Forma&on and contribu&on of highly oxygenated organic molecules (HOM) to the growth of new par&cles over the boreal forest
|
|
- Letitia Sims
- 5 years ago
- Views:
Transcription
1 Forma&on and contribu&on of highly oxygenated organic molecules (HOM) to the growth of new par&cles over the boreal forest Pontus Roldin Nuclear Physics Lund University, Lund Sweden
2 Model & measurement framework ADCHEM Field measurements (Hyytiälä, Pallas) ADCHAM Chamber exp. (JPAC) ADCHEM; Roldin et al., Atmos. Chem. Phys., 11, , 2011 ADCHAM; Roldin et al., Atmos. Chem. Phys., 14, 14, , 2014
3 Model & measurement framework ADCHEM Field measurements (Hyytiälä, Pallas) Part 1 ADCHAM Chamber exp. (JPAC) ADCHEM; Roldin et al., Atmos. Chem. Phys., 11, , 2011 ADCHAM; Roldin et al., Atmos. Chem. Phys., 14, 14, , 2014
4 Model & measurement framework Part 2 ADCHEM Field measurements (Hyytiälä, Pallas) Part 1 ADCHAM Chamber exp. (JPAC) ADCHEM; Roldin et al., Atmos. Chem. Phys., 11, , 2011 ADCHAM; Roldin et al., Atmos. Chem. Phys., 14, 14, , 2014
5 Formation of Highly Oxygenated Molecules (HOM; O:C 0.7) by autoxidation of monoterpenes (MT) MT C10 H16 + O3!C10 H15 O2 -OO C10 H15 O2 -OO C10 H15 O4 -OO C10 H15 O6 -OO C10 H15 O8 -OO H-shift+O2 H-shift+O2 H-shift+O2 H-shift+O2 (! = 9 % for α-pinene) st C10 H15 O4 -OO (1 H-shift + O2) C10 H15 O6 -OO (2 H-shift + O2) C10 H15 O8 -OO (3 H-shift + O2) C10 H15 O10 -OO (4 H-shift + O2) nd rd th Reactions terminating the autoxidation, leading to formation of stable HOMs: C10 H15 Ox -OO + HO2 C10 H15 Ox -OH C10 H15 Ox -OO +RO2 α C10 H15 Ox -OH + β C10 H14 Ox =O + γ C10 H15 Ox -O + (1-α-β-γ) C20 H30 Ox+4 C10 H15 Ox -OO + NO α C10 H15 Ox -ONO2 + β C10 H14 Ox =O + γ C10 H15 Ox O + (1-α) NO2 + fragmentation prod. C10 H15 Ox OO C10 H15 Ox OH The HOM mechanism comprise 822 reactions and 80 compounds. It keeps the carbon number and mass balance The mechanism is fully coupled to the Master Chemical Mechanism v 3.3.1
6 Highly Oxygenated Molecules contribu6on to SOA forma6on Are HOM Extremely low-vola&lity organic compounds (ELVOC)? Results from Kurtén et al., (J. Phys. Chem A 2016)
7 Highly Oxygenated Molecules contribu6on to SOA forma6on Are HOM Extremely low-vola&lity organic compounds (ELVOC)? ELVOC: p sat <10-9 Pa Results from Kurtén et al., (J. Phys. Chem A 2016)
8 10-50 km Part 2: Implemen&ng the knowledge from the smog chamber experiments into the process-based atmospheric chemistry transport model ADCHEM 2-3 km Wind direction 10 s ADCHEM; Roldin et al., Atmos. Chem. Phys., 11, , 2011
9 10-50 km Part 2: Implemen&ng the knowledge from the smog chamber experiments into the process-based atmospheric chemistry transport model ADCHEM Typically 40 ver&cal layers of which 4 are inside the forest canopy. BVOC emissions from MEGAN or LPJ- Guess. 2-3 km Wind direction 10 s ADCHEM; Roldin et al., Atmos. Chem. Phys., 11, , 2011
10 10-50 km Part 2: Implemen&ng the knowledge from the smog chamber experiments into the process-based atmospheric chemistry transport model ADCHEM Typically 40 ver&cal layers of which 4 are inside the forest canopy. BVOC emissions from MEGAN or LPJ- Guess. 2-3 km The Atmospheric Cluster Dynamics Code (ACDC) is explicitly simula&ng the growth and losses of molecule clusters which lead to new par&cles in the atmosphere. Currently we only consider clusters consis&ng of ammonium and sulfuric acid. Wind direction 10 s ADCHEM; Roldin et al., Atmos. Chem. Phys., 11, , 2011
11 Contribution of HOMs to new particle activation and growth in the atmosphere (Pallas NPF events ) Öström et al., ACP 2017
12 Contribution of HOMs to new particle activation and growth in the atmosphere (Pallas NPF events ): Öström et al., ACP 2017
13 Contribution of HOMs to new particle activation and growth in the atmosphere (Pallas NPF events ): Median particle number size distributions from 10 NPF events at Pallas in northern Finland Öström et al. ACP 2017
14 ADCHEM model simula6ons of NPF and growth at Pallas: Median PN(D p > 50 nm) from 10 NPF events at Pallas in northern Finland Öström et al. ACP 2017
15 Summary and conclusions We have developed a unique HOM gas-phase mechanism and coupled it to Master Chemical Mechanism v3.3.1 The HOM mechanism has been implemented into the process-based chemistry transport model ADCHEM. According to our model simula&ons HOM are crucial for the growth of new par&cles into the cloud condensa&on nuclei (CCN) size range over the sub-arc&c forest region. Over the Boreal forest in Southern Finland the contribu&on of HOM to the number of CCN during a new par&cle forma&on intensive period in Spring 2014 was approximately 15 %.
Supplementary Information for α-pinene Autoxidation. Products May not Have Extremely Low Saturation Vapor
Supplementary Information for α-pinene Autoxidation Products May not Have Extremely Low Saturation Vapor Pressures Despite High O:C Ratios by Theo Kurtén, Kirsi Tiusanen, Pontus Roldin, Matti Rissanen,
More informationDiesel soot aging in urban plumes within hours under cold dark and humid conditions
Supporting information for Diesel soot aging in urban plumes within hours under cold dark and humid conditions A. C. Eriksson 1,2*, C. Wittbom 1, P. Roldin 1,3, M. Sporre 4, E. Öström 1,5, P. Nilsson 2,
More informationThe Sensitivity of Global Nucleation, CCN and Climate to SO2 and Criegee-Intermediate Chemistry
The Sensitivity of Global Nucleation, CCN and Climate to SO2 and Criegee-Intermediate Chemistry Jeff Pierce, Mat Evans, Cat Scott, Steve D'Andrea, Delphine Farmer, Erik Swietlicki and Dom Spracklen Pierce,
More informationEFFECT OF NOX IN THE PHOTOCHEMICAL SYSTEM OF Α-PINENE
EFFECT OF NOX IN THE PHOTOCHEMICAL SYSTEM OF Α-PINENE 12.06.2018 I SUNGAH KANG, THOMAS MENTEL, JÜRGEN WILDT, IIDA PULLINEN MONIKA SPRINGER, SEBASTIAN SCHMITT 1. MOTIVATION Peroxy Radical and Highly Oxidized
More informationSupplementary Figures
1 Supplementary Figures 2 3 4 5 6 7 Supplementary Figure 1. Schematic of the experimental setup. Juelich Plant Atmosphere Chamber (JPAC) is shown. SMPS: scanning mobility particle sizer; CPC: condensation
More informationArctic Chemistry And Climate
21 July 2016 Connaught Summer Institute 1 Arctic Chemistry And Climate Connaught Summer Institute 2016 William (Bill) Simpson Geophysical Institute and Department of Chemistry, University of Alaska Fairbanks
More informationExploring the potential of the nano-köhler theory to describe the growth of atmospheric molecular clusters by organic vapors
Atmos. Chem. Phys. Discuss., https://doi.org/.194/acp-18-393 Exploring the potential of the nano-köhler theory to describe the growth of atmospheric molecular clusters by organic vapors Jenni Kontkanen
More informationLee Mauldin Airmodus University of Helsinki University of Colorado
Nitrate Ion Chemical Ionization Lee Mauldin Airmodus University of Helsinki University of Colorado Co axial Nitrate Ion Chemical Ionization Used extensively for OH, H 2 SO 4, and MSA measurements Ground
More informationUsing COSMOTherm to evaluate properties of atmospheric autoxidation products
Using COSMOTherm to evaluate properties of atmospheric autoxidation products 7 th March 2018 Theo Kurtén Department of Chemistry University of Helsinki, Finland 1 Co-workers and organizations COSMOtherm
More informationSecondary organic aerosol from low-volatility and traditional VOC precursors
Secondary organic aerosol from low-volatility and traditional VOC precursors Havala Olson Taylor Pye 1,2 and John H. Seinfeld 1 1 Department of Chemical Engineering, California Institute of Technology
More informationBiogenic aerosols and their interactions with climate. Yuzhong Zhang
Biogenic aerosols and their interactions with climate Yuzhong Zhang 2011.4.4 Biogenic aerosols and their interactions with climate 1. OVERVIEW OF BIOGENIC AEROSOL Definition and categories Why important?
More informationHighly Oxygenated Organic Molecules (HOM) from Gas-Phase Autoxidation Involving Peroxy Radicals: A Key Contributor to Atmospheric Aerosol
This is an open access article published under a Creative Commons Attribution (CC-BY) License, which permits unrestricted use, distribution and reproduction in any medium, provided the author and source
More informationSupplemental Material for Elemental Composition and Oxidation of Chamber Organic Aerosol
Supplemental Material for Elemental Composition and Oxidation of Chamber Organic Aerosol P. S. Chhabra 1,N.L.Ng 2, M. R. Canagaratna 2, A. L. Corrigan 3, L. M. Russell 3, D. R. Worsnop 2, R. C. Flagan
More informationAtmospheric chemistry Acidification
Atmospheric chemistry Acidification Presented by Pontus Roldin Most material from Erik Swietlicki Avd. för Kärnfysik Fysiska institutionen Lunds universitet Acidification 1 Acidification Sulphur- and nitrogen-containing
More informationAtmosphere Modelling Group
Atmosphere Modelling Group (with a strong focus on new particle formation) University of Helsinki Department of Physics Division of Atmospheric Sciences cm meters kilometers PENCIL- COUD UHMA MALTE SCADIS
More informationSolar eclipse demonstrating the importance of photochemistry in new particle formation
https://helda.helsinki.fi Solar eclipse demonstrating the importance of photochemistry in new particle formation Jokinen, Tuija 2017-04-04 Jokinen, T, Kontkanen, J, Lehtipalo, K, Manninen, H E, Aalto,
More informationChemistry of stabilized Criegee intermediates in the CLOUD chamber
Chemistry of stabilized Criegee intermediates in the CLOUD chamber Nina Sarnela, Mikko Sipilä, Tuija Jokinen, Heikki Junninen, and CLOUD Collaboration Citation: AIP Conference Proceedings 1527, 381 (2013);
More informationGas Particle Partitioning to OA
Gas Particle Partitioning to OA Advanced Atmospheric chemistry CHEM 5152 Prof. J.L. Jimenez Last updated: Spring 2017 1 Gas Phase vs Aerosol Compounds For monofunctional compounds, alkanes beyond C 20
More informationInteractive comment on Reactive uptake of ammonia to secondary organic aerosols: kinetics of organonitrogen formation by Y. Liu et al.
Atmos. Chem. Phys. Discuss., 15, C7412 C7424, 215 www.atmos-chem-phys-discuss.net/15/c7412/215/ Author(s) 215. This work is distributed under the Creative Commons Attribute 3. License. Atmospheric Chemistry
More informationPaul Ziemann Department of Chemistry & CIRES University of Colorado at Boulder
Gas- and Particle-Phase Products and their Mechanisms of Formation from the Reactions of Monoterpenes with N 3 Radicals: Comprehensive Measurements and Modeling Paul Ziemann Department of Chemistry & CIRES
More informationGrowth of atmospheric clusters involving cluster cluster collisions: comparison of different growth rate methods
doi:10.5194/acp-16-5545-2016 Author(s) 2016. CC Attribution 3.0 License. Growth of atmospheric clusters involving cluster cluster collisions: comparison of different growth rate methods Jenni Kontkanen
More informationHelsinki, Finland. 1 Aerodyne Research Inc., Billerica, MA, USA. 2 Chemistry Department, Boston College, Chestnut Hill, MA, USA
Supplementary material to article: Relationship between aerosol oxidation level and hygroscopic properties of laboratory generated secondary organic aerosol (SOA) particles (paper #0GL0 to Geophysical
More informationImpact of new particle formation on the concentrations of aerosols and cloud condensation nuclei around Beijing
! JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116, D19208, doi:10.1029/2011jd016025, 2011!! Impact of new particle formation on the concentrations of aerosols and cloud condensation nuclei around Beijing H.
More informationThe Effect of Future Climate Change on Aerosols: Biogenic SOA and Inorganics
The Effect of Future Climate Change on Aerosols: Biogenic SOA and Inorganics GCAP Phase 2 Science Team Meeting October 12, 2007 Havala O. T. Pye 1, Hong Liao 2, John Seinfeld 1, Shiliang Wu 3, Loretta
More informationBACCHUS. Impact of Biogenic versus Anthropogenic emissions on Clouds and Climate: towards a Holistic UnderStanding. Collaborative Project
BACCHUS Impact of Biogenic versus Anthropogenic emissions on Clouds and Climate: towards a Holistic UnderStanding Collaborative Project SEVENTH FRAMEWORK PROGRAMME ENV.2013.6.1-2 Atmospheric processes,
More informationInfluence of Organic-Containing Aerosols on Marine Boundary Layer Processes
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Influence of Organic-Containing Aerosols on Marine Boundary Layer Processes John H. Seinfeld California Institute of Technology,
More informationMonoterpene and Sesquiterpene Emissions from Ponderosa Pine: Implications for Secondary Organic Aerosol Formation
Monoterpene and Sesquiterpene Emissions from Ponderosa Pine: Implications for Secondary Organic Aerosol Formation Anita Lee, Gunnar Schade, Allen Goldstein UC Berkeley GCEP Workshop: August 19, 2002 What
More informationPutting Secondary Organic Aerosol in Global Models. Issues and Approaches
Putting Secondary Organic Aerosol in Global Models (and FRP s) Issues and Approaches Dean Hegg (University of Washington) Walter Sessions (NRL Monterey) Outline of Talk 1. The necessity of dealing with
More informationEffect of relative humidity on the mechanism of new particle formation from monoterpene oxidation
Effect of relative humidity on the mechanism of new particle formation from monoterpene oxidation James N. Smith, Sabrina Chee (UC Irvine) Xiaoxiao Li, Jiming Hao, Jingkun Jiang (Tsinghua Univ.) Jonathan
More informationChemistry 471/671. Atmospheric Chemistry III: Stratospheric Ozone Depletion
Chemistry 471/671 Atmospheric Chemistry III: Stratospheric Ozone Depletion 2 The Chapman Mechanism O 2 + hn 2 O( 1 D) O( 1 D) + O 2 + M O 3 + M Exothermic O( 1 D) + O 3 2 O 2 O 3 + hn O( 1 D) + O 2 ( 1
More information2. What are the four most common gasses in the atmosphere and their percentages?
Meteorology Review Directions: Answer the following open ended review questions. Utilize a diagram where appropriate and do make sure that you label and describe the drawing. Atmospheric Composition 1.
More informationAerodyne Chinese AMS/ACSM Clinic, Nanjing, April Why are we here? Data Analysis Clinics Boulder, PSI. Barcelona, Boulder
Aerodyne Chinese AMS/ACSM Clinic, Nanjing, 20-22 April 2018 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 2014 2015 2016 2017 1st/2nd AMS Users Meeting Portland / Aerodyne 3rd Aerodyne
More informationInteractive comment on Volatility and hygroscopicity of aging secondary organic aerosol in a smog chamber by T. Tritscher et al.
Atmos. Chem. Phys. Discuss., 11, C2397 C2406, 2011 www.atmos-chem-phys-discuss.net/11/c2397/2011/ Author(s) 2011. This work is distributed under the Creative Commons Attribute 3.0 License. Atmospheric
More informationOxidation Chemistry and Evolving Volatility of Organic Aerosol
Oxidation Chemistry and Evolving Volatility of Organic Aerosol Neil M. Donahue Carnegie Mellon University Center for Atmospheric Particle Studies US - Nordic Workshop on Secondary Organic Aerosols 2 Jul
More informationAn annual cycle of size-resolved aerosol hygroscopicity at a forested site in Colorado
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 117,, doi:10.1029/2011jd016854, 2012 An annual cycle of size-resolved aerosol hygroscopicity at a forested site in Colorado E. J. T. Levin, 1 A. J. Prenni, 1 M. D.
More informationParameterization of the nitric acid effect on CCN activation
Atmos. Chem. Phys., 5, 879 885, 25 SRef-ID: 168-7324/acp/25-5-879 European Geosciences Union Atmospheric Chemistry and Physics Parameterization of the nitric acid effect on CCN activation S. Romakkaniemi,
More informationNO X emissions, isoprene oxidation pathways, and implications for surface ozone in the Southeast United States
NO X emissions, isoprene oxidation pathways, and implications for surface ozone in the Southeast United States Katherine (Katie) Travis CMAS 216: 1/26/16 Co-authors: D. J. Jacob, J. A. Fisher, P. S. Kim,
More informationScience Ques*on 3: Cloud Processing Impacts on Aerosol
Science Ques*on 3: Cloud Processing Impacts on Aerosol How does liquid-cloud-water-mediated processing modify the par8cle size distribu8on, organic mass loading, oxida8on state, O:C ra8o, mixing state,
More informationEquilibration timescale of atmospheric secondary organic aerosol partitioning
GEOPHYSICAL RESEARCH LETTERS, VOL. 39,, doi:10.1029/2012gl054008, 2012 Equilibration timescale of atmospheric secondary organic aerosol partitioning Manabu Shiraiwa 1 and John H. Seinfeld 1 Received 25
More informationBST 200 Radia+ve forcing and Greenhouse Gases
BST 200 Radia+ve forcing and Greenhouse Gases Atmospheric Burden and Residence Time suppose a tub holds 100 kg of water (Burden) and Source = Sink = 5 kg/minute Residence +me = 100 kg 5 kg/minute = 20
More informationOne year boundary layer aerosol size distribution data from five nordic background stations
Atmos. Chem. Phys., 3, 2183 225, 23 Atmospheric Chemistry and Physics One year boundary layer aerosol size distribution data from five nordic background stations P. Tunved 1, H.-C. Hansson 1, M. Kulmala
More informationThe regional distribution characteristics of aerosol optical depth over the Tibetan Plateau
The regional distribution characteristics of aerosol optical depth over the Tibetan Plateau C. Xu, Y. M. Ma, CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences xuchao@itpcas.ac.cn
More informationSTUDY OF AIR IONS AND NANOMETER PARTICLES IN THE ATMOSPHERE DURING NUCLEATION BURST EVENTS
STUDY OF AIR IONS AND NANOMETER PARTICLES IN THE ATMOSPHERE DURING NUCLEATION BURST EVENTS U. HÕRRAK 1,2, H. TAMMET 1, P.P. AALTO 2, L. LAAKSO 2 and M. KULMALA 2 1 Institute of Environmental Physics, University
More informationControls on O 3 and SOA production in wildfire plumes (and how to model them)
Controls on O 3 and SOA production in wildfire plumes (and how to model them) M. J. Alvarado 1, D. A. Jaffe 2, C. R. Lonsdale 1, N. L. Wigder 2, P. Baylon 2, R. J. Yokelson 3, K. Travis 4, E. V. Fischer
More informationATOC 3500/CHEM 3151 Air Pollution Chemistry Lecture 1
ATOC 3500/CHEM 3151 Air Pollution Chemistry Lecture 1 Note Page numbers refer to Daniel Jacob s online textbook: http://acmg.seas.harvard.edu/publications/ jacobbook/index.html Atmos = vapor + sphaira
More informationThe reaction of Criegee Intermediates with NO, RO 2, and SO 2, and their fate in the atmosphere. - Supporting Information -
The reaction of Criegee Intermediates with NO, RO 2, and SO 2, and their fate in the atmosphere. - Supporting Information - L. Vereecken, H. Harder and A. Novelli Table of content p. 2 : Loss process contributions
More informationOn Stationary state, also called steady state. Lifetimes and spatial scales of variability
On sources and sinks ATOC 3500/CHEM 3151 Week 5-6 Additional Notes February 16/18, 2016 On lifetimes, variability, and models On Stationary state, also called steady state Lifetimes and spatial scales
More informationAtmospheric New Particle Formation and Climate Sensitivity: the CLOUD experiment.
Atmospheric New Particle Formation and Climate Sensitivity: the CLOUD experiment 4th April 2017 Molteni Ugo ugo.molteni@psi.ch About me Master degree in Applied and Environmental Chemistry at the University
More informationThe size-dependent charge fraction of sub-3-nm particles as a key diagnostic of competitive nucleation mechanisms under atmospheric conditions
The size-dependent charge fraction of sub-3-nm particles as a key diagnostic of competitive nucleation mechanisms under atmospheric conditions Fangqun Yu 1 and Richard Turco 2 1 Atmospheric Sciences Research
More informationSurface Ozone Problem in Two Polluted Regions in China and VOGA-NCP 2013 Summer Campaign
Surface Ozone Problem in Two Polluted Regions in China and VOGA-NCP 2013 Summer Campaign Liang Ran Key Laboratory of Middle Atmosphere and Global Environment Observation (LAGEO) Institute of Atmospheric
More informationResponse: Changes in the manuscript: Response
We would like to thank the referee for providing valuable comments on our manuscript and we have carefully addressed the referee s comments point-by-point as follows (referee s comments in black and our
More informationON THE GROWTH OF ATMOSPHERIC NANOPARTICLES BY ORGANIC VAPORS
UNIVERSITY OF HELSINKI REPORT SERIES IN PHYSICS HU-P-D208 ON THE GROWTH OF ATMOSPHERIC NANOPARTICLES BY ORGANIC VAPORS TAINA YLI-JUUTI Division of Atmospheric Sciences Department of Physics Faculty of
More informationChapter Eight: Conclusions and Future Work
2004 PhD Thesis 202 Chapter Eight: Conclusions and Future Work 8.1 Conclusions The Aerodyne aerosol mass spectrometer is capable of providing quantitative information on the chemical composition of the
More informationComposition and temporal behavior of ambient ions in the boreal forest
Composition and temporal behavior of ambient ions in the boreal forest M. Ehn 1, H. Junninen 1, T. Petäjä 1, T. Kurtén 1, V.-M. Kerminen 1,2, S. Schobesberger 1, H. E. Manninen 1, I. K. Ortega 1, H. Vehkamäki
More informationSupplement of Temporal variability and sources of VOCs in urban areas of the eastern Mediterranean
Supplement of Atmos. Chem. Phys., 1, 1 1, 1 http://www.atmos-chem-phys.net/1/1/1/ doi:1.19/acp-1-1-1-supplement Author(s) 1. CC Attribution. License. Supplement of Temporal variability and sources of VOCs
More informationSources, sinks and transformation of BVOCs and aerosols in boreal forest boundary layer
REPORT SERIES IN AEROSOL SCIENCE N:o 210 (2018) Sources, sinks and transformation of BVOCs and aerosols in boreal forest boundary layer Putian Zhou Institute for Atmospheric and Earth System Research/Physics,
More informationEffect of solubility limitation on hygroscopic growth and cloud drop activation of SOA particles produced from traffic exhausts
Journal of Atmospheric Chemistry (208) 75:359 383 https://doi.org/0.007/s0874-08-9380-5 Effect of solubility limitation on hygroscopic growth and cloud drop activation of SOA particles produced from traffic
More informationDust in the Earth System EESC G9910
Dust in the Earth System EESC G9910 Chemical transforma0ons in the atmosphere and deposi0on Jean Guo 2/10/2016 Impact of air pollu
More informationTropospheric OH chemistry
Tropospheric OH chemistry CO Oxidation mechanism: CO + OH CO 2 + H, H + O 2 + M HO 2 + M, HO 2 + NO OH + NO 2 NO 2 + hν (+O 2 ) NO + O 3 Initiation step Propagation Net: CO + 2 O 2 CO 2 + O 3 HO 2 + HO
More informationRecent anthropogenic increases in SO2 from Asia have minimal impact on stratospheric aerosol
!1 Recent anthropogenic increases in SO2 from Asia have minimal impact on stratospheric aerosol Ryan R. Neely III (NCAR/ASP), O. Brian Toon, Susan Solomon, Karen H. Rosenlof, John S Daniel, J. English,
More informationThe connection between cosmic rays, clouds and climate
The connection between cosmic rays, clouds and climate Martin Enghoff, Jacob Svensmark, Nir Shaviv* and Henrik Svensmark, National Space Institute of Denmark *University of Jerusalem The connection between
More information0. Background Knowledge
0-1 0. Background Knowledge ME 200 builds on courses you have already taken, including CHEM 115, MATH 165 and 166, and PHYS 172 and 241. You should have the following material at immediate recall. 0.1
More informationProcesses Controlling Arc/c Aerosol Number and Size
Processes Controlling Arc/c Aerosol Number and Size ICG7 Mee/ng May 4, 2015 B. Cro: 1, J.R. Pierce 2, G. Wentworth 3, J. Murphy 3, W.R. Leaitch 4, J. Kodros 2, J. AbbaK 3, R. Mar/n 1,5 1 Dalhousie University,
More informationSupplement of Observation of isoprene hydroxynitrates in the southeastern United States and implications for the fate of NO x
Supplement of Atmos. Chem. Phys., 15, 11257 11272, 2015 http://www.atmos-chem-phys.net/15/11257/2015/ doi:10.5194/acp-15-11257-2015-supplement Author(s) 2015. CC Attribution 3.0 License. Supplement of
More informationAerosols-Cloud-Precipitation Interactions in the Climate System. Meinrat O. Andreae Max Planck Institute for Chemistry Mainz, Germany
Aerosols-Cloud-Precipitation Interactions in the Climate System Meinrat O. Andreae Max Planck Institute for Chemistry Mainz, Germany The global annual mean Earth s energy budget for 2000-2004 (W m 2 ).
More informationComprehensive analysis of particle growth rates from nucleation mode to cloud condensation nuclei in Boreal forest
Atmos. Chem. Phys. Discuss., https://doi.org/.194/acp-18-169 Comprehensive analysis of particle growth rates from nucleation mode to cloud condensation nuclei in Boreal forest Pauli Paasonen 1, Maija Peltola
More informationCHEM J-5 June 2014
CHEM1101 2014-J-5 June 2014 The molecular orbital energy level diagrams for H 2, H 2 +, H 2 and O 2 are shown below. Fill in the valence electrons for each species in its ground state and label the types
More informationThe Atmosphere. Topic 3: Global Cycles and Physical Systems. Topic 3: Global Cycles and Physical Systems. Topic 3: Global Cycles and Physical Systems
The Atmosphere 1 How big is the atmosphere? Why is it cold in Geneva? Why do mountaineers need oxygen on Everest? 2 A relatively thin layer of gas over the Earths surface Earth s radius ~ 6400km Atmospheric
More informationAerosol Effects on Water and Ice Clouds
Aerosol Effects on Water and Ice Clouds Ulrike Lohmann Department of Physics and Atmospheric Science, Dalhousie University, Halifax, N. S., Canada Contributions from Johann Feichter, Johannes Hendricks,
More informationSupplement of Constraining uncertainties in particle-wall deposition correction during SOA formation in chamber experiments
Supplement of Atmos. Chem. Phys., 17, 2297 2310, 2017 http://www.atmos-chem-phys.net/17/2297/2017/ doi:10.5194/acp-17-2297-2017-supplement Author(s) 2017. CC Attribution 3.0 License. Supplement of Constraining
More informationInfluence of Biogenic VOCs on Photooxidant Formation: Simulation Experiments in EUPHORE and Comparison with Model Calculations
Introduction Influence of Biogenic VOCs on Photooxidant Formation: Simulation Experiments in EUPHORE and Comparison with Model Calculations Fraunhofer Institut Atmosphärische Umweltforschung, IFU Kreuzeckbahnstr.
More informationTananyag fejlesztés idegen nyelven
Tananyag fejlesztés idegen nyelven Prevention of the atmosphere KÖRNYEZETGAZDÁLKODÁSI AGRÁRMÉRNÖKI MSC (MSc IN AGRO-ENVIRONMENTAL STUDIES) Fundamentals to atmospheric chemical reactions. The stratospheric
More informationNATS 101 Section 13: Lecture 31. Air Pollution Part II
NATS 101 Section 13: Lecture 31 Air Pollution Part II Last time we talked mainly about two types of smog:. 1. London-type smog 2. L.A.-type smog or photochemical smog What are the necessary ingredients
More informationGas/particle partitioning of water-soluble organic aerosol in Atlanta
Atmos. Chem. Phys., 9, 3613 3628, 09 www.atmos-chem-phys.net/9/3613/09/ Author(s) 09. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics Gas/particle
More informationDeveloping Reactivity- and Source-Based Monoterpene Parameterizations for SOA Modeling
Kelley Barsanti, Isaac Afreh, Jia Jiang Chemical & Environmental Engineering/CE-CERT Developing Reactivity- and Source-Based Monoterpene Parameterizations for SOA Modeling Overview of SOA Formation 2.
More informationContribution of SOA to Ambient PM 2.5 Organic Carbon in Eastern United States Locations
Contribution of SOA to Ambient PM 2.5 Organic Carbon in Eastern United States Locations Tadeusz E. Kleindienst 1, Edward O. Edney 1, Michael Lewandowski 1, John H. Offenberg 1, and Mohammed Jaoui 2 1 National
More informationModelling the formation of organic particles in the atmosphere
Atmos. Chem. Phys., 4, 1071 1083, 2004 SRef-ID: 1680-7324/acp/2004-4-1071 Atmospheric Chemistry and Physics Modelling the formation of organic particles in the atmosphere T. Anttila 1,2, V.-M. Kerminen
More informationSemi-volatile and highly oxygenated gaseous and particulate organic compounds observed above a boreal forest canopy
Semi-volatile and highly oxygenated gaseous and particulate organic compounds observed above a boreal forest canopy Ben H. Lee 1, Felipe D. Lopez-Hilfiker 1,, Emma L. D Ambro 1, Putian Zhou 2, Michael
More informationThe Atmosphere. All of it. In one hour. Mikael Witte 10/27/2010
The Atmosphere All of it. In one hour. Mikael Witte 10/27/2010 Outline Structure Dynamics - heat transport Composition Trace constituent compounds Some Atmospheric Processes Ozone destruction in stratosphere
More informationNew particle formation during α- and β-pinene oxidation by O 3, OH and NO 3, and the influence of water vapour: particle size distribution studies
Atmos. Chem. Phys., 2, 183 196, 2002 Atmospheric Chemistry and Physics New particle formation during α- and β-pinene oxidation by O 3, OH and NO 3, and the influence of water vapour: particle size distribution
More informationAQRP WORKSHOP. Update and evaluation of model algorithms needed to predict Particulate Matter from Isoprene. William Vizuete Jason Surratt
AQRP WORKSHOP Update and evaluation of model algorithms needed to predict Particulate Matter from Isoprene William Vizuete Jason Surratt Isoprene-Derived Epoxides Promote SOA Formation [Paulot et al.,
More informationAtmospheric Chemistry and Physics
Atmos. Chem. Phys., 8, 6681 6698, 28 www.atmos-chem-phys.net/8/6681/28/ Author(s) 28. This work is distributed under the Creative Commons Attribution 3. License. Atmospheric Chemistry and Physics Technical
More informationRegions of the Atmosphere
Regions of the Atmosphere Thermosphere Mesosphere Stratosphere Troposphere Earth Troposphere: 0 15 km; layer of the atmosphere in which we live Stratosphere: 15 50 km; contains ozone layer Mesosphere:
More informationUpdated H 2 SO 4 -H 2 O binary homogeneous nucleation look-up tables
Click Here for Full Article JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113,, doi:10.1029/2008jd010527, 2008 Updated H 2 SO 4 -H 2 O binary homogeneous nucleation look-up tables Fangqun Yu 1 Received 2 June
More informationAtmos. Chem. Lecture 12, 10/21/13: Atmospheric organic chemistry (intro!)
Atmos. Chem. Lecture 12, 10/21/13: Atmospheric organic chemistry (intro!) lareth: Measurement networks H + alkanes: New branch points ther oxidants, hydrocarbons Implicatons for H x PSet 3 due Wed 10/23;
More informationThe Atmospheric Chemistry and Physics of Ammonia
The Atmospheric Chemistry and Physics of Ammonia Russell Dickerson Dept. Meteorology, The University of Maryland Presented at the National Atmospheric Deposition Program Ammonia Workshop October 23, 2003
More informationFinal Exam: Monday March 17 3:00-6:00 pm (here in Center 113) Slides from Review Sessions are posted on course website:
Final Exam: Monday March 17 3:00-6:00 pm (here in Center 113) 35% of total grade Format will be all multiple choice (~70 questions) Final exam will cover entire course - material since 2 nd midterm weighted
More informationEffect of aging on cloud nucleating properties of atmospheric aerosols
Effect of aging on cloud nucleating properties of atmospheric aerosols Yan Ma Nanjing University of Information Science & Technology The 1st Regional GEOS-Chem Asia Meeting 2015 年 5 月 8 日 Indirect effect
More informationElectronic supplementary information to Heterogeneous OH oxidation. of biomass burning organic aerosol surrogate compounds: Assessment
Electronic supplementary information to Heterogeneous OH oxidation of biomass burning organic aerosol surrogate compounds: Assessment of volatilisation products and the role of OH concentration on the
More informationChemistry-Part 1. Inside the Atom
ChemistryPart 1 Inside the Atom What is an Atom? Matter is anything that takes up space and has mass. Matter is made up of atoms. Atoms: the smallest unit into which matter can be divided building blocks
More informationPhase State and Physical Properties of Ambient and Laboratory. Generated Secondary Organic Aerosol
1 2 Phase State and Physical Properties of Ambient and Laboratory Generated Secondary Organic Aerosol 3 4 5 6 7 8 9 10 11 Rachel E. O Brien, 1, 2* Alexander Neu, 1 Scott A. Epstein, 3 Amanda C. MacMillan,
More informationThe contribution of boundary layer nucleation events to total particle concentrations on regional and global scales
Author(s) 2006. This work is licensed under a Creative Commons License. Atmospheric Chemistry and Physics The contribution of boundary layer nucleation events to total particle concentrations on regional
More informationA combined photochemistry/aerosol dynamics model: model development and a study of new particle formation
BOREAL ENVIRONMENT RESEARCH : 55 5 ISSN 9-695 Helsinki December 5 5 A combined photochemistry/aerosol dynamics model: model development and a study of new particle formation Alf Grini )), Hannele Korhonen
More informationResponse to Reviewer s comments
Response to Reviewer s comments (MS Ref. No.: acp-2010-98): Long-term record of aerosol optical properties and chemical composition from a high-altitude site (Manora Peak) in Central Himalaya by K. Ram
More informationSteve McMillan. Drexel University Philadelphia
Steve McMillan Drexel University Philadelphia Josh Wall Mordecai-Mark Mac Low Ralf Klessen Simon Portegies Zwart (Drexel) (AMNH) (Heidelberg) (Leiden) Astrophysical Context Eva Grebel s list test model
More informationIncorporating Space-borne Observations to Improve Biogenic Emission Estimates in Texas (Project )
Incorporating Space-borne Observations to Improve Biogenic Emission Estimates in Texas (Project 14-017) Arastoo Pour Biazar, Richard T. McNider, Andrew White University of Alabama in Huntsville Daniel
More informationCharged and total particle formation and growth rates during EUCAARI 2007 campaign in Hyytiälä
Atmos. Chem. Phys., 9, 4077 4089, 2009 Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics Charged and total particle formation
More informationSOAS 2013: Tower & chamber working group
SOAS 2013: Tower & chamber working group SOAS Coordination Meeting Paul Wennberg, presenting March 13, 2013 Gas-phase chemistry and SOAS Overarching Goal: Tie the emissions of BVOC and NOx to the formation
More informationRules for Assigning Oxidation Numbers. 1. The oxidation number of an element in any elementary substance is zero.
Rules for Assigning Oxidation Numbers 1. The oxidation number of an element in any elementary substance is zero. For example, the oxidation number of chlorine in Cl 2, phosphorus in P 4, and sulfur in
More informationDEVELOPMENT, EXTENSION AND VALIDATION OF (THEORY-BASED) SARS DECEMBER 2018 I LUC VEREECKEN
DEVELOPMENT, EXTENSION AND VALIDATION OF (THEORY-BASED) SARS DECEMBER 2018 I LUC VEREECKEN THE NEED FOR DATABASES AND SARS Models for atmospheric chemistry are ever more complex - Air quality : more, and
More information