Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.

Slides:



Advertisements
Similar presentations
year analysis Upgrade + integration Direct model implementation BB sources Soil dust 1D-VAR /4D-VARadjointization analysis Evaluation.
Advertisements

Whitecaps, sea-salt aerosols, and climate Magdalena D. Anguelova Physical Oceanography Dissertation Symposium College of Marine Studies, University of.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Global Change Research in Belgium Guy P. Brasseur Max Planck Institute for Meteorology Chair, International Geosphere Biosphere Programme (IGBP)
CMIP5: Overview of the Coupled Model Intercomparison Project Phase 5
School of Earth and Environment INSTITUTE FOR CLIMATE AND ATMOSPHERIC SCIENCE Dust – Climate Interactions Kerstin Schepanski k.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Discussion Space Research Centre. Urbanization and Industrialization: in 2008, more than half of humans live in cities UN Population Report 2007.
DARGAN M. W. FRIERSON DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 16: 05/20/2010 ATM S 111, Global Warming: Understanding the Forecast.
Climate modeling Current state of climate knowledge – What does the historical data (temperature, CO 2, etc) tell us – What are trends in the current observational.
Clouds and Climate: Forced Changes to Clouds SOEE3410 Ken Carslaw Lecture 4 of a series of 5 on clouds and climate Properties and distribution of clouds.
Environmentally Conscious Design & Manufacturing (ME592) Date: March 29, 2000 Slide:1 Environmentally Conscious Design & Manufacturing Class 11: Air Quality.
Air Quality-Climate Interactions Aijun Xiu Carolina Environmental Program.
What are aerosols ? Aerosol is a collection of particles suspended in the air, they range in size from 0.01 microns to several tens of microns.
Urban Air Pollution, Tropospheric Chemistry, and Climate Change: An Integrated Modeling Study Chien Wang MIT.
Intercontinental Transport and Climatic Effects of Air Pollutants Intercontinental Transport and Climatic Effects of Air Pollutants Workshop USEPA/OAQPS.
METR112-Climate Modeling Basic concepts of climate Modeling Components and parameterization in the model sensitivity of the model.
METO 637 Lesson 13. Air Pollution The Troposphere In the Stratosphere we had high energy photons so that oxygen atoms and ozone dominated the chemistry.
ARM Atmospheric Radiation Measurement Program. 2 Improve the performance of general circulation models (GCMs) used for climate research and prediction.
METR112-Climate Modeling Basic concepts of climate Modeling Components and parameterization in the model sensitivity of the model.
Federal Science Research on the Role of Aerosols in Climate Change Sylvia A. Edgerton * National Science Foundation Workshop on Secondary Organic Aerosols,
STRATOSPHERIC CHEMISTRY. TOPICS FOR TODAY 1.Review of stratospheric chemistry 2.Recent trends in stratospheric ozone and forcing 3.How will stratospheric.
Clouds and Climate: Forced Changes to Clouds SOEE3410 Ken Carslaw Lecture 4 of a series of 5 on clouds and climate Properties and distribution of clouds.
Radiation’s Role in Anthropogenic Climate Change AOS 340.
4. Models of the climate system. Earth’s Climate System Sun IceOceanLand Sub-surface Earth Atmosphere Climate model components.
Next Gen AQ model Need AQ modeling at Global to Continental to Regional to Urban scales – Current systems using cascading nests is cumbersome – Duplicative.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
CMAQ (Community Multiscale Air Quality) pollutant Concentration change horizontal advection vertical advection horizontal dispersion vertical diffusion.
Aerosol Microphysics: Plans for GEOS-CHEM
A Modeling Investigation of the Climate Effects of Air Pollutants Aijun Xiu 1, Rohit Mathur 2, Adel Hanna 1, Uma Shankar 1, Frank Binkowski 1, Carlie Coats.
Modelling the Canadian Arctic and Northern Air Quality using GEM-MACH Wanmin Gong and Stephen Beagley Science and Technology Branch Environment Canada.
Clouds, Aerosols and Precipitation GRP Meeting August 2011 Susan C van den Heever Department of Atmospheric Science Colorado State University Fort Collins,
Report on March Crystal City Workshop to Identify Grand Challenges in Climate Change Science By its cochair- Robert Dickinson For the 5 Sept
Global models. Content Principles of Earth System Models and global models Global aerosol models as part of Earth System Models Model input Computation.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Biosphere/Atmosphere Interactions in the Tropics.
Climate Modeling at GFDL: The Scientific Challenges V. Ramaswamy NOAA/ Geophysical Fluid Dynamics Laboratory November 12, 2008.
Status of the Sea Ice Model Testing of CICE4.0 in the coupled model context is underway Includes numerous SE improvements, improved ridging formulation,
Research Needs for Decadal to Centennial Climate Prediction: From observations to modelling Julia Slingo, Met Office, Exeter, UK & V. Ramaswamy. GFDL,
Coupling between the aerosols and hydrologic cycles Xiaoyan Jiang Climatology course, 387H Dec 5, 2006.
Linking Anthropogenic Aerosols, Urban Air Pollution and Tropospheric Chemistry to Climate ( actually, to CAM/CCSM ) Chien Wang Massachusetts Institute.
Wildland Fire Impacts on Surface Ozone Concentrations Literature Review of the Science State-of-Art Ned Nikolov, Ph.D. Rocky Mountain Center USDA FS Rocky.
Chemistry-Climate Working Group Meeting (March 22-24, 2006) Background –SSC expectations and the next IPCC (Bill Collins) Summarize where we are now Discuss.
Workshop on Tropical Biases, 28 May 2003 CCSM CAM2 Tropical Simulation James J. Hack National Center for Atmospheric Research Boulder, Colorado USA Collaborators:
Aerosols and climate - a crash course Marianne T. Lund CICERO Nove Mesto 17/9-15.
The Basic Research Model Models/Theory NWP GCM/CSMs Process Mods. Observations Soundings Satellites Surface Obs. Predictions Boundary Conditions Initial.
REGIONAL/GLOBAL INTERACTIONS IN ATMOSPHERIC CHEMISTRY Greenhouse gases Halocarbons Ozone Aerosols Acids Nutrients Toxics SOURCE CONTINENT REGIONAL ISSUES:
Dust aerosols in NU-WRF – background and current status Mian Chin, Dongchul Kim, Zhining Tao.
Presented by LCF Climate Science Computational End Station James B. White III (Trey) Scientific Computing National Center for Computational Sciences Oak.
Understanding The Effect Of Anthropogenic Aerosol Weekly Cycles Upon The Climate Using A Global Model Of Aerosol Processes (GLOMAP) Introduction GLOMAP.
Chien Wang Massachusetts Institute of Technology A Close Look at the Aerosol-Cloud Interaction in Tropical Deep Convection.
Case 5: Tracer Transport in Deep Convection STERAO-1996 From Dye et al. (2000)
March 31, 2004BGC Working Group Interactive chemistry in CAM Jean-François Lamarque, D. Kinnison and S. Walters Atmospheric Chemistry Division NCAR.
Radiative Forcing of Climate Change: Expanding the Concept and Addressing Uncertainties Report from the NRC Committee on Radiative Forcing of Climate commissioned.
Troposphere Strastosphere D. H. Gas phase chemistry Scavenging processes Fossil fuel Emissions Biomass burning emissions Biogenic emissions Boundary layer.
School of Earth and Environment INSTITUTE FOR CLIMATE AND ATMOSPHERIC SCIENCE The UK Chemistry and Aerosol Project (UKCA)
March 9, 2004CCSM AMWG Interactive chemistry in CAM Jean-François Lamarque, D. Kinnison S. Walters and the WACCM group Atmospheric Chemistry Division NCAR.
Mayurakshi Dutta Department of Atmospheric Sciences March 20, 2003
Status of CAM, March 2004 Phil Rasch. Differences between CAM2 and CAM3 (standard physics version) Separate liquid and ice phases Advection, sedimentation.
Lupu, Semeniuk, Kaminski, Mamun, McConnell
Aerosol Physics & Climate
What are the causes of GCM biases in cloud, aerosol, and radiative properties over the Southern Ocean? How can the representation of different processes.
A model of sea salt aerosol for Cape Grim Preliminary investigations
GFDL Climate Model Status and Plans for Product Generation
IPCC Climate Change Report
Modeling the Atmos.-Ocean System
Benchmarking of chemical mechanisms
Presentation transcript:

Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009

Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Atmospheric Chemistry and Physics Synthesis and Future Directions Presented by Hiram Levy Presented by Hiram Levy

3 Atmospheric Physics and Chemistry - Synthesis 3 Recent Accomplishments: Antarctic ozone hole recovery predicted for ~2070 Modeled “significant” stratospheric cooling appears by early 20th century Methane reduction is a win-win for climate and air quality 2-step dissolution mechanism explains a wide range of iron solubility in dust Controls on Asian emissions may significantly impact future US summertime warming On-line interactive aerosols in AM3/CM3 in good agreement with observations Aerosol-cloud interactions produce realistic cloud drop concentrations in AM3/CM3 and dominate aerosol cooling (indirect effects) CM3 is driven by emissions of short-lived species, has interactive aerosols with explicit cloud droplet activation, coupled stratospheric-tropospheric chemistry, dynamic vegetation and comprehensive hydrology Satellite spectral radiance enables a new metric for verifying climate models

4 Future Research Directions 4 In the next 18 months CM3 will be integrated for at least 3000 model years to generate a base-state climate and produce multiple simulations of historical climate and multiple projections of future climate The Next 5 Years Will Also Focus On: Improving existing and incorporating missing individual components of the atmospheric model to clarify their role in and contribution to the earth’s climate and air quality Completing the atmospheric chemistry-climate loop to evaluate the nature, size and sensitivity of air quality–climate interactions and feedbacks Increasing horizontal and vertical resolution to improve physical and chemical realism and enhance our understanding of regional climate forcing, change and air quality

5 Use high-spectral-resolution in the radiation code to evaluate the climate model's radiation budget and investigate the accuracy of feedbacks Develop self-consistent radiation codes for heating-cooling (climate) and photodissociation (chemistry) Address cloud feedbacks, improve cloud radiative properties and include the indirect effect in deep convection, by incorporating multi-moment microphysics (including ice) in all cloud schemes Implement a new parameterization of both boundary layer mixing and cloud macrophysics to reduce cloud-related deficiencies in surface energy balance Increased realism of global aerosols distributions and properties: More accurate physical representation of the formation of nucleation mode particles, of aerosol activation and of wet removal Microphysical and optical accounting of internal mixing of multiple species Use satellite data (e.g., CO, aerosols,…) to evaluate large-scale tracer transport and distributions (already changed) Improving Atmospheric Physics and Chemistry Components

6 Completing the Atmospheric Chemistry – Climate Cycle Complete the coupling of vegetation, physical climate and atmospheric chemistry models to address: vegetation emissions of reactive compounds soil biogenic emissions of NOx biomass burning emissions of gases and particles formation of secondary organic aerosols Include aerosol surface emission and deposition in the dynamic vegetation module of AM3/CM3 and account for aerosols on snow Couple the oceanic sources of sulfur directly to ocean biogeochemistry

7 Higher resolution (1.0 and 0.5 degree) versions of CM3 will be developed to realistically simulate key physical processes and to predict and assess regional climate at spatial scales approaching those of interest to policymakers Higher resolution is also required to capture non-linearities in emissions and chemistry that will improve air quality simulations and predictions In the next session, Isaac Held will discuss GFDL’s current efforts and future plans for higher resolution model development HIGHER RESOLUTION

Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009