3 ] + [O] R2 R3 R4 R1.
Atmospheric chemistry Day 4 Air pollution Regional ozone formation.
Simple Chemical modeling of ozone sensitivity
QUESTIONS   1. What is the most abundant greenhouse gas in the Earth’s atmosphere?    2. What is the radiative equilibrium temperature of the Earth’s surface.
Fundamentals of air Pollution – Atmospheric Photochemistry – Part B Yaacov Mamane Visiting Scientist NCR, Rome Dec May 2007 CNR, Monterotondo, Italy.
Meteorologisches Observatorium Hohenpeißenberg, Sulfuric acid is a key components in new particle formation in the atmosphere. Nucleation.
Xuexi Tie Xu Tang,Fuhai Geng, and Chunsheng Zhao Shanghai Meteorological Bureau Atmospheric Chemistry Division/NCAR Peking University Understand.
Sensitivity of Methane Lifetime to Sulfate Geoengineering: Results from the Geoengineering Model Intercomparison Project (GeoMIP) Giovanni Pitari V. Aquila,
Outline: 1.Atmospheric Regimes: Scientific Questions & Observational Needs UT/LS (HO x, water ) Middle & Lower Troposphere (clouds, aerosols, NO x, regional.
Urban Air Pollution Public and Environmental Health Concerns –Elevated levels of toxic compounds Regional and Global Impacts –Background Chemistry and.
Spectrometry and Photochemistry Theodore S. Dibble Chemistry Department SUNY-Environmental Science and Forestry Syracuse, NY.
Copyright © 2014 R. R. Dickerson & Z.Q. Li 1 Spectroscopy and Photochemistry AOSC 620 R. Dickerson Fall 2015.
SAMPLE EXERCISE 14.7 Using the Integrated First-Order Rate Law
QUESTIONS 1.What molar fraction of HNO 3 do you expect to partition into fog droplets at room temperature? How does this compare to the fraction that would.
TROPOSPHERIC OZONE AND OXIDANT CHEMISTRY Troposphere Stratosphere: 90% of total The many faces of atmospheric ozone: In stratosphere: UV shield In middle/upper.
Acids and Bases Calculating Excess. Calculations involving strong acids and bases During an experiment, a student pours 25.0 mL of 1.40 mol/L nitric acid.
The Atmosphere as a Chemical Reactor OutputsInputs Chemistry Radiation (energy) Biogeochemical Cycling.
Intermediate model for the annual and global evolution of species
Recent Trend of Stratospheric Water Vapor and Its Impacts Steve Rieck, Ning Shen, Gill-Ran Jeong EAS 6410 Team Project Apr
Basic Chemistry Copyright © 2011 Pearson Education, Inc. 1 Chapter 14 Acids and Bases 14.5 Ionization of Water.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 14: Methane and CO Don Wuebbles Department of Atmospheric Sciences University of Illinois,
TM3 results compared with SONEX observations Ernst Meijer, Michiel van Weele, and Bram Bregman.
2006 Graduate Student Symposium Measurement of HCl (g) in troposphere and lower stratosphere with CIMS technique Analytical characteristics and its implications.
Basic Chemistry Copyright © 2011 Pearson Education, Inc Molarity and Dilution Chapter 12 Solutions.
QUESTIONS 1. If the Earth were twice its distance from the Sun, by how much would its effective temperature decrease? 2. What is the most abundant greenhouse.
Center for Environmental Research and Technology/Environmental Modeling University of California at Riverside Data Needs for Evaluation of Radical and.
Near-Infrared Photochemistry of Atmospheric Nitrites Paul Wennberg, Coleen Roehl, Geoff Blake, and Sergey Nizkorodov California Institute of Technology.
III/1 Atmospheric transport and chemistry lecture I.Introduction II.Fundamental concepts in atmospheric dynamics: Brewer-Dobson circulation and waves III.Radiative.
The regional chemical transport model, STEM, with advanced photochemical modules including SAPRC99 mechanism, KPP chemical solver and explicit photolysis.
METO 621 CHEM Lesson 4. Total Ozone Field March 11, 1990 Nimbus 7 TOMS (Hudson et al., 2003)
Caltech Chemical Ionization Mass Spectrometer (CIMS) Measurements INTEX-NA Data Review John Crounse Alan Kwan Paul Wennberg.
Chemistry: An Introduction to General, Organic, and Biological Chemistry, Eleventh Edition Copyright © 2012 by Pearson Education, Inc. Chapter 8 Acids.
General, Organic, and Biological Chemistry Fourth Edition Karen Timberlake 10.3 Ionization of Water Chapter 10 Acids and Bases © 2013 Pearson Education,
Jingqiu Mao, Daniel Jacob Harvard University Jennifer Olson(NASA Langley), Xinrong Ren(U Miami), Bill Brune(Penn State), Paul Wennberg(Caltech), Mike Cubison(U.
Atmospheric Chemistry of the Ozone Layer. Levels of Atmospheric Ozone have been Dropping NASA -
Atmospheric Processes and Composition:
Workshop on Air Quality Data Analysis and Interpretation
ATS 621 Fall 2012 Lecture 9.
11.5 Dissociation of Water The equilibrium reached between the conjugate acid–base pairs of water produces both H3O+ and OH−. H2O(l) + H2O(l)
Chapter 14 Acids and Bases
Ch Acids & Bases III. Neutralization (p )
Observations of Total Peroxy Nitrates during TOPSE
ATS 621 Fall 2012 Lecture 10.
Snowpack photochemistry - focused on the PAN(Peroxyacetyl Nitrate)
Spectroscopy and Photochemistry
Spectroscopy and Photochemistry
Characteristics of Urban Ozone Formation During CAREBEIJING-2007 Experiment Zhen Liu 04/21/09.
OH/H2SO4 & HO2/RO2 during NOMADSS
12.1/12.2 Equations and Chemical Calculations
Modeling the chemistry during TOPSE low ozone events
Chapter 14 Acids and Bases
大气圈地球化学及其环境效益.
Troposphere The Air We Breath.
The mole ratio.
Mass to Mass Conversions
Chapter 10 Acids and Bases
Presentation transcript:

Spring 2001 AGU Meeting Peroxy Radical Distribution During TOPSE and Implications for Ozone Photochemistry Christopher Cantrell and TOPSE Science Team

Spring 2001 AGU Meeting Outline Description of CIMS peroxy radical measurements Steady-state radical concentrations Budgets of radicals and O 3 during TOPSE Possible role of photochemistry in TOPSE O 3 trends

Spring 2001 AGU Meeting TOPSE in situ O 3

Spring 2001 AGU Meeting TOPSE Steady State HO 2 + RO 2

Spring 2001 AGU Meeting TOPSE Steady State OH

Spring 2001 AGU Meeting TOPSE O( 1 D)+H 2 O Rate

Spring 2001 AGU Meeting TOPSE Temperature

Spring 2001 AGU Meeting CIMS HO 2 and HO 2 +RO 2 Measurements Based on conversion of ambient peroxy radicals to gas-phase H 2 SO 4 –HO 2 + NO  OH + NO 2 –OH + SO 2 (O 2, H 2 O, M)  H 2 SO 4 Chemical ionization – Calibration –Photolysis of water vapor by nm radiation –Lamp flux by N 2 O actinometry

Spring 2001 AGU Meeting CIMS Inlets, rack, C130 photos

Spring 2001 AGU Meeting Steady-State Radical Concentrations Equation for each radical (OH, HO 2, CH 3 O 2 ) – Assume dX/dt << P or L, P-L  0 n equations and n unknowns (radical concentrations) Solve by iterative numerical method (Newton- Raphson). Requires initial estimate. Use measured quantities (NO x,CO, NMHCs, O 3, j- values, etc.) when available in equations Include HNO 4 chemistry (estimate of jHNO 4 ) Two calculations: effective CH 4, explicit treatment of NMHCs (and thus RO 2 )

Spring 2001 AGU Meeting Comparison of measurements and steady-state HO 2 +RO 2

Spring 2001 AGU Meeting TOPSE Measured & SS HO 2 +RO 2

Spring 2001 AGU Meeting TOPSE SS Peroxy Radical Ratios

Spring 2001 AGU Meeting TOPSE HOx Production & Loss

Spring 2001 AGU Meeting TOPSE HO x Production

Spring 2001 AGU Meeting Steady State HO 2 NO 2

Spring 2001 AGU Meeting TOPSE Net O 3 Production and Loss

Spring 2001 AGU Meeting TOPSE Net O 3 Production

Spring 2001 AGU Meeting TOPSE Net O 3 Production

Spring 2001 AGU Meeting Comparison with Other Studies

Spring 2001 AGU Meeting Acknowledgements NCAR –ACD –RAF/ATD NSF TOPSE Colleagues Churchill Airport Thule Air Base