Deliverables

Draft: April 18, 2005





There is a strong need to reduce uncertainty in estimates of radiative forcing of climate and climate change by aerosols. The DOE Atmospheric Science Program is a major component of a larger national and international program addressing this issue. In particular, in addition to research on aerosol properties and processes affecting climate forcing, there is a need to represent aerosol processes, properties, and influences on clouds and radiation in large-scale climate models. While such modeling is beyond the scope of ASP, it requires the products of ASP research in evaluating such large-scale influences. In particular this effort requires models and parameterizations of the pertinent aerosol properties and processes, that is, numerical descriptions of these processes that can be incorporated in such large scale models, together with assessments of the accuracy of such models and parameterizations. These requirements drive research that is conducted within ASP and also the deliverables of the Program. These deliverables are distinguished into two categories:

Science deliverables are specific advances that form the scientific basis for program deliverables. Science deliverables range from data sets (from field and laboratory studies) comprising the primary results of these studies, to scientific papers published in the peer-reviewed literature that document the findings on which ASP models and parameterizations are based and the associated uncertainties. These science deliverables will generally be completed in a given funding cycle; the current funding cycle extends over FY 2005-FY 2007.

Program deliverables are the products that will be delivered by the program as a whole. These program deliverables incorporating these advances in science will generally be completed in following three-year funding cycle, i.e., during FY 2008-FY 2010.

This document introduces the ASP Program Deliverables and the ASP Science Deliverables that are needed to support those Program Deliverables.


PROGRAM DELIVERABLES



Models and parameterizations
suitable for representing aerosol properties and processes required to compute aerosol radiative forcing of climate in large-scale climate models, together with an assessment of their accuracy and limitations.

  • Models and parameterizations relating aerosol light scattering and absorption, including dependence on relative humidity and other controlling variables, to aerosol chemical and microphysical properties.

  • Models and parameterizations relating cloud microphysical properties and dependence on controlling variables, to concentration, and chemical and microphysical properties of pre-cloud aerosol.

  • Models and parameterizations relating the evolution of aerosol composition and microphysical properties, and optical and cloud nucleating properties, to concentrations of precursor gases, properties of the pre-existing aerosol, cloud processing, and other controlling variables.


    SCIENCE DELIVERABLES



    1. FIELD MEASUREMENTS

    Measurements of concentrations and properties of aerosols and aerosol precursors and other pertinent variables (e.g., insolation, meteorological and micrometeorological data) suitable for developing and/or evaluating model-based representation of the processes controlling the loading and properties of atmospheric aerosols especially pertinent to their direct and indirect radiative forcing.

    These data sets will be intensive in space, time, and multivariate, encompassing multiple measurements by multiple techniques, permitting highly differentiated examination of interrelations between aerosol properties and governing processes and development of qualitative and quantitative descriptions of aerosol processes in the atmosphere.

    Specific deliverables

  • Data sets from G-1 aircraft flights during ASP field campaigns, including documentation and visualization tools. Measurements include atmospheric state parameters, concentrations of core gas-phase species (CO, SO2, O3, NO, NO2, NOy, etc), and aerosol properties, together with other pertinent data (location, altitude, etc.). Data are to be provided in customary physical units and readily usable format and documented with appropriate calibrations and uncertainties. [Hubbe, Springston]

  • A merged data set of all the surface observations made during the ASP field experiments on a uniform time grid.

  • Data set of vertical profiles of aerosol optical properties in "curtains" under the Flight International Lear Jet. These properties include (a) Aerosol backscatter coefficient at 532 nm and 1064 nm; (b) Aerosol extinction coefficient at 532 nm; and (c) Aerosol depolarization (%) at 532 nm and 1064 nm. These deliverables would be provided for measurements acquired as part of the ASP 2006 Megacity Aerosol eXperiment in Mexico city (MAX-Mex), the Aerosol Processing in Cumuliform Clouds experiment, and proposed future ASP missions as requested by the ASP science team. [Hostetler]

  • Comparisons of measurements of aerosol optical properties with optical properties calculated from measured aerosol size distributions, aerosol morphology, and chemical composition, together with assessment of uncertainties. [optical properties working group]

  • Determination of the evolution of aerosol microphysical and optical properties during well defined Lagrangian or quasi-Lagrangian situations, and comparison with model calculations of such evolution. [multiple investigators]

  • Measurements of aerosol size-distribution and aerosol hygroscopicity and volatility pertinent to size-resolved aerosol mixing state and composition [Wang] and comparison with model calculations of such properties.

  • Chemical content of secondary organic aerosol (SOA); concentration of gaseous SOA precursors and oxidants. [Molina]

  • Measurements by proton-transfer ion-trap mass spectrometry time-of-flight mass spectrometry chemical identity and concentration of SOA and gaseous SOA precursors. [Alexander]

  • Characterization by a variety of microscopic and spectroscopic techniques of chemical, hygroscopic, and morphological properties of bulk aerosol and individual particles. [Laskin]

  • Characterization by near-edge x-ray absorption spectra of atmospheric particles that do or do not contain soot (black carbon, BC); determination of the extent to which x-ray microscopy imaging can be used to quantify the mixing state of BC particles. [Gilles]

  • Measurements by liquid-phase chromatography of filter samples of concentrations total organic carbon and water soluble organic carbon in aerosols in conjunction with characterization of humic-like substances in these aerosols. [Lee]

  • Characterization of field collected organic aerosol particles pertinent to relationships between chemical structure and physical (hygroscopic and optical) properties. [Finlayson-Pitts]

  • CCN data set--concentrations active at at least 10 different supersaturations every few seconds throughout the research portions of all research flights in MASE. The entire range of supersaturations should span 1-0.02%. [Hudson]

  • Measurements of aerosol absorption using a photoacoustic and photothermal interferometric techniques. [Arnott, Sedlacek].

  • Determination of black carbon and organic carbon aerosol mass and optical properties. [Paulson]

  • Determination of aerosol mean lifetimes and black carbon washout rates. [Gaffney]

  • Chemical characterization for activated and non-activated aerosols. [Berkowitz and Jobson]

  • Chemical and size characterization of aerosols following their passage through cumuliform clouds. [Berkowitz and Berg]

    Examples of possible derived products

  • Identification of mechanisms by which gas-phase precursors are converted to condensed phase material by secondary atmospheric reaction, e.g., acid catalyzed reaction and the responsible reagent substances.

  • Determination of rates and yields of aerosol processes such as secondary organic aerosol formation and conversion of hydrophobic to hydrophilic aerosol.

  • Identification of conditions under which new particle formation occurs in the atmosphere, the responsible nucleating substances, threshold conditions, and the like.

    2. LABORATORY STUDIES

    Laboratory measurements of concentrations and properties of aerosols and aerosol precursors and other pertinent variables (e.g., insolation, meteorological and micrometeorological data) suitable for determination of derived products such as rate constants and mechanisms, suitable for incorporation in and/or evaluation of model-based representation of the processes controlling the amount and properties of atmospheric aerosols especially pertinent to their direct and indirect radiative forcing.
    These studies examine aerosol properties and of their evolution under controlled laboratory conditions, together with a specification of those conditions, permitting qualitative and quantitative descriptions of aerosol processes in the atmosphere, their rates, and their dependence on governing conditions.

    Specific deliverables

  • Determination of physical and chemical properties of BC particles subjected to surface oxidation and coating with organic and inorganic species. Examination of effect of soot morphology and chemistry on hydroscopic and optical properties. [Davidovits]

  • Smog chamber data for acid-catalyzed SOA formation from a variety of parent VOCs, including molecular speciation by mass spectrometry and hygroscopicity characterization. [Seinfeld]

  • Characterization by a variety of microscopic and spectroscopic techniques of chemical, hygroscopic, and morphological properties of bulk aerosol and individual particles produced under controlled laboratory conditions . [Laskin]

  • Characterization of organic particles produced under controlled laboratory conditions to determine structure-physical (hygroscopic and optical) properties relationships for SOA and nitrate particles. [Finlayson-Pitts]

  • Rate constants for reactions of OH, NO3, and O3 with various particulate organic compounds including molecular tracers commonly used for organic sources suitable for modeling atmospheric oxidation rates of primary particulate emissions. [Ziemann]

  • Identification of non-volatile, semi-volatile, and volatile products formed from organic particle oxidation by OH, NO3, and O3, and the reaction mechanisms suitable for developing quantitative predictions of the effect of oxidation on hygroscopicity and CCN activity. [Ziemann]

  • Laboratory measurements of the chemical identity and rate of production secondary organic aerosols (SOA) and their precursors. [Alexander]

    Derived products

  • Identification of mechanisms of aerosol formation, e.g., acid catalyzed reaction.

  • Determination of rates and yields of aerosol processes, and dependence on controlling variables, for processes such as secondary organic aerosol formation and conversion of hydrophobic to hydrophilic aerosol.

    3. INSTRUMENT DEVELOPMENT

    Development of new instruments and methods for measurement of properties of atmospheric aerosols pertinent to direct and indirect radiative forcing and precursors of these aerosols pertinent to their formation and evolution.

    These activities design, construct, deploy, evaluate, and determine the accuracy of new instruments and methods for measurement of properties of atmospheric aerosols (especially properties pertinent to direct and indirect radiative forcing) and precursor species, including comparison with alternative measurement approaches.
    Deliverables consist of accounts (publications, reports, design specifications) of these research activities and data sets resulting from deployment and evaluation of these instruments and methods.

    Specific deliverables

  • Proton transfer reaction - ion trap mass spectrometer for rapid, real-time aircraft speciation and quantification of gas-phase organics. [Alexander/Jobson]

  • Particle into liquid sampler - oxidative/conductimetric analyzer for rapid, real-time aircraft measurement of aerosol organic carbon. [Lee]

  • Coupled mobility particle sizer - chemical ionization mass spectrometer for speciation of organics in aerosol particles. [McMurry]

  • Fluorimetric system for rapid, real-time aircraft measurement of gaseous hydroperoxyl radical, hydroperoxides, and ammonia. [Lloyd]

  • Multi-channel aerosol mobility size spectrometer for rapid determination of particle size distributions in aircraft measurements. [Wang]

  • Polar nephelometer to measure aerosol angular scattering and polarization. [Paulson/Liou]

  • Photothermal interferometer system for direct measurement of aerosol absorption. [Sedlacek]

  • Ultrafiltration-spectrophotometric method for the characterization and quantitative determination of the highly absorbing "humic-like" substances in aerosol particles. [Marley]

    4. MODELS, MODULES, AND PARAMETERIZATIONS

    Modules representing chemical reactions and microphysical processes of atmospheric aerosols suitable for incorporation in large-scale chemical transport models and climate models representing direct and indirect radiative forcing by atmospheric aerosols, together with estimates of their uncertainties, as determined by evaluation in field measurement campaigns and/or laboratory studies.

    Models are a key transferable product of research conducted in this program, serving as input to investigators examining aerosol radiative forcing and climate response to this and other forcings on regional global scales. As aerosol properties and processes are inherently local, emphasis is given to development and evaluation of modules, computer codes that describe aerosol properties and the evolution of these properties on local scales, so-called box-models or zero-dimensional models. However it is essential that such models be capable of being applied in higher-dimensional models, both for purpose of evaluating model performance using data from ASP field measurements and other sources, and for assuring the utility of these modules as components of higher-dimensional models.

    Specific deliverables

  • A new cloud microphysics module capable of tracking transformations of cloud condensation nuclei inside cloud droplets. This new module linked with both a detailed cloud resolving model (CRM) and a Lagrangian parcel framework will provide benchmark simulations for evaluating simplified treatments of aerosol processing used in large-scale models, including WRF-Chem. [Ovtchinnikov, Easter]

  • A parameterization for atmospheric new particle formation enhanced by organic acids. [McGraw]

  • A parameterization for coupled nucleation and growth rates in the presence of background aerosol, suitable for incorporation into chemical transport and climate models, for assessment studies, and for interpretation of field measurements. The accuracy of this parameterization will be tested using box models and plume dispersion models and through comparisons with field measurements. [McGraw]

  • Fully-explicit mechanisms for secondary organic aerosol (SOA) formation along with a repository of measured and estimated kinetic, mechanistic, thermodynamic, and spectroscopic data. [Madronich]

  • Comprehensive SOA-inorganic model representation of gas-particle partitioning, acid-catalyzed SOA chemistry, and physical properties. [Madronich, Seinfeld, Zaveri]

  • Size- and composition-resolved gas-aerosol Lagrangian box-model incorporating laboratory findings on SOA formation, BC aging, and heterogeneous chemistry. [Zaveri]

  • Box, column, and 3-D model evaluation and interpretation of MAX-Mex field observations. [Atherton, Fast, Kotamarthi, Madronich, Wright/Schwartz, Zaveri]

  • A fully-coupled meteorology-chemistry-aerosol model, WRF-chem, that has been evaluated by field measurements will be made publicly available to the atmospheric and global climate modeling communities via the Weather Research and Forecasting (WRF) model framework. [Fast]

  • Simulated 3-D fields of aerosol mass, size distribution, composition, optical properties, and radiative forcing using WRF-chem that have been evaluated with ASP measurements made during the 2004 International Consortium of Atmospheric Research on Transport and Transformation Project (ICARRT) and 2006 Megacity Aerosol Experiment in Mexico City (MAX-Mex) field campaigns will be made available to other scientists for further analysis. [Fast]

  • A single-column module for treating cloud processing of pollutants which efficiently uses cloud-scale transport and microphysical information from a cloud-resolving model. [Ghan, Easter, Berg]

  • A parameterized cumulus scheme designed to represent the effects of cumuliform clouds on the regional-scale redistribution of aerosols and changes to their optical properties following transport through clouds. [Berg, Zaveri, Berkowitz]

  • A coupled column aerosol-chemistry-pbl dynamics and radiation model. This will have detailed chemistry of the gas phase, aerosol phase, organic and inorganic aerosols, highly resolved PBL with 2.5 level PBL closure model and RRTM radiation model. [Kotamarthi]

  • A regional scale coupled model for aerosol-chemistry (full suite of gas phase and aerosol chemistry), meteorology ( MM5/WRF) , and radiation suitable for evaluating regional scale climate change issues. [Kotamarthi]

    5. DISSEMINATION OF RESEARCH RESULTS

    Self documenting, publicly accessible data archive
    Publicly available descriptions and codes of aerosol evolution modules, together with pertinent documentation

    Peer reviewed accounts of research published in appropriate scientific journals

    Special issues of appropriate scientific journals

    Special sessions in national and international meetings of appropriate scientific societies



    Ashley Williamson
    Climate Change Research Division
    Germantown Building
    U.S. Department of Energy SC-23.3
    1000 Independence Avenue SW
    Washington    DC    20585 - 1290
    (301) 903-3120
    Fax: (301) 903-8519
    Email: Ashley.Williamson@science.doe.gov

      This page was last updated 17Oct2006

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