1 Two-Dimensional Chemistry Transport Model 11/16/2006.

Slides:



Advertisements
Similar presentations
Institut für Physik der Atmosphäre Institut für Physik der Atmosphäre Climate-Chemistry Interactions - User Requirements Martin Dameris DLR-Institut für.
Advertisements

Institut für Physik der Atmosphäre Ensemble Climate-Chemistry simulations for the past 40 years Volker Grewe and the DLR/MPI Team Institut für Physik der.
DEVELOPMENT AND PRELIMINARY RESULTS OF A LIMITED AREA ATMOSPHERE-CHEMISTRY MODEL: BOLCHEM M. D’Isidoro (1),S. Fuzzi (1), A. Maurizi (1), F. Monforti (2),
Institute for Climate and Atmospheric Science SCHOOL OF EARTH AND ENVIRONMENT 3D SLIMCAT Studies of Arctic Ozone Loss Wuhu Feng Acknowledgments: Martyn.
Scientific Advisory Committee Meeting, November 25-26, 2002 Modeling of the Middle and Upper Atmosphere M. A. Giorgetta E. Manzini 1, M. Charron 2, H.
ISSI Meeting, Bern January 2014 New 3D photochemical global model with ions in D-region: The instrument for solar-atmospheric relations study Alexei.
Modeling the Distribution of H 2 O and HDO in the upper atmosphere of Venus Mao-Chang Liang Research Center for Environmental Changes, Academia Sinica.
Modeling the Distribution of H 2 O and HDO in the upper atmosphere of Venus Mao-Chang Liang Research Center for Environmental Changes, Academia Sinica.
Using global models and chemical observations to diagnose eddy diffusion.
By studying the case with QBO signal only, the model reproduces the previous observation that QBO signal of column ozone at equator is anti-correlated.
Modeling Carbon Species in the Atmosphere of Neptune and Comparison with Spitzer Observations Xi Zhang 1, Mao-Chang Liang 2, Daniel Feldman 1, Julianne.
The equatorial QBO affects the polar stratosphere during winter with the easterly phase of the QBO (e-QBO) creating the condition for a more perturbed.
Chemistry and Transport in the Lower Stratosphere Wuhu Feng 1, Martyn Chipperfield 1, Howard Roscoe 2 1. Institute for Atmospheric Science, School of the.
Modeling of OCS in the Lower Atmosphere of Venus Yuk L. Yung M. C. Liang, X. Jiang, C. Lee, B. Bezard and E. Marq California Institute of Technology
The comparison of TransCom continuous experimental results at upper troposphere Takashi MAKI, Hidekazu MATSUEDA and TransCom Continuous modelers.
1 Non-stationary Synchronization of Equatorial QBO with SAO in Observation and Model 1. Division of Geological and Planetary Sciences, California Institute.
Stratospheric NO y Studies with the SLIMCAT 3D CTM Wuhu Feng, Stewart Davies, Jeff Evans and Martyn Chipperfield School of the Environment, University.
1 Interannual Variability in Stratospheric Ozone Xun Jiang Advisor: Yuk L. Yung Department of Environmental Science and Engineering California Institute.
Chemical Sources and Sinks of OCS in the Lower Atmosphere of Venus Yuk L. Yung M. C. Liang, California Institute of Technology EGU.
EQUATORIAL WAVES part 2: Vertical Propagation & the QBO.
Titan's photochemical model: neutral species L.M. Lara IAA-CSIC Granada, Spain.
Three-Dimensional Chemical Transport Model Studies of Arctic Ozone Depletion Wuhu Feng and Martyn Chipperfield School of the Earth and Environment, University.
Larger Chemical Ozone Loss in 2004/2005 Arctic Winter/Spring Wuhu Feng and Martyn Chipperfield School of Earth and Environment, University of Leeds Acknowledgments.
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.
Solar Forcing on Climate Through Stratospheric Ozone Change Le Kuai.
(a)(b)(c) Simulation of upper troposphere CO 2 from two-dimensional and three-dimensional models Xun Jiang 1, Runlie Shia 2, Qinbin Li 1, Moustafa T Chahine.
1 The 1D model of IPSL : IPSL05 Intercomparison of 1D photochemical models of Titan atmosphere Nathalie Carrasco Workshop ISSI Bern th march 2009.
Influence of the sun variability and other natural and anthropogenic forcings on the climate with a global climate chemistry model Martin Schraner Polyproject.
1 Planetary Wave-Induced Ozone Heating and its Effect on Troposphere-Stratosphere Communication Terry Nathan Atmospheric Science Program University of.
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.
*K. Ikeda (CCSR, Univ. of Tokyo) M. Yamamoto (RIAM, Kyushu Univ.)
Using GPS data to study the tropical tropopause Bill Randel National Center for Atmospheric Research Boulder, Colorado “You can observe a lot by just watching”
Analysis of a simulation with prognostic ozone in ARPEGE-Climat Jean-François Royer, Hubert Teysseidre, Hervé Douville, Sophie Tyteca Meteo-France,
The effects of solar variability on the Earth’s climate Joanna D. Haigh 2010/03/09 Pei-Yu Chueh.
Intermediate model for the annual and global evolution of species
General Circulation Modelling on Triton and Pluto
1 JRA-55 the Japanese 55-year reanalysis project - status and plan - Climate Prediction Division Japan Meteorological Agency.
V/1 Atmospheric transport and chemistry lecture I.Introduction II.Fundamental concepts in atmospheric dynamics: Brewer-Dobson circulation and waves III.Radiative.
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.
IAC ETH, 26 October 2004 Sub-project: Effects of Solar irradiance variability on the atmosphere (steady-state sensitivity study) Progress report (final)
1 Longitudinally-dependent ozone recovery in the Antarctic polar vortex revealed by satellite-onboard ILAS-II observation in 2003 Kaoru Sato Department.
Camp et al. (2003) illustrated that two leading modes of tropical total ozone variability exhibit structrures of the QBO and the solar cycle. Figure (1)
EVAT 554 OCEAN-ATMOSPHERE DYNAMICS EQUATIONS OF MOTION (CONT); ENERGY EQUATION LECTURE 4 (Reference: Peixoto & Oort, Chapter 3)
Response of the Earth’s environment to solar radiative forcing
10-11 October 2006HYMN kick-off TM3/4/5 Modeling at KNMI HYMN Hydrogen, Methane and Nitrous oxide: Trend variability, budgets and interactions with the.
Mao-Chang Liang 1,2, Claire Newman 3, Yuk L. Yung 3 1 Research Center for Environmental Changes, Academia Sinica, Taipei, Taiwan 2 Graduate Institute of.
Dynamical Influence on Inter-annual and Decadal Ozone Change Sandip Dhomse, Mark Weber,
NCAR Advanced Study Program (ASP) Seminar, February 13, Solar Semidiurnal Tide in the Atmosphere Jeff Forbes Department of Aerospace Engineering.
Impact of solar UV variability on sudden stratospheric warming with LMDz-Reprobus A. Hauchecorne 1, S. Bekki 1, M. Marchand 1, C. Claud 2, P. Keckhut 1,
X. Zhang 1, R. Shia 1, M. Liang 2, C. Newman 1, D. Shemansky 3, Y. Yung 1, 1 Division of Geological and Planetary Sciences, California Institute of Technology,
Intro to Modeling – Terms & concepts Marti Blad, Ph.D., P.E. ITEP
slide 1 Polar Ozone: Past and present Chapter 4 of WMO 2006 Ozone Assessment Summary Part 1 Polar stratospheric observations update Part 2 Progress.
Nansen Environmental and Remote Sensing Center Modifications of the MICOM version used in the Bergen Climate Model Mats Bentsen and Helge Drange Nansen.
Developing General Circulation Models for Hot Jupiters
(a)(b)(c) Simulation of upper troposphere CO 2 from two-dimensional and three-dimensional models Xun Jiang 1, Runlie Shia 2, Qinbin Li 1, Moustafa T Chahine.
Dynamical Constraints on the Gravity Wave Source Spectrum Used in a Parameterization of Gravity Wave Forcing David Ortland NorthWest Research Associates.
Troposphere Strastosphere D. H. Gas phase chemistry Scavenging processes Fossil fuel Emissions Biomass burning emissions Biogenic emissions Boundary layer.
Multivariate Time Series Analysis Charles D. Camp MSRI July 18, 2008.
Tropical Convection and MJO
Influence of Convective Momentum Transport on Tropical Waves
Global dynamics in the MLT region
A model of sea salt aerosol for Cape Grim Preliminary investigations
Mathematics in Chemistry
Tomoko Matsuo DAI/GSP *in collaboration with Jeff Anderson(DAI),
ATOC 4720 class37 1. The vertically averaged divergence
Models of atmospheric chemistry
Extratropical stratoshere-troposphere exchange in a 20-km-mesh AGCM
Wildfire Plume Height Simulations
O2 O2 CH4 H2O CO2 H2O2 CH3OH O2 O2 CH4 H2O CO2 H2O2 CH3OH O2 O2 CH4
VarSITI Closing Simposium, Sofia, Bulgaria, June 2019
Presentation transcript:

1 Two-Dimensional Chemistry Transport Model 11/16/2006

2 Overview  Offline 2-D CTM (Caltech/JPL Kinetics model)  ThinAir Model (Two-and-a-Half-dimesional INter-Active Isentropic Research model, J. Kinnersley and K. K. Tung)  Discussion

3 Continuity Equation for Chemical Species (Morgan et al. 2004) 1.Advection (V and W or Streamfuction) 2. Eddy Diffusion (Kyy) 3. Vertical Diffusion (Kzz) 4. Chemical Sources and Sinks 5. Resolution and Vertical Coordinate 6. Numeical Scheme and Time Spliting

4 Interactive 2-D CTM 1.Dynamics Model 2.Radiation code 3.Chemistry Transport Model 4.Interactions between the three Modules

5 ThinAir Model 1.Isentropic Coordinate 2.Two and a Half Dimensional Dynamics Model (zonally averaged dynamics plus three longest planetary waves) 3.Planetary Wave Breaking Parameterization for Kyy 4.Gravity Wave Breaking Parameterization for Kzz

6 ThinAir Model 5. Radiation (J. Haigh, 1984): UV and Visible (O3 and O2) NIR (H2O, CO2, O2, CH4 and N2O) IR (H2O, CO2 and O3)

7 ThinAir Model 6. Chemistry: 45 Species Rate Data from DeMore et al. (1992) PSC Parameterization and Heterogeneous Reactions

8 ThinAir Model 7. QBO-Source Term in the Momentum Equation: Wave Parameterization (Kinnersley, 1996b) Kelvin Waves and Rossby-Gravity Waves or Relaxation to Observed QBO (Singapore, 80-93) Winds (Kinnersley, 1998)

9 Discussions 1. Climatology (Kinnersley, 1996) 2. Modification and Updating: Adding Solar Cycle QBO data and Lower Boundary Condition for Planetary Waves Extended to The use of ThinAir