GMI Capabilities Sarah Strode, Jose Rodriguez, Steve Steenrod, Junhua Liu, Susan Strahan, Eric Nielsen.

Slides:



Advertisements
Similar presentations
Martin G. Schultz, MPI Meteorology, Hamburg GEMS proposal preparation meeting, Reading, Dec 2003 GEMS RG Global reactive gases monitoring and forecast.
Advertisements

GEOS-Chem meeting, 12 April 2007 Preliminary results for the year-to-year variation in satellite-derived NOx sources S. Koumoutsaris 1, I. Bey 1, N. Moore.
Using beryllium-7 to assess stratosphere-to- troposphere transport in global models 4 th GEOS-Chem Users’ Meeting Harvard University, April 7-10, 2009.
Seasonal Variations in the Mixing Layer in the UTLS Dave MacKenzie University of Toronto GEOS-Chem Meeting April 2009.
Interannual variations in global OH radicals over the period in GEOS-Chem, and preliminary comparisons to other models I. Bey 1, S. Koumoutsaris.
Bay Area Earth Science Institute (BAESI)
Wuhu Feng and Martyn Chipperfield
Constraints on the Production of Nitric Oxide by Lightning as Inferred from Satellite Observations Randall Martin Dalhousie University With contributions.
Introduction. A major focus of SCOUT-O3 is the tropics and a key issue here is testing how well existing global 3D models perform in this region. This.
GEOS Meteorological and Chemical Data Assimilation Steven Pawson Global Modeling and Assimilation Office NASA GSFC.
Stratosphere–Troposphere Exchange: Isabel RamosÁlvaro.
Hauglustaine et al., IGAC, 19 Sep 2006 Forward and inverse modelling of atmospheric trace gas at LSCE P. Bousquet, I. Pison, P. Peylin, P. Ciais, D. Hauglustaine,
Variability of Tropical to Extra-tropical Transport in the Lower Stratosphere Mark Olsen UMBC/GSFC Anne Douglass, Paul Newman, and Eric Nash.
INTERCONTINENTAL TRANSPORT OF AIR POLLUTION WITH GMI AND PLANS FOR THE NEW HEMISPHERIC TRANSPORT OF AIR POLLUTANTS (HTAP) MODEL INTERCOMPARISON STUDY ROKJIN.
Transport analysis and source attribution of the tropical CO seasonal and interannual variability in the UT/LS Junhua Liu and Jennifer Logan School of.
Seasonal variability of UTLS hydrocarbons observed from ACE and comparisons with WACCM Mijeong Park, William J. Randel, Louisa K. Emmons, and Douglas E.
Past and Future Changes in Southern Hemisphere Tropospheric Circulation and the Impact of Stratospheric Chemistry-Climate Coupling Collaborators: Steven.
Copyright 2007 Northrop Grumman Corporation 1 AURA Runs Megan Rose Damon SIVO - Advanced Software Technology Group Northrop Grumman Information Technology-TASC.
The effect of pyro-convective fires on the global troposphere: comparison of TOMCAT modelled fields with observations from ICARTT Sarah Monks Outline:
Figure (a-c). Latitude-height distribution of monthly mean ozone flux for the months of (a) January, (b) April and (c) July averaged over years 2000 to.
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.
MAP MODELING EFFORTS MAP: Building Integrated Earth System Analysis (Modeling): IESA CTM work funded by MAP will be seen as part of the overall Earth System.
Asian Sources of Methane and Ethane Y. Xiao, D.J. Jacob, J. Wang, G.W. Sachse, D.R. Blake, D.G. Streets, et al. Atmospheric Chemistry Modeling Group Harvard.
1 Ozone depletion: Misconceptions Misconceptions Meteorology 10 De Anza College.
Impact of lightning-NO and radiatively- interactive ozone on air quality over CONUS, and their relative importance in WRF-Chem M a t u s M a r t i n i.
Long-range transport of NO y and O 3 Thomas Walker Dalhousie University Department of Physics & Atmospheric Science December 6, 2006.
GEOS-CHEM users’ meeting Harvard University Gabriele Curci6/2/2003 Stratospheric chemistry and SMVGEAR II in GEOS-CHEM model Gabriele Curci University.
QUESTIONS 1. How does the thinning of the stratospheric ozone layer affect the source of OH in the troposphere? 2. Chemical production of ozone in the.
INTERCONTINENTAL TRANSPORT OF OZONE AND ITS SEASONAL VARIATIONS IN EUROPE Dick Derwent rdscientific 2 nd ICAP Workshop Chapel Hill, North Carolina October.
THE GLOBAL MODELING INITIATIVE (GMI): PAST CURRENT AND FUTURE ACTIVITIES Jose M. Rodriguez RSMAS/MAC University of Miami
Itsushi UNO*, Youjiang HE, Research Institute for Applied Mechanics, Kyushu University, Kasuga, Fukuoka, JAPAN Toshimasa OHARA, Jun-ichi KUROKAWA, Hiroshi.
OVERVIEW OF ATMOSPHERIC PROCESSES: Daniel J. Jacob Ozone and particulate matter (PM) with a global change perspective.
TEMIS User Workshop, Frascati, Italy October 8-9, 2007 Formaldehyde application Derivation of updated pyrogenic and biogenic hydrocarbon emissions over.
A modelling study on trends and variability of the tropospheric chemical composition over the last 40 years S.Rast(1), M.G.Schultz(2) (1) Max Planck Institute.
Model evolution of a START08 observed tropospheric intrusion Dalon Stone, Kenneth Bowman, Cameron Homeyer - Texas A&M Laura Pan, Simone Tilmes, Doug Kinnison.
Constraints on the Production of Nitric Oxide by Lightning as Inferred from Satellite Observations Randall Martin Dalhousie University With contributions.
Vertical transport of chemical compounds from the surface to the UT/LS: What do we learn from SEAC 4 RS? Qing Liang 1 & Thomas Hanisco 2, Steve Wofsy 3,
Status of MOZART-2 Larry W. Horowitz GFDL/NOAA MOZART Workshop November 29, 2001.
Use of GMI to Study Tropospheric and Stratospheric Bromine Budgets Debra Weisenstein AER, Inc. GMI Science Team Meeting March 2008.
Climatic implications of changes in O 3 Loretta J. Mickley, Daniel J. Jacob Harvard University David Rind Goddard Institute for Space Studies How well.
Global Aerosol Forecasting System Applications to Houston/Costa Rica Aura Validation Experiments Arlindo da Silva Global Modeling and Assimilation Office,
Analysis of TES and MLS tropospheric data for ozone and CO in 2005 and 2006 using the GMI and GEOS-Chem global models. Jennifer A. Logan, Ray Nassar, Inna.
OsloCTM2  3D global chemical transport model  Standard tropospheric chemistry/stratospheric chemistry or both. Gas phase chemistry + essential heteorogenous.
MOCA møte Oslo/Kjeller Stig B. Dalsøren Reproducing methane distribution over the last decades with Oslo CTM3.
Analysis of Satellite Observations to Estimate Production of Nitrogen Oxides from Lightning Randall Martin Bastien Sauvage Ian Folkins Chris Sioris Chris.
Proposal Science Issues How will ozone recover over the next few decades in a changing climate? How has past ozone change affected the changing climate.
Controls on the Past and Future Depletion of Antarctic Ozone and the Emergence of Healing Susan Solomon Richards Professor of Atmospheric Chemistry and.
Yuqiang Zhang1, Owen R, Cooper2,3, J. Jason West1
Transport Working Group
A proposal for multi-model decadal hindcast simulations
A New Tropopause Definition for Use in Chemistry-Transport Models
Advisor: Michael McElroy
Atmospheric modelling of the Laki eruption
Randall Martin Dalhousie University
Sensitivity of continental boundary layer chemistry to a new isoprene oxidation mechanism Jingqiu Mao (Harvard), Fabien Paulot (Caltech), Daniel Jacob.
Characteristics of Urban Ozone Formation During CAREBEIJING-2007 Experiment Zhen Liu 04/21/09.
SUMMER 2004 FIELD STUDIES Modeling support by Harvard University
Lu Hu Global budget of tropospheric ozone: long-term trend and recent model advances Lu Hu With Loretta Mickley,
Aura Science Team meeting
Daniel J. Jacob Harvard University
Global Simulation of CH3Cl
Diurnal Variation of Nitrogen Dioxide
Shiliang Wu1 Loretta J. Mickley1, Daniel J
Asian outflow and chemical evolution of ozone and nitrogen oxides over the Pacific Mathew Evans, Daniel Jacob, Harvard Group, TRACE-P Science Team et al.
Harvard University and NASA/GFSC
Lin Zhang, Daniel J. Jacob, Jennifer A
Effects of global change on U.S. ozone air quality
Chemistry and Dynamics in the Lower Stratosphere: Trends in Ozone and HCl The title of this talk is a science result, but this science result is made.
Benchmarking of chemical mechanisms
Climatic implications of changes in O3
Presentation transcript:

GMI Capabilities Sarah Strode, Jose Rodriguez, Steve Steenrod, Junhua Liu, Susan Strahan, Eric Nielsen

Model Information The Global Modeling Initiative (GMI) CTM includes the following: Stratospheric & tropospheric chemistry with 124 species (including the reactive nitrogen species & oxidants measured by Atom), >400 reactions Diagnostics for individual reaction rates Output for specific station locations Specialized tracers including e90, idealized lifetime tracers, tendencies due to chemistry/advection/etc.

Recent GMI Simulations Suite of Long Hindcast simulations: 1990-2012 with time-dependent fossil fuel & biomass burning emissions 1990-2012 with fixed emissions 1979-2012 CCMI hindcast ATom simulations: 1x1.25 degree horizontal resolution, 72 levels (~30 from 0-12km) Meteorology from MERRA (MERRA2 coming soon) Hindcasts possible within 1-3 months of met field availability

Recent Science Highlights Strode et al. (submitted) GMI Hindcast with time-dependent emissions captures observed changes in the annual cycle of U.S. surface O3. Strahan et al. (2014) GMI results suggest that the IAV of tropospheric ozone over Reunion is mainly driven by the IAV of stratospheric contribution.  Inorganic chlorine causes ozone depletion but its level inside the vortex is not measured. We inferred chlorine levels during the past decade using a method that combines MLS N2O data and the time-dependent N2O/Cly correlation determined by the GMI Hindcast. O3 mixing ratio (ppb) StratO3/O3 (%) Liu et al. (in prep) Year

Preliminary ATom Results Prod or Loss (Mmol/day) [NOx] (ppt) Latitude

Relationship to GEOS-5 The GMI chemical mechanism is also included in the GEOS-5 Chemistry Climate Model (GEOSCCM) GEOS-5 can run as a free-running GCM, “replay” to a reanalysis, or run as a CTM (GEOS-CTM) Can use recently produced met fields High resolutions (up to 1/8 degree) are possible

High Resolution GEOSCCM Result