Progress on Application of Modal Aerosol Dynamics to CAM

Similar documents
Testing MOSAIC aerosol scheme implemented in CESM and evaluation with observations

Aerosol modeling with WRF/Chem

Dependence of Radiative Forcing on Mineralogy in the Community Atmosphere Model

CHAPTER 8. AEROSOLS 8.1 SOURCES AND SINKS OF AEROSOLS

AEROCOM-Workshop,Paris, June 2-3, model. Øyvind Seland; Alf Kirkevåg

Aerosols AP sizes AP types Sources Sinks Amount and lifetime Aerosol radiative effects. Aerosols. Trude Storelvmo Aerosols 1 / 21

On-line Aerosols in the Oslo Version of CAM3: Some shortcomings. Seland,

The Sensitivity of Global Nucleation, CCN and Climate to SO2 and Criegee-Intermediate Chemistry

Aerosol Dynamics. Antti Lauri NetFAM Summer School Zelenogorsk, 9 July 2008

Introduction to HadGEM2-ES. Crown copyright Met Office

Introduction to aerosol modeling with WRF/Chem

Can a change of single scattering albedo in Amami-Oshima in a low pressure condition be explained by GCM simulations?

Implications of Sulfate Aerosols on Clouds, Precipitation and Hydrological Cycle

Response to Referee 2

Slides partly by Antti Lauri and Hannele Korhonen. Liquid or solid particles suspended in a carrier gas Described by their

Effective radiative forcing in the aerosol climate model CAM5.3- MARC-ARG

How good are our models?

Direct radiative forcing due to aerosols in Asia during March 2002

Impacts of aerosols in the CORDEX-Europe domain using the regional aerosol-climate model REMO-HAM

Polar Ozone Depletion and Trends as Represented by the Whole Atmosphere Community Climate Model (WACCM)

UKCA_RADAER Aerosol-radiation interactions

Aerosol Basics: Definitions, size distributions, structure

Status/Updates of CAM4/5 Chemistry

Outline. What is Cloud Microphysics Different Approaches CAM implementafon of Microphysics Aerosol Modeling OpFons in CAM InteracFons

Physio-chemical and Optical Characterization of Anthropogenic and Natural Aerosol: Implications for Assessing Global Effects

Descrip(on of Chemistry, Aerosols in CESM and WACCM

The effects of dust emission on the trans- Pacific transport of Asian dust in the CESM

AEROSOL PROPERTIES AND PROCESSES A Path from Field and Laboratory Measurements to Global Climate Models

Atmospheric Aerosols: Size Distributions and Composition

Understanding the importance of chemistry representation in CESM1-CAM5

Standalone simulations: CAM3, CAM4 and CAM5

Aerosol type how to use the information from satellites for models???

The Atmosphere. All of it. In one hour. Mikael Witte 10/27/2010

Modelling of Saharan dust transport to the Southern Italy

Precipitation Processes METR σ is the surface tension, ρ l is the water density, R v is the Gas constant for water vapor, T is the air

Parameterization of the nitric acid effect on CCN activation

Aerosol Effects on Water and Ice Clouds

Aerosol. Challenge: Global Warming. Observed warming during 20 th century, Tapio. 1910s. 1950s. 1990s T [Kelvin]

Global transport of POPs: the role of aerosol particles

P = x i. P i. = y i. Aerosol and Aqueous Chemistry. Raoult s Law. Raoult s Law vs. Henry s Law. or C i. = HC i. = k H

Aerosols and climate. Rob Wood, Atmospheric Sciences

Implementation of modules for wet and dry deposition into the ECMWF Integrated Forecast System

MIRAGE: Model description and evaluation of aerosols and trace gases

The Atmospheric Chemistry and Physics of Ammonia

Differences in the aerosol indirect effect between simulations with GEOS-Chem Bulk and TOMAS. Jack Kodros & Jeff Pierce

What is PRECIS? The Physical Parameters Boundary Conditions Why the Mediterranean Basin? The Sulfur Cycle & Aerosols Aerosols Impacts Data Analysis

Radiative forcing of fine ash and volcanic sulphate aerosol. sulphate aerosol after a very large Northern hemisphere mid-latitude eruption

The Fate of Saharan Dust Across the Atlantic and Implications for a Central American Dust Barrier

Annual mean AOT by MODIS/Terra in 2006

Updated H 2 SO 4 -H 2 O binary homogeneous nucleation look-up tables

Sulfur Biogeochemical Cycle

model to data comparison over Europe for year 2001

Dust in the Earth System EESC G9910

Short-term modulation of Indian summer monsoon rainfall bywest Asian dust

Stratospheric sulfate geoengineering has limited efficacy and increases tropospheric sulfate burdens

1 Executive summary. 2 Research activities and results

SPCAM5: Multi-scale Modeling of Aerosols, Clouds and Precipitation

CONTENTS 1 MEASURES OF ATMOSPHERIC COMPOSITION

Predicting cloud droplet number concentration in Community Atmosphere Model (CAM)-Oslo

Updated Dust-Iron Dissolution Mechanism: Effects Of Organic Acids, Photolysis, and Dust Mineralogy

Study of the Effects of Acidic Ions on Cloud Droplet Formation Using Laboratory Experiments

Aerosol size-dependent below-cloud scavenging by rain and snow in the ECHAM5-HAM

J. Schneider & Chr. Voigt - Physics and Chemistry of Aerosols and Ice Clouds

Impact of new particle formation on the concentrations of aerosols and cloud condensation nuclei around Beijing

CESM1.0/WACCM4 with CARMA3.0 Microphysics. Michael Mills Charles Bardeen

Aerosols-Cloud-Precipitation Interactions in the Climate System. Meinrat O. Andreae Max Planck Institute for Chemistry Mainz, Germany

Supporting Information

Chasing Aerosol Particles Down to Nano Sizes

Professional English

Updates to CAM-chem. Jean-François Lamarque National Center for Atmospheric Research (on leave at NOAA)

Importance of Composition and Hygroscopicity of BC Particles to the Effect of BC Mitigation on Cloud Properties: Application to California Conditions

Modelling aerosol-cloud interations in GCMs

SATELLITE AEROSOL COMPOSITION RETRIEVAL

A study on characterization, emission and deposition of black carbon over Indo- Gangetic Basin

Update on CAM and the AMWG. Recent activities and near-term priorities. by the AMWG

TOWARD ASSESSING THE EFFECT OF AEROSOLS ON DEEP CONVECTION: A NUMERICAL STUDY USING THE WRF-CHEMISTRY MODEL

Assessment of the global impact of aerosols on tropospheric oxidants

Importance of vertical velocity variations in the cloud droplet nucleation process of marine stratus clouds

A cloud microphysics model including trace gas condensation and sulfate chemistry

representing in-cloud oxidation of sulfur in a particle-based cloud-microphysics scheme

The Interaction between Climate Forcing and Feedbacks From the global scale to the process level

Effects of Externally-Through-Internally-Mixed Soot Inclusions Within Clouds and Precipitation on Global Climate

Introduction Methodology Some early results Conclusion Questions. Production-tagged aerosols in NorESM

Review of the IMPROVE Equation for Estimating Ambient Light Extinction

Chemical characteristics of aerosols over Arabian Sea & Bay of Bengal: Impact of Anthropogenic Sources. Manmohan Sarin

Aerosol/Transport issues in VOCALS region

Aerosol Composition and Radiative Properties

Aerosol-Cloud-Radiation Interactions in Atmospheric Forecast Models

Cloud Condensation Nuclei Hygroscopic Parameter Kappa

Chapter Eight: Conclusions and Future Work

New capabilities with high resolution cloud micro-structure facilitated by MTG 2.3 um channel

Indices of Refraction of Absorptive Aerosol Their Importance and Complexity

Online Coupled Meteorology and Chemistry Models in the U.S.

ROBUSTNESS ANALYSIS OF ATMOSPHERIC AEROSOL REMOVAL BY PRECIPITATION

Potential impacts of aerosol and dust pollution acting as cloud nucleating aerosol on water resources in the Colorado River Basin

Introduction. Effect of aerosols on precipitation: - challenging problem - no agreement between the results (quantitative and qualitative)

Introduction to WRF-Chem

Kinetic Limitations on Cloud Droplet Formation and Impact on Cloud Albedo

modeling system Steven Peckham WRF/Chem web site -

Description and evaluation of GMXe: a new aerosol submodel for global simulations (v1)

Transcription:

Progress on Application of Modal Aerosol Dynamics to CAM Xiaohong Liu, Steve Ghan, Richard Easter, Rahul Zaveri, Yun Qian (Pacific Northwest National Laboratory) Jean-Francois Lamarque, Peter Hess, Natalie Mahowald, Francis Vitt, (NCAR)

Current Aerosol Treatment in CAM3 hydrophobic black carbon sea salt 1 soil dust 1 ammonium hydrophobic organic carbon sea salt 2 soil dust 2 hydrophilic black carbon sea salt 3 soil dust 3 secondary organic carbon hydrophilic organic carbon sea salt 4 soil dust 4

Current Weaknesses in CAM Aerosol species are externally mixed (individual particles are composed of only a single species).

Current Weaknesses in CAM Aerosol species are externally mixed (individual particles are composed of only a single species). Their size distribution is prescribed ( is diagnosed from the predicted mass). Processes that should only affect mass (condensation, chemistry) also affect. Processes that only affect (nucleation, coagulation) are neglected.

Current Weaknesses in CAM Aerosol species are externally mixed (individual particles are composed of only a single species). Their size distribution is prescribed ( is diagnosed from the predicted mass). Processes that should only affect mass (condensation, chemistry) also affect. Processes that only affect (nucleation, coagulation) are neglected. Hydrophobic carbon ages to hydrophilic with prescribed timescale

Proposed Benchmark Aerosol Treatment for CAM4 Aitken water ammmonium coagulation condensation Accumulation water ammonium hydrophobic OC BC Fine Soil Dust water soil dust ammonium Fine Sea Salt water sea salt ammonium All modes log-normal with prescribed width. Total transported aerosol tracers: 32 (42) Cloud-borne aerosol predicted but not transported. Primary Carbon hydrophobic OC BC Coarse Soil Dust water soil dust ammonium Coarse Sea Salt water sea salt ammonium

Proposed Simplified Aerosol Treatment for CAM4 Assume aerosol are hydrated for RH > crystalization RH. Carry soil dust and sea salt in same mode because sources are separate. Assume primary carbon is internally mixed with secondary aerosol. Assume ammonium neutralizes, and neglect. Aitken Accumulation primary OC black carbon Fine soil dust sea salt Coarse soil dust sea salt coagulation condensation All modes are log-normal with prescribed width. Total transported aerosol tracers: 15 Cloud-borne aerosol are predicted but not transported.

Progress Emissions (size-resolved) (done) Fossil fuel SO2 emissions over 0-100 m and >100 m based on EDGAR-2000; 3% (by mole) of fossil fuel SO2 emissions goes to SO4 (Aitken & Accu. modes, mass &, Whitby 1978); OM and BC to primary carbon mode (mass & no.); Sea salt emission based on Gong et al (1997) to fine and coarse sea salt modes (mass & no.); Dust emissions to fine and coarse dust modes (mass & no.).

Progress Aerosol activation and droplet nucleation (Ghan scheme) (done) Wet scavenging (done) In-cloud rainout based on activated aerosol; Below-cloud impaction scavenging rates (mass & no.) using a look-up table (wet size, precipitation rate). Dry deposition (based on Zhang et al., 2001) & gravitational settling (done) Cloud sulfur chemistry (done) Bulk chemistry based on calculated ph Sulfate mass produced distributed to modes based on of activated aerosols in modes. Include contribution from H2SO4 (g) uptakes

Progress New particle formation: binary nucleation (H2SO4-H2O) parameterization (Vehkamaki et al., 2002) (done) Coagulation: Brownian within, between modes. (done) Water vapor and trace gas (H2SO4 & NH3) uptake (done) Intermode transfer (renaming) due to condensation, coagulation, and cloud chemistry (done) Compile OK

Works in Progress Trace gas and water vapor uptake (with hysteresis dependent on previous aerosol water) will be replaced with MOSAIC module (consider gas-particle transfer) Aerosol optical properties: parameterization in terms of wet refractive index and wet surface mode radius.

CAM Simulations Benchmark modal present-day On-line oxidants (HO x,o 3 chemistry) Off-line oxidants (input HO x,o 3 ) Benchmark modal pre-industrial Simplified modal present day, offline oxidants Simplified modal pre-indu., offline oxidants Offline benchmark present day (interpolation from monthly mean of on-line benchmark) Offline benchmark pre-industrial

Testing Evaluate on-line benchmark treatment using in situ (surface and aloft) and remote aerosol measurements (mass,, size, CCN, AOD,...). Utilize AEROCOM and other model evaluation efforts. Evaluate approximations used in on-line simplified treatment by comparing direct and indirect aerosol effects with on-line benchmark treatment. Evaluate off-line benchmark treatment by comparing with on-line benchmark treatment.