Composition and optical properties of secondary organic aerosol particles

Size: px
Start display at page:

Download "Composition and optical properties of secondary organic aerosol particles"

Transcription

1 Concordia University - Portland From the SelectedWorks of Matthew E. Wise November, 2014 Composition and optical properties of secondary organic aerosol particles Felisha Imholt, Concordia University - Portland Ryan Caylor, Concordia University - Portland Matthew E. Wise, Concordia University - Portland John Shilling, Pacific Northwest National Laboratory Available at:

2 Felisha Imholt 1, Ryan Caylor 1, Matthew Wise 1 and John Shilling 2 1 Math and Science Department, Concordia University, Portland, OR 2 Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA

3

4 IPCC 2013: Climate Change 2013: The Physical Science Basis

5 Black Carbon (BC) Optical properties fairly well known Absorb wavelengths above ~500 nm Brown Carbon (BrC) Optical properties not as well known as BC Different in nature than BC Absorbs at ~300 to 500 nm Secondary Organic Aerosols (SOA) could be a form of BrC Absorbs between ~300 to 500 nm

6 What is the chemical composition of SOA? Does SOA absorb UV/Vis radiation? If SOA does absorb UV/Vis radiation, how strong of an absorber is it?

7 10.6 m 3 Teflon chamber 25 o C, 0% RH UV blacklights (340 nm) 1,2,4 trimethylbenzene (TMB (g)) NaNO 2 (aq) H 2 SO 4 (aq) Creates gas phase OH and NO radicals after lights are turned on pump 9 L/min ~3-4 hrs SOA Teflon filter Possible product Liu et al. (2012)

8 Chemistry is complicated and not well known Xu, L. et al. (2014)

9

10 Responsible for light absorption? Absorbance (arbitrary units) Wavenumbers (cm -1 )

11 New research question?

12 Absorbance (arbitrary units) Day 1 Day Wavenumbers (cm -1 )

13 Absorbance (arbitrary units) 1 hr. 26 hrs. 82 hrs. 111 hrs Wavenumbers (cm -1 )

14 1 hour compared to 111 hours Absorbance (arbitrary units) <30 % decrease 6% 4% increase 300 % 152 % Wavenumbers (cm -1 )

15 Integration (Arbitrary units) Days in Storage

16

17 UV/Vis light source Liquid Waveguide Capillary Cell (LWCC) UV/Vis Spectrometer Light in Light out Instruments Light source - Ocean Optics Inc. model DT- MINI-2-GS LWCC - World Precision Instruments model LWCC-3100 Spectrometer - Ocean Optics, Inc. Jaz model UX Sample in Sample out

18 Solvent Amount FA Amount solvent Final Concentration Water g 50.5 g 120 mg/l

19 Mass Specific Absorption Cross-Section (MAC) MAC allows comparison between samples at different concentrations AA MMMMMM UUUU/VVVVVV = [SSSSSS] ee xx LL Imaginary Refractive Index (k) kk = MMMMMM xx λλλλ MAC and k values of SOA will be used in climate models 4ππ System MAC (m 2 /g) k FA/H 2 O 0.15 ± ± Literature FA/H 2 O MAC = 0.17 m 2 /g Ghabbour, E. A. & Davies, G. (2009)

20

21 UV/Vis Spectrometry UV/Vis technique was optimized for water MAC and k values of FA are consistent with the literature values Specific types of SOA absorb radiation (between 350 and 600 nm) more strongly than FA IR Spectrometry Chemical composition of SOA very complicated and not fully elucidated by IR spectra SOA exhibited significant compositional changes during sample storage New research question: How does sample storage effect light absorbance?

22 Determination of the SOA chemical composition necessary to absorb more UV/Vis radiation than fulvic acid Determination of the effect storage time has on SOA composition and its resulting UV/Vis absorbance Studying the effects different precursors have on the composition and absorbance of SOA

23 Dr. Matthew Wise Dr. John Shilling PNNL Visiting Faculty Program Concordia University

24 IPCC, 2013: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 1535 pp. Ghabbour, E. A. & Davies, G. (2009). Spectrophotometric analysis of fulvic acid solutions - A second look. Annals of Environmental Science: 3(10). Liu, S., Shilling, J., Song, C., Hiranuma, N., Zaveri, R., & Russell, L. (2012). Hydrolysis of Organonitrate Functional Groups in Aerosol Particles. Aerosol Science and Technology, 46(12), Xu, L., Kollman, M. S., Song, C., Shilling, J. E., & Ng, N. L. (2014). Effects of NOx on the volatility of secondary organic aerosol from isoprene photooxidation. Environmental Science & Technology, 48(4), doi: /es

Determination of the optical properties of secondary organic aerosol particles

Determination of the optical properties of secondary organic aerosol particles Determination of the optical properties of secondary organic aerosol particles Abstract The enhanced greenhouse effect is currently considered to be our most important global environmental problem. While

More information

Imholt 1. Optical properties of secondary organic aerosols using ultraviolet/visible spectroscopy. Felisha Imholt

Imholt 1. Optical properties of secondary organic aerosols using ultraviolet/visible spectroscopy. Felisha Imholt Imholt 1 Optical properties of secondary organic aerosols using ultraviolet/visible spectroscopy Felisha Imholt Imholt 2 I. ABSTRACT It is well known that the increased warming effect due to greenhouse

More information

GEOL 437 Global Climate Change 5/1/18: Climate sensitivity

GEOL 437 Global Climate Change 5/1/18: Climate sensitivity GEOL 437 Global Climate Change 5/1/18: Climate sensitivity How sensitive is the climate to external radiative forcing? FAQ 12.3 Fig 1 in: Collins, M., R. Knutti, J. Arblaster, J.- L. Dufresne, T. Fichefet,

More information

Trend of Annual One-Day Maximum Rainfall Series over South India

Trend of Annual One-Day Maximum Rainfall Series over South India Trend of Annual One-Day Maximum Rainfall Series over South India Dr. Ashoke Basistha Hydrologist Dam Rehabilitation & Improvement Project 1 st National Dam Safety Conference, Chennai 2 Organization Introduction

More information

Global warming Summary evidence

Global warming Summary evidence Global warming Summary evidence Learning goals Observations of global temperature change How/why we can be confident in the results Difference between forcing and response Notion of an interaction The

More information

Determination of total peroxide content in secondary organic aerosol particles

Determination of total peroxide content in secondary organic aerosol particles Determination of total peroxide content in secondary organic aerosol particles Abstract Secondary organic aerosol particles (SOA) formed from the oxidation of monoterpenes can impact the Earth s radiation

More information

Determining the Optical Properties of Secondary Organic Aerosols using UV-Vis Spectroscopy

Determining the Optical Properties of Secondary Organic Aerosols using UV-Vis Spectroscopy Determining the Optical Properties of Secondary Organic Aerosols using UV-Vis Spectroscopy A senior thesis submitted to The Department of Math-Science College of Theology, Arts, & Sciences In partial fulfillment

More information

Twenty-five winters of unexpected Eurasian cooling unlikely due to Arctic sea-ice loss

Twenty-five winters of unexpected Eurasian cooling unlikely due to Arctic sea-ice loss SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO2820 Twenty-five winters of unexpected Eurasian cooling unlikely due to Arctic sea-ice loss Kelly E. McCusker 1,2, John C. Fyfe 2 & Michael Sigmond 2 1 School

More information

3.1. The Climatological Relation Between Extreme Precipitable Water Vapor (PWV) and Precipitation for the September 2013 Colorado Flooding Event

3.1. The Climatological Relation Between Extreme Precipitable Water Vapor (PWV) and Precipitation for the September 2013 Colorado Flooding Event The Climatological Relation Between Extreme Precipitable Water Vapor (PWV) and Precipitation for the September 213 Colorado Flooding Event Jacola Roman 1, Robert Knuteson 2, Steve Ackerman 3, and Hank

More information

Supplemental Material for Elemental Composition and Oxidation of Chamber Organic Aerosol

Supplemental 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 information

Ryan P. Shadbolt * Central Michigan University, Mt. Pleasant, Michigan

Ryan P. Shadbolt * Central Michigan University, Mt. Pleasant, Michigan 14A.1 RECENT CLIMATE CHANGE IN THE HIGH ELEVATIONS OF THE SOUTHERN APPALACHIANS Ryan P. Shadbolt * Central Michigan University, Mt. Pleasant, Michigan 1. INTRODUCTION Island species are often vulnerable

More information

Background. The Influence of Climate Change on Hurricanes. Further information on climate change and storms

Background. The Influence of Climate Change on Hurricanes. Further information on climate change and storms Background Already, this Atlantic hurricane season has seen devastation with Hurricane Harvey bringing extremely intense and prolonged rainfall and flooding to Texas and Louisiana. Analysis by MetStat

More information

Supporting Information for. Suppression of OH Generation from the Photo-Fenton Reaction in the Presence of α-pinene Secondary Organic Aerosol Material

Supporting Information for. Suppression of OH Generation from the Photo-Fenton Reaction in the Presence of α-pinene Secondary Organic Aerosol Material 1 2 3 4 5 6 7 8 9 10 11 12 13 14 Supporting Information for Suppression of OH Generation from the Photo-Fenton Reaction in the Presence of α-pinene Secondary Organic Aerosol Material Rachel F. Hems *,

More information

Top-of-atmosphere radiative forcing affected by brown carbon in the upper troposphere

Top-of-atmosphere radiative forcing affected by brown carbon in the upper troposphere In the format provided by the authors and unedited. SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO2960 Top-of-atmosphere radiative forcing affected by brown carbon in the upper troposphere Yuzhong Zhang 1,

More information

Melanie S. Hammer 1, Randall V. Martin 1,2, Aaron van Donkelaar 1, Virginie Buchard 3,4, Omar Torres 3, David A. Ridley 5, Robert J.D.

Melanie S. Hammer 1, Randall V. Martin 1,2, Aaron van Donkelaar 1, Virginie Buchard 3,4, Omar Torres 3, David A. Ridley 5, Robert J.D. Interpreting the Ultraviolet Aerosol Index Observed with the OMI Satellite Instrument to Understand Absorption by Organic Aerosols: Implications for Atmospheric Oxidation and Direct Radiative Effects Melanie

More information

Ensemble mean of CMIP5 Sea Surface Temperature projections under climate change and their reference climatology

Ensemble mean of CMIP5 Sea Surface Temperature projections under climate change and their reference climatology Ensemble mean of CMIP5 Sea Surface Temperature projections under climate change and their reference climatology Bruno COMBAL 1, Albert FISCHER 2 1, 2 Intergovernmental Oceanographic Commission (IOC) of

More information

Climate System Scenario Tables. Year RCP2.6 RCP4.5 RCP6.0 RCP8.5 A2 B1 RCP2.6 & RCP4.5 & RCP6.0 & RCP8.5 &

Climate System Scenario Tables. Year RCP2.6 RCP4.5 RCP6.0 RCP8.5 A2 B1 RCP2.6 & RCP4.5 & RCP6.0 & RCP8.5 & Annex II Climate System Scenario Tables Table AII.4.12 HFC-143a abundance (ppt) AII Year RCP2.6 RCP4.5 RCP6.0 RCP8.5 A2 B1 RCP2.6 & RCP4.5 & RCP6.0 & RCP8.5 & 2011 12.0 12.0 12.0 12.0 2010 10.2 9.4 8.4

More information

Phase State and Physical Properties of Ambient and Laboratory. Generated Secondary Organic Aerosol

Phase 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 information

MULTI-WAVELENGTH OPTICAL CALIBRATION OF THERMAL/OPTICAL ANALYZER AND

MULTI-WAVELENGTH OPTICAL CALIBRATION OF THERMAL/OPTICAL ANALYZER AND MULTI-WAVELENGTH OPTICAL CALIBRATION OF THERMAL/OPTICAL ANALYZER AND POTENTIAL APPLICATIONS John G. Watson, Judith C. Chow, L.-W. Antony Chen, Xiaoliang Wang, Ben Sumlin Division of Atmospheric Sciences,

More information

An Analysis of the Evolution of Physical Processes Producing Daily Widespread Precipitation Extremes in Alaska using six CMIP5 GCMs

An Analysis of the Evolution of Physical Processes Producing Daily Widespread Precipitation Extremes in Alaska using six CMIP5 GCMs Meteorology Senior Theses Undergraduate Theses and Capstone Projects 12-2016 An Analysis of the Evolution of Physical Processes Producing Daily Widespread Precipitation Extremes in Alaska using six CMIP5

More information

The Projection of Temperature and Precipitation over Bangladesh under RCP Scenarios using CMIP5 Multi-Model Ensemble

The Projection of Temperature and Precipitation over Bangladesh under RCP Scenarios using CMIP5 Multi-Model Ensemble Paper ID: WRE-37 International Conference on Recent Innovation in Civil Engineering for Sustainable Development (IICSD-5) Department of Civil Engineering DUET - Gazipur, Bangladesh The Projection of Temperature

More information

Interactive comment on Reactive uptake of ammonia to secondary organic aerosols: kinetics of organonitrogen formation by Y. Liu et al.

Interactive 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 information

WHAT DO WE KNOW ABOUT FUTURE CLIMATE IN COASTAL SOUTH CAROLINA?

WHAT DO WE KNOW ABOUT FUTURE CLIMATE IN COASTAL SOUTH CAROLINA? WHAT DO WE KNOW ABOUT FUTURE CLIMATE IN COASTAL SOUTH CAROLINA? Amanda Brennan & Kirsten Lackstrom Carolinas Integrated Sciences & Assessments November 13, 2013 Content Development Support: Greg Carbone

More information

Project report STUDY OF SALT AEROSOLS AT THE SYNCHROTRON SOLEIL. Supervisor : Isaak UNGER, Clara SAAK and Olle BJÖRNEHOLM Examiner : Dimitri ARVANITIS

Project report STUDY OF SALT AEROSOLS AT THE SYNCHROTRON SOLEIL. Supervisor : Isaak UNGER, Clara SAAK and Olle BJÖRNEHOLM Examiner : Dimitri ARVANITIS STUDY OF SALT AEROSOLS AT THE SYNCHROTRON SOLEIL by Mathilde Brunelle Supervisor : Isaak UNGER, Clara SAAK and Olle BJÖRNEHOLM Examiner : Dimitri ARVANITIS Department of Physics and Astronomy, Uppsala

More information

Can Small Boxes Model the Atmospheric Greenhouse?

Can Small Boxes Model the Atmospheric Greenhouse? Can Small Boxes Model the Atmospheric Greenhouse? In other words: Do boxes similar to solar collectors warm up by converting the incident sunlight to infrared and concentrating it? This would mean they

More information

Supplementary Materials for

Supplementary Materials for www.sciencemag.org/content/363/6423/128/suppl/dc1 Supplementary Materials for How fast are the oceans warming? Lijing Cheng*, John Abraham, Zeke Hausfather, Kevin E. Trenberth *Corresponding author. Email:

More information

GRIMM Aerosol Spectrometer and Dust Monitors. Measuring principle

GRIMM Aerosol Spectrometer and Dust Monitors. Measuring principle Grimm Aerosol-Technik GRIMM Aerosol Spectrometer and Dust Monitors Measuring principle Eng. Wolfgang Brunnhuber 1 Agenda Part A physical background general principles of optical particle detection Part

More information

Fine Scale Climate Change Analysis: from Global Models to Local Impact Studies in Serbia

Fine Scale Climate Change Analysis: from Global Models to Local Impact Studies in Serbia Fine Scale Climate Change Analysis: from Global Models to Local Impact Studies in Serbia Ana Vukovic 1,2, Mirjam Vujadinovic 3,2, Vladimir Djurdjevic 4,2, Bojan Cvetkovic 2, Zorica Rankovic-Vasic 3, Zoran

More information

Ultraviolet-Visible and Infrared Spectrophotometry

Ultraviolet-Visible and Infrared Spectrophotometry Ultraviolet-Visible and Infrared Spectrophotometry Ahmad Aqel Ifseisi Assistant Professor of Analytical Chemistry College of Science, Department of Chemistry King Saud University P.O. Box 2455 Riyadh 11451

More information

PCIC SCIENCE BRIEF: SEA LEVEL RISE OBSERVATIONS

PCIC SCIENCE BRIEF: SEA LEVEL RISE OBSERVATIONS PCIC SCIENCE BRIEF: SEA LEVEL RISE OBSERVATIONS AND ACCELERATION Three recent journal articles examine the rate of sea level rise and the ability of models to accurately simulate sea level rise at a global

More information

8.2 Tropospheric ozone

8.2 Tropospheric ozone 8.2 Tropospheric ozone Prev Chapter 8. Ozone Next 8.2 Tropospheric ozone Tropospheric ozone is only about 10% of the total amount of ozone contained in a vertical column in the atmosphere. However, this

More information

Supplementary Material for. Reactive Uptake of Ammonia by Secondary Organic Aerosols: Implications for Air Quality

Supplementary Material for. Reactive Uptake of Ammonia by Secondary Organic Aerosols: Implications for Air Quality Supplementary Material for Reactive Uptake of Ammonia by Secondary Organic Aerosols: Implications for Air Quality Jeremy R. Horne, 1 Shupeng Zhu, 1 Julia Montoya-Aguilera, 2 Mallory L. Hinks, 2 Lisa M.

More information

Surface 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 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 information

Statistical Estimation of the Atmospheric Aerosol Absorption Coefficient Based on the Data of Optical Measurements

Statistical Estimation of the Atmospheric Aerosol Absorption Coefficient Based on the Data of Optical Measurements Statistical Estimation of the Atmospheric Aerosol Absorption Coefficient Based on the Data of Optical Measurements V.N. Uzhegov, V.S. Kozlov, M.V. Panchenko, Yu.A.Pkhalagov, V.V. Pol kin, S.A. Terpugova,

More information

Conference Proceedings Paper Climatic influence on atmospheric evaporative demand in Estonia ( )

Conference Proceedings Paper Climatic influence on atmospheric evaporative demand in Estonia ( ) Conference Proceedings Paper Climatic influence on atmospheric evaporative demand in Estonia (1951-2015) Fernando Domínguez-Castro 1, *, Sergio Vicente-Serrano 1, Jaak Jaagus 2, Miquel Tomas-Burguera 3,

More information

A Preservice Mathematics Teacher s Covariational Reasoning as Mediator for Understanding of Global Warming. Dario A. Gonzalez University of Georgia

A Preservice Mathematics Teacher s Covariational Reasoning as Mediator for Understanding of Global Warming. Dario A. Gonzalez University of Georgia A Preservice Mathematics Teacher s Covariational Reasoning as Mediator for Understanding of Global Warming Dario A. Gonzalez University of Georgia I examine one preservice mathematics teacher s (PST s)

More information

Insights Into Atmospheric Organic Aerosols Using An Aerosol Mass Spectrometer

Insights Into Atmospheric Organic Aerosols Using An Aerosol Mass Spectrometer Insights Into Atmospheric Organic Aerosols Using An Aerosol Mass Spectrometer A thesis submitted to the University of Manchester Institute of Science and Technology for the degree of Doctor of Philosophy

More information

Annual and seasonal air temperature and precipitation trends in the North of the Apuseni Mountains

Annual and seasonal air temperature and precipitation trends in the North of the Apuseni Mountains Annual and seasonal air temperature and precipitation trends in the North of the Apuseni Mountains Viorel Arghiuş, Liviu Muntean, Corina Arghiuş, Gheorghe Roşian, Radu Mihăiescu, Nicolae Baciu, Cristian

More information

Helsinki, Finland. 1 Aerodyne Research Inc., Billerica, MA, USA. 2 Chemistry Department, Boston College, Chestnut Hill, MA, USA

Helsinki, 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 information

Atmospheric New Particle Formation and Climate Sensitivity: the CLOUD experiment.

Atmospheric 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 information

Ultraviolet-Visible and Infrared Spectrophotometry

Ultraviolet-Visible and Infrared Spectrophotometry Ultraviolet-Visible and Infrared Spectrophotometry Ahmad Aqel Ifseisi Assistant Professor of Analytical Chemistry College of Science, Department of Chemistry King Saud University P.O. Box 2455 Riyadh 11451

More information

Effect of aging on cloud nucleating properties of atmospheric aerosols

Effect 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 information

The Impact of Climate Change on the Intensity and Frequency of Windstorms in Canada

The Impact of Climate Change on the Intensity and Frequency of Windstorms in Canada The Impact of Climate Change on the Intensity and Frequency of Windstorms in Canada Lou Ranahan, Meteorologist March 27, 219 mase889/ Twitter 1 P a g e Table of Contents List of Figures... 2 List of Tables...

More information

Tropospheric OH chemistry

Tropospheric 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 information

Supplementary Information

Supplementary Information Electronic Supplementary Material (ESI) for RSC Advances. This journal is The Royal Society of Chemistry 2016 Supplementary Information Multifunctional Fe 2 O 3 /CeO 2 Nanocomposites for Free Radical Scavenging

More information

Wavelength λ Velocity v. Electric Field Strength Amplitude A. Time t or Distance x time for 1 λ to pass fixed point. # of λ passing per s ν= 1 p

Wavelength λ Velocity v. Electric Field Strength Amplitude A. Time t or Distance x time for 1 λ to pass fixed point. # of λ passing per s ν= 1 p Introduction to Spectroscopy (Chapter 6) Electromagnetic radiation (wave) description: Wavelength λ Velocity v Electric Field Strength 0 Amplitude A Time t or Distance x Period p Frequency ν time for 1

More information

CLIMATE ABSOLUTE RADIANCE AND REFRACTIVITY OBSERVATORY (CLARREO)

CLIMATE ABSOLUTE RADIANCE AND REFRACTIVITY OBSERVATORY (CLARREO) CLIMATE ABSOLUTE RADIANCE AND REFRACTIVITY OBSERVATORY (CLARREO) J. Leckey a, * a National Aeronautics and Space Agency (NASA) Langley Research Center (LARC), Bldg. 1202 MS 468, Hampton, Virginia 23681

More information

Chapter 5 Conclusions and Future Studies

Chapter 5 Conclusions and Future Studies 177 Chapter 5 Conclusions and Future Studies 178 Conclusions and Future Studies The results of the studies presented in this thesis confirm that ambient and laboratory-generated aerosols exhibit complex

More information

Spectrophotometric titrations to characterize and monitor chromophoric dissolved organic matter (CDOM) in natural waters

Spectrophotometric titrations to characterize and monitor chromophoric dissolved organic matter (CDOM) in natural waters Spectrophotometric titrations to characterize and monitor chromophoric dissolved organic matter (CDOM) in natural waters Carmen Cartisano*, Rossana Del Vecchio, and Neil Blough* * Department of Chemistry

More information

Secondary organic aerosol from low-volatility and traditional VOC precursors

Secondary 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 information

Testing MOSAIC aerosol scheme implemented in CESM and evaluation with observations

Testing MOSAIC aerosol scheme implemented in CESM and evaluation with observations Testing MOSAIC aerosol scheme implemented in CESM and evaluation with observations Zheng Lu, Xiaohong Liu University of Wyoming Rahul A. Zaveri, Balwinder Singh, Richard Easter, Phil Rasch Pacific Northwest

More information

SPECIAL PROJECT FINAL REPORT

SPECIAL PROJECT FINAL REPORT SPECIAL PROJECT FINAL REPORT All the following mandatory information needs to be provided. Project Title: Modelling Interglacial Climate Computer Project Account: Spdklang Start Year - End Year : 2014

More information

Corresponding Author Ailing Ren

Corresponding Author Ailing Ren 5th International Conference on Environment, Materials, Chemistry and Power Electronics (EMCPE 216) Effects of Ozone concentration and relative humidity on secondary organic aerosol formation from reactions

More information

Morphology of mixed primary and secondary organic particles and the adsorption of spectator organic gases during aerosol formation

Morphology of mixed primary and secondary organic particles and the adsorption of spectator organic gases during aerosol formation Morphology of mixed primary and secondary organic particles and the adsorption of spectator organic gases during aerosol formation Timothy D. Vaden a, Chen Song a, Rahul A. Zaveri a, Dan Imre b, and Alla

More information

1901 Application of Spectrophotometry

1901 Application of Spectrophotometry 1901 Application of Spectrophotometry Chemical Analysis Problem: 1 Application of Spectroscopy Organic Compounds Organic compounds with single bonds absorb in the UV region because electrons from single

More information

Supplementary Information

Supplementary Information Electronic Supplementary Material (ESI) for Nanoscale. This journal is The Royal Society of Chemistry 2014 Supplementary Information Large-scale lithography-free metasurface with spectrally tunable super

More information

Supplementary Information for Fatty acid Surfactant. Photochemistry Results in New Particle Formation

Supplementary Information for Fatty acid Surfactant. Photochemistry Results in New Particle Formation Supplementary Information for Fatty acid Surfactant Photochemistry Results in New Particle Formation Peter A. Alpert 1,,* Raluca Ciuraru 1,a, Stéphanie Rossignol 1,b, Monica Passananti 1,c, Liselotte Tinel

More information

Diesel soot aging in urban plumes within hours under cold dark and humid conditions

Diesel 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 information

9/28/10. Visible and Ultraviolet Molecular Spectroscopy - (S-H-C Chapters 13-14) Valence Electronic Structure. n σ* transitions

9/28/10. Visible and Ultraviolet Molecular Spectroscopy - (S-H-C Chapters 13-14) Valence Electronic Structure. n σ* transitions Visible and Ultraviolet Molecular Spectroscopy - (S-H-C Chapters 13-14) Electromagnetic Spectrum - Molecular transitions Widely used in chemistry. Perhaps the most widely used in Biological Chemistry.

More information

Infrared Spectroscopy: Identification of Unknown Substances

Infrared Spectroscopy: Identification of Unknown Substances Infrared Spectroscopy: Identification of Unknown Substances Suppose a white powder is one of the four following molecules. How can they be differentiated? H N N H H H H Na H H H H H A technique that is

More information

Hyperspectral Atmospheric Correction

Hyperspectral Atmospheric Correction Hyperspectral Atmospheric Correction Bo-Cai Gao June 2015 Remote Sensing Division Naval Research Laboratory, Washington, DC USA BACKGROUND The concept of imaging spectroscopy, or hyperspectral imaging,

More information

Formation, Speciation, and Chemical Processing of Atmospheric Particulate Matter Kara E. Huff Hartz

Formation, Speciation, and Chemical Processing of Atmospheric Particulate Matter Kara E. Huff Hartz Formation, Speciation, and Chemical Processing of Atmospheric Particulate Matter Kara E. Huff Hartz Department of Chemistry and Biochemistry Southern Illinois University Carbondale Carbondale, IL USA khuffhartz@chem.siu.edu

More information

SUPPORTING INFORMATION. How rice (Oryza sativa L.) responds to elevated As under different Si-rich soil amendments

SUPPORTING INFORMATION. How rice (Oryza sativa L.) responds to elevated As under different Si-rich soil amendments SUPPORTING INFORMATION How rice (Oryza sativa L.) responds to elevated As under different Si-rich soil amendments William A. Teasley, Matt A. Limmer, Angelia L. Seyfferth* Department of Plant and Soil

More information

Managing Risk for Development

Managing Risk for Development International Policy Workshop World Development Report 2014 Managing Risk for Development Do we understand the drivers of risk? Prof. Dr. Joern BIRKMANN UNU-EHS, Bonn, Germany birkmann@ehs.unu.edu Increasing

More information

Preface to the Second Edition. Preface to the First Edition

Preface to the Second Edition. Preface to the First Edition Contents Preface to the Second Edition Preface to the First Edition iii v 1 Introduction 1 1.1 Relevance for Climate and Weather........... 1 1.1.1 Solar Radiation.................. 2 1.1.2 Thermal Infrared

More information

Response of Arctic temperature to changes in emissions of short-lived climate forcers

Response of Arctic temperature to changes in emissions of short-lived climate forcers SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE2880 Response of Arctic temperature to changes in emissions of short-lived climate forcers M. Sand, T. K. Berntsen, K. von Salzen, M. G. Flanner, J. Langner

More information

EFFECT OF NOX IN THE PHOTOCHEMICAL SYSTEM OF Α-PINENE

EFFECT 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 information

causes Associate Professor Department of Meteorology The Pennsylvania State University

causes Associate Professor Department of Meteorology The Pennsylvania State University Recent climate change and its causes Raymond Najjar Associate Professor Department of Meteorology The Pennsylvania State University Presentation for: Erie County Climate Adaptation Workshop September 1,

More information

DEVELOPMENT OF A NEXT-GENERATION ENVIRONMENTAL CHAMBER FACILITY FOR CHEMICAL MECHANISM AND VOC REACTIVITY RESEARCH

DEVELOPMENT OF A NEXT-GENERATION ENVIRONMENTAL CHAMBER FACILITY FOR CHEMICAL MECHANISM AND VOC REACTIVITY RESEARCH DEVELOPMENT OF A NEXT-GENERATION ENVIRONMENTAL CHAMBER FACILITY FOR CHEMICAL MECHANISM AND VOC REACTIVITY RESEARCH SUMMARY OF PROGRESS AND DRAFT RESEARCH PLAN BY WILLIAM P. L. CARTER COLLEGE OF ENGINEERING

More information

An Introduction to Ultraviolet-Visible Molecular Spectrometry (Chapter 13)

An Introduction to Ultraviolet-Visible Molecular Spectrometry (Chapter 13) An Introduction to Ultraviolet-Visible Molecular Spectrometry (Chapter 13) Beer s Law: A = -log T = -logp 0 / P = e x b x C See Table 13-1 for terms. In measuring absorbance or transmittance, one should

More information

Heterogeneous Process Studies on the Formation of Secondary Aerosol

Heterogeneous Process Studies on the Formation of Secondary Aerosol 2016 BC workshop Heterogeneous Process Studies on the Formation of Secondary Aerosol Maofa Ge Institute of Chemistry Chinese Academy of Sciences June-27-2016 Aerosol Heterogeneous Chemistry Atmospheric

More information

FLAME PHOTOMETRY AIM INTRODUCTION

FLAME PHOTOMETRY AIM INTRODUCTION FLAME PHOTOMETRY AIM INTRODUCTION Atomic spectroscopy is based on the absorption, emission or fluorescence process of light by atoms or elementary ions. Information for atomic scale is obtained in two

More information

Department of Chemistry of The College of Staten Island and The Graduate Center, The City University of

Department of Chemistry of The College of Staten Island and The Graduate Center, The City University of Electronic Supplementary Material (ESI) for Journal of Materials Chemistry A. This journal is The Royal Society of Chemistry 2014 Fe 3 O 4 /Carbon quantum dots hybrid nanoflowers for highly active and

More information

Trends in temperature and rainfall extremes during recent years at different stations of Himachal Pradesh

Trends in temperature and rainfall extremes during recent years at different stations of Himachal Pradesh Vol. Journal 19, No. of Agrometeorology 1 19 (1) : 51-55 (March 2017) PRASAD et al 51 Trends in temperature and rainfall extremes during recent years at different stations of Himachal Pradesh RAJENDRA

More information

Direct radiative forcing due to aerosols in Asia during March 2002

Direct radiative forcing due to aerosols in Asia during March 2002 Direct radiative forcing due to aerosols in Asia during March 2002 Soon-Ung Park, Jae-In Jeong* Center for Atmospheric and Environmental Modeling *School of Earth and Environmental Sciences, Seoul National

More information

OFF THE CHARTS: 2013 WAS AUSTRALIA S HOTTEST YEAR

OFF THE CHARTS: 2013 WAS AUSTRALIA S HOTTEST YEAR OFF THE CHARTS: 2013 WAS AUSTRALIA S HOTTEST YEAR The Climate Council is an independent, crowd-funded organisation providing quality information on climate change to the Australian public. 2013 was a remarkable

More information

VALLIAMMAI ENGINEERING COLLEGE SRM Nagar, Kattankulathur

VALLIAMMAI ENGINEERING COLLEGE SRM Nagar, Kattankulathur VALLIAMMAI ENGINEERING COLLEGE SRM Nagar, Kattankulathur 603 203 DEPARTMENT OF ELECTRONICS AND INSTRUMENTATION ENGINEERING QUESTION BANK V SEMESTER EI6501 Analytical Instruments Regulation 2013 Academic

More information

Updates on Aerodyne PAM Oxidation Flow Reactor. Andy Lambe 1

Updates on Aerodyne PAM Oxidation Flow Reactor. Andy Lambe 1 ass Updates on Aerodyne PAM Oxidation Flow Reactor w at ere Andy Lambe 1 Potential Aerosol Mass (PAM) Oxidation Flow Reactor Developed by Bill Brune, improved and manufactured by Aerodyne Flow-through

More information

Hand in Question sheets with answer booklets Calculators allowed Mobile telephones or other devices not allowed

Hand in Question sheets with answer booklets Calculators allowed Mobile telephones or other devices not allowed York University Department of Earth and Space Science and Engineering ESSE 3030 Department of Physics and Astronomy PHYS 3080 Atmospheric Radiation and Thermodynamics Final Examination 2:00 PM 11 December

More information

Advanced Pharmaceutical Analysis

Advanced Pharmaceutical Analysis Lecture 2 Advanced Pharmaceutical Analysis IR spectroscopy Dr. Baraa Ramzi Infrared Spectroscopy It is a powerful tool for identifying pure organic and inorganic compounds. Every molecular compound has

More information

Chapter Eight: Conclusions and Future Work

Chapter 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 information

Aerodyne Chinese AMS/ACSM Clinic, Nanjing, April Why are we here? Data Analysis Clinics Boulder, PSI. Barcelona, Boulder

Aerodyne 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 information

Chapter 9. Atomic emission and Atomic Fluorescence Spectrometry Emission spectrophotometric Techniques

Chapter 9. Atomic emission and Atomic Fluorescence Spectrometry Emission spectrophotometric Techniques Chapter 9 Atomic emission and Atomic Fluorescence Spectrometry Emission spectrophotometric Techniques Emission Spectroscopy Flame and Plasma Emission Spectroscopy are based upon those particles that are

More information

THIN ICE AREA EXTRACTION IN THE SEASONAL SEA ICE ZONES OF THE NORTHERN HEMISPHERE USING MODIS DATA

THIN ICE AREA EXTRACTION IN THE SEASONAL SEA ICE ZONES OF THE NORTHERN HEMISPHERE USING MODIS DATA THIN ICE AREA EXTRACTION IN THE SEASONAL SEA ICE ZONES OF THE NORTHERN HEMISPHERE USING MODIS DATA K. Hayashi 1, K. Naoki 1, K. Cho 1 *, 1 Tokai University, 2-28-4, Tomigaya, Shibuya-ku, Tokyo, Japan,

More information

Chem 434 Instrumental Analysis Test 1

Chem 434 Instrumental Analysis Test 1 Chem 434 Instrumental Analysis Test 1 Name: 1. (15 points) In Chapter 5 we discussed four sources of instrumental noise: Thermal Noise, Shot Noise, Flicker Noise, and Environmental noise. Discuss the differences

More information

Supporting Information for The Active Role of the Ocean in Transient Climate Sensitivity

Supporting Information for The Active Role of the Ocean in Transient Climate Sensitivity GEOPHYSICAL RESEARCH LETTERS Supporting Information for The Active Role of the Ocean in Transient Climate Sensitivity Oluwayemi A. Garuba 1 Jian Lu 1, Fukai Liu 2, and Hansi A. Singh 1 Contents of this

More information

Climatic Variability and Linear Trend Models for the Six Major Regions of Gilgit-Baltistan, Pakistan

Climatic Variability and Linear Trend Models for the Six Major Regions of Gilgit-Baltistan, Pakistan Proceedings of the Pakistan Academy of Sciences: B. Life and Environmental Sciences 53 (2): 129 136 (216) Copyright Pakistan Academy of Sciences ISSN: 377-2969 (print), 236-1448 (online) Pakistan Academy

More information

Chromatography & instrumentation in Organic Chemistry

Chromatography & instrumentation in Organic Chemistry Chromatography & instrumentation in Organic Chemistry What is Chromatography? Chromatography is a technique for separating mixtures into their components in order to analyze, identify, purify, and/or quantify

More information

Chemistry Instrumental Analysis Lecture 34. Chem 4631

Chemistry Instrumental Analysis Lecture 34. Chem 4631 Chemistry 4631 Instrumental Analysis Lecture 34 From molecular to elemental analysis there are three major techniques used for elemental analysis: Optical spectrometry Mass spectrometry X-ray spectrometry

More information

CHAPTER 7 SUMMARY OF THE PRESENT WORK AND SUGGESTIONS FOR FUTURE WORK

CHAPTER 7 SUMMARY OF THE PRESENT WORK AND SUGGESTIONS FOR FUTURE WORK 161 CHAPTER 7 SUMMARY OF THE PRESENT WORK AND SUGGESTIONS FOR FUTURE WORK 7.1 SUMMARY OF THE PRESENT WORK Nonlinear optical materials are required in a wide range of important applications, such as optical

More information

CURRENT STATUS OF THE DEVELOPMENT AND EVALUATION OF AN UPDATED DETAILED MECHANISM FOR VOC OXIDATION

CURRENT STATUS OF THE DEVELOPMENT AND EVALUATION OF AN UPDATED DETAILED MECHANISM FOR VOC OXIDATION CURRENT STATUS OF THE DEVELOPMENT AND EVALUATION OF AN UPDATED DETAILED MECHANISM FOR VOC OXIDATION William P. L. Carter Statewide Air Pollution Research Center and College of Engineering, Center for Environmental

More information

Aerosols and climate. Rob Wood, Atmospheric Sciences

Aerosols and climate. Rob Wood, Atmospheric Sciences Aerosols and climate Rob Wood, Atmospheric Sciences What are aerosols? Solid or liquid particles suspended in air Sizes range from a few nm to a few thousand nm Huge range of masses Where do aerosols come

More information

Ann M. Dillner, Travis Ruthenburg. UC Davis. IMPROVE Steering Committee Meeting, 2011

Ann M. Dillner, Travis Ruthenburg. UC Davis. IMPROVE Steering Committee Meeting, 2011 FT-IR: a promising method for checking consistency between Teflon and quartz channels and measuring OM on IMPROVE samples Ann M. Dillner, Travis Ruthenburg UC Davis IMPROVE Steering Committee Meeting,

More information

Stefan-Boltzmann law for the Earth as a black body (or perfect radiator) gives:

Stefan-Boltzmann law for the Earth as a black body (or perfect radiator) gives: 2. Derivation of IPCC expression ΔF = 5.35 ln (C/C 0 ) 2.1 Derivation One The assumptions we will make allow us to represent the real atmosphere. This remarkably reasonable representation of the real atmosphere

More information

Chemistry 524--Final Exam--Keiderling May 4, :30 -?? pm SES

Chemistry 524--Final Exam--Keiderling May 4, :30 -?? pm SES Chemistry 524--Final Exam--Keiderling May 4, 2011 3:30 -?? pm -- 4286 SES Please answer all questions in the answer book provided. Calculators, rulers, pens and pencils are permitted. No open books or

More information

Introduction to Global Warming

Introduction to Global Warming Introduction to Global Warming Cryosphere (including sea level) and its modelling Ralf GREVE Institute of Low Temperature Science Hokkaido University Sapporo, 2010.09.14 http://wwwice.lowtem.hokudai.ac.jp/~greve/

More information

PHYSICS 231 INTRODUCTORY PHYSICS I

PHYSICS 231 INTRODUCTORY PHYSICS I PHYSICS 231 INTRODUCTORY PHYSICS I Lecture 17 Heat: Q = Energy transferred due to microscopic contact Recap - Heat Transfer Heat can: Change temperature Q = mc!t c = specific heat For water: c= 1.0 cal/(g

More information

Questions on Instrumental Methods of Analysis

Questions on Instrumental Methods of Analysis Questions on Instrumental Methods of Analysis 1. Which one of the following techniques can be used for the detection in a liquid chromatograph? a. Ultraviolet absorbance or refractive index measurement.

More information

Supplementary Figure 1 UV-Vis spectra and Tauc plots of (a) ZnO and (b) Cu2O nanoparticles.

Supplementary Figure 1 UV-Vis spectra and Tauc plots of (a) ZnO and (b) Cu2O nanoparticles. Supplementary Figure 1 UV-Vis spectra and Tauc plots of (a) ZnO and (b) Cu2O nanoparticles. Supplementary Figure 2 GC-MS chromatogram at m/e = 17 using 13 CO2 and Na2 13 CO3 as carbon sources for CO2 reduction.

More information

Aurélien Ribes 1. Introduction

Aurélien Ribes 1. Introduction ESAIM: PROCEEDINGS AND SURVEYS, 2018, Vol. 60, p. 104-113 Jean-François Coeurjolly & Adeline Leclercq-Samson IS FUTURE CLIMATE PREDICTABLE WITH STATISTICS? Aurélien Ribes 1 Abstract. The purpose of this

More information