PALMS Single particle composition measurements for ATom Karl Froyd 1,2 and Dan Murphy 1 1. NOAA Earth Systems Research Laboratory 2. CIRES, University.

Slides:



Advertisements
Similar presentations
Water in the Atmosphere
Advertisements

What’s Up There May be a Problem, or then again, Maybe Not Now for a Little Information on Aerosols Rosemary Millham, PhD NASA GSFC/SSAI.
A Dictionary of Aerosol Remote Sensing Terms Richard Kleidman SSAI/NASA Goddard Lorraine Remer UMBC / JCET Short.
Soot Particle Aerosol Mass Spectrometer: Development, Validation, and Initial Application T. B. Onasch,A. Trimborn,E. C. Fortner,J. T. Jayne,G. L. Kok,L.
P. D. Hien, V. T. Bac, N. T. H. Thinh Vietnam Atomic Energy Commission.
Proposed Aerosol Treatment for CAM4 Steve Ghan, Richard Easter, Xiaohong Liu, Rahul Zaveri Pacific Northwest National Laboratory precursor emissions coagulation.
Section highlights Organic Aerosol and Field Studies.
Global Aerosol Microphysics With TOMAS Peter J. Adams Acknowledgments: Win Trivitayanurak GEOS-CHEM User’s Meeting April 7, 2009 Center for Atmospheric.
Two-Moment Aerosol Microphysics (TOMAS) Development GEOS-CHEM User’s Meeting 4-6 April 2005 Funding: NSF / NASA Peter Adams Kaiping Chen Jeffrey Pierce.
Carbonaceous Particles: Practical Micro-Apportionment via Single Particle SEM/EDX Alex Laskin, Martin Iedema, James Cowin Pacific Northwest National Laboratory.
Eric M. Leibensperger, Loretta J. Mickley, Daniel J. Jacob School of Engineering and Applied Sciences, Harvard University Climate response to changing.
Ultrafine Particles and Climate Change Peter J. Adams HDGC Seminar November 5, 2003.
Investigating Organic Aerosol Loading in the Remote Marine Environment K. Lapina 1, ), C. L. Heald 1, D. V. Spracklen 2, S.
1 High Time-Resolution Size- Resolved Aerosol Predictions: Learning about CCN from Aerosol Field Campaigns Win Trivitayanurak GEOS-CHEM Meeting Harvard.
Illumination Independent Aerosol Optical Properties n Extinction Scattering Absorption n Volume scattering function (phase) n Transmittance.
Aerosols and climate Rob Wood, Atmospheric Sciences.
MET 12 Global Climate Change – Lecture 8
Brown carbon in the continental troposphere: sources, evolution and radiative impacts Evolution of Brown Carbon in Wildfire Plumes -Submitted to GRL- Rodney.
Chemical composition of aerosols Composition of tropospheric aerosols is not uniform. It varies with particle size and source of particles: Ultrafine particles.
Implementing Online Marine Organic Aerosol Emissions into GEOS-Chem Implementing Online Marine Organic Aerosol Emissions into GEOS-Chem NASA Ames Research.
MAOS (Mobile Aerosol Observing System) and the G1 Aircraft at Cape Cod Allie Marquardt Collow.
Aerosol Working Group The 7 th International GEOS-Chem User’s Meeting May 4, 2015 Aerosol WG Co-Chairs Colette Heald: Jeff Pierce (outgoing):
Visualization, Exploration, and Model Comparison of NASA Air Quality Remote Sensing data via Giovanni Ana I. Prados, Gregory Leptoukh, Arun Gopalan, and.
Urban Air Pollution IB syllabus: AP syllabus Ch 17, 18.
CCN measurements at an urban location Julia Burkart University of Vienna Istitute of Aerosol Physics, Biophysics and Environmental Physics.
The effect of the size of CCN on drizzle and rain formation in convective clouds Roelof T. Bruintjes Research Applications Program, National Center for.
June 7, 2004 Laboratory Studies of Ice Initiation by Atmospheric Aerosol Particles Paul J. DeMott With acknowledgment to numerous contributors.
Aerosol Microphysics: Plans for GEOS-CHEM
Sources and Processes Affecting the Chemical and Physical Properties of Denver Aerosol during DISCOVER-AQ FRAPPÉ/DISCOVER-AQ Science Team Meeting 4 May.
(Impacts are Felt on Scales from Local to Global) Aerosols Link Climate, Air Quality, and Health: Dirtier Air and a Dimmer Sun Emissions Impacts == 
Proposal for a Research Infrastructure for Advanced Aerosol Observations and Capacity Building in China Alfred WIEDENSOHLER Leibniz Institute for Tropospheric.
Monday, 8/31/091 ATMO Class #2 Monday, August 31, 2009 Chapter 1 Introduction to the Atmosphere.
School of something FACULTY OF OTHER 1 Lecture 2: Aerosol sources and sinks Ken Carslaw.
Lidar Working Group on Space-Based Winds, Snowmass, Colorado, July 17-21, 2007 A study of range resolution effects on accuracy and precision of velocity.
Chapter 17.1 Atmospheric Characteristics
Improving Black Carbon (BC) Aging in GEOS-Chem Based on Aerosol Microphysics: Constraints from HIPPO Observations Cenlin He Advisers: Qinbin Li, Kuo-Nan.
Black Carbon Measurements at Whistler Sarah Hanna (UBC)
ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: The Aerosol mass Spectrometer Hugh Coe School of Earth, Atmospheric and Environmental Sciences.
Properties of Particulate Matter Physical, Chemical and Optical Properties Size Range of Particulate Matter Mass Distribution of PM vs. Size: PM10, PM2.5.
Biosphere/Atmosphere Interactions in the Tropics.
UNH Soluble Acidic Gases and Aerosol (SAGA) during INTEX Phase A Jack E. Dibb, Eric Scheuer, and Robert W. Talbot With Thanks to the INTEX Science Team.
Progress on Application of Modal Aerosol Dynamics to CAM Xiaohong Liu, Steve Ghan, Richard Easter, Rahul Zaveri, Yun Qian (Pacific Northwest National.
Studies of Emissions & Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys (SEAC 4 RS) Brian Toon Department of Atmospheric and Oceanic.
GLOBAL SULFUR BUDGET [Chin et al., 1996] (flux terms in Tg S yr -1 ) Phytoplankton (CH 3 ) 2 S SO 2  1.3d DMS  1.0d OHNO 3 Volcanoes Combustion.
The GEOS-CHEM Simulation of Trace Gases over China Li ZHANG and Hong LIAO Institute of Atmospheric Physics Chinese Academy of Sciences April 24, 2008.
A NASA / NSF / NRL airborne field campaign focusing on atmospheric composition, chemistry, and climate over Southeast Asia. Programmatic Context, Issues.
Temporal variations of aerosol components in Tijuana, Mexico, during the Cal-Mex campaign S. Takahama, A. Johnson, J. Guzman Morales, L.M. Russell Scripps.
Recent Advances in the Use of Chemical Transport Models in Atmospheric Chemistry Studies G. Carmichael, I. Uno, Y. Tang, J. Woo, D. Streets, G. Kurata,
SEAC4RS Payload Payload Synergies Synergies. Complementarity between aircraft can be considered to fall into three categories. Each has considerations.
ASCOS planning meeting, 8 th April 2008 IAC ETH Single Particle Chemical Characterization and Measurements of Cloud Condensation Nuclei Berko Sierau, Maria.
Relating Aerosol Mass and Optical Depth in the Southeastern U.S. C. A. Brock, N. L. Wagner, A. M. Middlebrook, T. D. Gordon, and D. M. Murphy Earth System.
Tracers of stratospheric influence and Asian dust over the Pacific during INTEX B phase II UNH SAGA special thanks to FASTOZ.
A Non-POC HYPOTHESIS (A. Clarke): The persistence of the adjacent Scu clouds that define a POC region is sustained as a result of entrainment of aged aerosol.
MILAGRO Science Workshop -- October 2006 Summary of preliminary discussions on near-, mid-, and far-field chemistry W. Brune reporting Preliminary Findings.
SOA derived from isoprene epoxydiols: Insights into formation, aging and distribution over the continental US from the DC3 and SEAC 4 RS campaigns Pedro.
Future for APS and related. APS-2 Reflight Report.
Atmospheric Particles  Size range: to 50  m,  m particle contains ~1000 molecules  Concentration ranges: cm -3 =
March 29 – April 1, INTEX-NA Workshop Aerosol and Cloud Spatial Distributions and Microphysical Properties Bruce Anderson, Lee Thornhill, Gao.
Marine biogenic emissions, sulfate formation, and climate: Constraints from oxygen isotopes Becky Alexander Harvard University Department of Earth and.
Aerosol 1 st indirect forcing in the coupled CAM-IMPACT model: effects from primary-emitted particulate sulfate and boundary layer nucleation Minghuai.
Monday, 8/30/20101 ATMO Class #2 Monday, August 30, 2010 Chapter 1 Introduction to the Atmosphere.
Modal Aerosol Treatment in CAM: Evaluation and Indirect Effect X. Liu, S. J. Ghan, R. Easter (PNNL) J.-F. Lamarque, P. Hess, N. Mahowald, F. Vitt, H. Morrison,
Aerosol Microphysical Properties (AMP) Measurements for ATom and cloud! 1) Where do particles come from in the remote troposphere? New particle formation.
University of Hawai`i, Hawai`i Group for Environments Aerosol Research School of Ocean and Earth Science and Technology A. Clarke, S. Howell, C. M c Naughton,
TOWARDS AN AEROSOL CLIMATOLOGY
Aerosol chemistry studies at the SMEARIII station in Kumpula
AEROSOLS REDUCE ATMOSPHERIC OXIDATION
Measuring microphysical, chemical and optical properties of aerosols aboard the NCAR/NSF C-130 during VOCALS Studying size-resolved aerosol cloud interactions.
TFMM Work plan for 2010 Build-up the appropriate framework for the implementation of the revised monitoring strategy Technical support to the Parties.
RECEPTOR MODELLING OF AIRBORNE PARTICULATE MATTER
Presentation transcript:

PALMS Single particle composition measurements for ATom Karl Froyd 1,2 and Dan Murphy 1 1. NOAA Earth Systems Research Laboratory 2. CIRES, University of Colorado Boulder, CO View from NASA WB-57 Supporting Measurements Aerosol size distributions (AMP – Chuck Brock, Bernadett Weinzierl) Instrument Data Products Science Objectives Logistics

Mineral Dust Aged Biomass Burning NOAA PALMS Instrument Particle Analysis by Laser Mass Spectrometry Single particle size and composition (0.2 ~ 4  m) detect a particle – – – vaporize & ionize Time-of-flight MS analyze ions focus particles 193 nm

Mineral Dust Processed Sea Salt Aged Biomass Burning Sulfate-Organic mixture Biomass Burning EC Sea Salt Mineral Dust Meteoric Oil Combustion Other Raw Data Basic Products Compositional Details Quantitative Abundances Combine with size distribution instrument Size-resolved and integrated number and mass for each particle type Aging Accumulation of secondary material during Chemical processing Markers for cloud processing Internal mixing etc PALMS Data Products Overview Size-Resolved Particle Types ~3 min resolution ≥5 min resolution

Particle Type Data Products SEAC4RS Gulf of Mexico Quantitative Products Composition-Apportioned Volume

Aerosol Composition Examples Clouds and BB plumes excluded SEAC4RS Aug-Sept 2013 DC3 May-June 2012 Sulfate-Organic mixture Biomass Burning EC Sea Salt Mineral Dust Meteoric Oil Combustion

PALMS ATom - Primary Science Objectives Mapping climate-relevant aerosol Mineral Dust Large fraction of PM, direct forcing, effective ice nuclei largely controls cirrus formation in the NH Sea Salt Large fraction of PM, CCN: partially controls marine stratus Biomass Burning Particles …i.e., internal mixtures of OC, BC, and inorganic fire emissions Large fraction of PM, largest source of OC to the free troposphere, direct forcing (BC and BrC) PALMS is less quantitative but very selective – can differentiate BB from other sources of OC and BC Often more sensitive than gas-phase tracers under bkgnd conditions Abundances are poorly constrained above the BL… in situ measurements are rare Upstream processes: urban emissions, fires, cloud processing, …

Ground Network Dust Aerosol Mass (  g m -3 ) GEOS-Chem PALMS Ground networks Dust simulations: SE US DC-8 Intercomparison Sea Salt PALMS SAGA derived ATom CCMs AM3 CAM-Chem GEOS-Chem All can track Sea Salt and Dust BB: fire-tagged aerosol or CO Initial Comparisons

Additional Science Capabilities Aging of primary particles All particles acquire secondary mat’l: sulfate, nitrate, organics, halogens… ‘Coatings’ deactivate mineral dust as ice nuclei, increase CCN activity Tracers and Indicators Cloud Processing: hydroxy-MSA, dicarboxylic acids, internal mixing, sulfate size & acidity Industrial emissions: Particles from heavy oil combustion, industrial metals Marine influence: methanesulfonic acid, sea salt High Potential for New Discoveries Historical Examples: Meteoric particle abundance, Pb ubiquity, Hg at the tropopause, organosulfates, BB particles throughout the stratosphere, … ATom possibility: Abundance of metallic aerosol. Extremely efficient IN. Largely from urban/industrial emissions. Distribution and abundance ???

Aerosol Sampling Limitations 1. Inside Clouds: Many aerosol measurements are not valid inside cloud due to shatter artifacts from water droplet and ice crystal impaction PALMS will exclude all in-cloud data 2. Aerosol Particles >5 microns: Windy/humid MBL Saharan dust plume No data for internal instruments However, external cloud/aerosol probe measures concentration: 0.5–50 microns Weak Saharan Plume SEAC4RS 8/8/2013 External cloud/aerosol probe internal aerosol instrument Artifact Fraction Artifacts 1. Aerosol from surface 2. Ablation of inlet material

Logistics Instrument Status: TRL 9, minor maintenance only Possible KORUS deployment Personnel: 1 operator/maintenance (Froyd or postdoc, TBD) Special field operations: Excimer laser gas maintenance: 15 mins every ~3 flights Beginning or end of ground maintenance days Equipment: Critical spares onboard, deploy other support equip Laser gas: pre-deploy at 2-3 locations, plus bring a small cylinder (TBD) onboard Ground schedules, flight plans, data policy… all OK.