Atmospheric Environment Characterization in Support of the ESA ExoMars Mission Intercomparison LMD – SwRI models T. Bertrand, S. Rafkin, F. Forget, A.

Slides:



Advertisements
Similar presentations
A thermodynamic model for estimating sea and lake ice thickness with optical satellite data Student presentation for GGS656 Sanmei Li April 17, 2012.
Advertisements

Radiative transfer simulations of the ATR-42 and Falcon 20 SW and LW radiation profiles above the ENEA Lampedusa supersite during the ChArMEx/ADRIMED SOP1a.
Climate change in centuries in observational and model data Evgeny Volodin, Institute of Numerical Mathematics RAS, Moscow, Russia.
Low clouds in the atmosphere: Never a dull moment Stephan de Roode (GRS) stratocumulus cumulus.
Solar constant The solar constant is the amount of incoming solar radiation per unit area, measured on the outer surface of Earth's atmosphere, in a plane.
Incoming Solar (Shortwave) at TOA DecemberMarch JuneSeptember.
John J. Cassano - University of Colorado Wieslaw Maslowski -Naval Postgraduate School William Gutowski - Iowa State University Dennis Lettenmaier – University.
1. weather or climate ? Annual mean temperature (red is warm, blue cold)
Radiative Properties of Clouds ENVI3410 : Lecture 9 Ken Carslaw Lecture 3 of a series of 5 on clouds and climate Properties and distribution of clouds.
Why Laminar Flow in Narrow Channels (Heat Transfer Analysis)
Heat Energy Solar and gravitational energy are the fundamental sources of energy for the Earth's climate system. Air-sea exchanges of heat (& freshwater)
Simulate Urban-induced Climate Change Via EOS Observations and Land Surface Model Dr. Menglin Jin, Meteorology Dept, U University of Maryland, College.
© Crown copyright Met Office Electromagnetic and light scattering by atmospheric particulates: How well does theory compare against observation? Anthony.
Matt Robinson Thomas Tolman.  Describes Convective Heat Transfer  Needed for all external and internal flow situations.
Earth-Atmosphere Energy Balance Earth's surface absorbs the 51 units of shortwave and 96 more of longwave energy units from atmospheric gases and clouds.
Pat Arnott, ATMS 749 Atmospheric Radiation Transfer Chapter 6: Blackbody Radiation: Thermal Emission "Blackbody radiation" or "cavity radiation" refers.
1 TEC-MTT/2012/3788/In/SL LMD1D v1 and v2 Comparison with Phoenix Flight Data Prepared by Stéphane Lapensée ESA-ESTEC, TEC-MTT Keplerlaan 1, 2201 AZ Noordwijk.
Radiative transfers in complex geometry for CFD modelling the urban canopy Maya Milliez.
Mesoscale Modeling Review the tutorial at: –In class.
Ozone Creation. Chapter 4 Atmosphere and Surface Energy Balances Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles.
Chapter 4 Atmosphere and Surface Energy Balances Robert W. Christopherson Charlie Thomsen.
Filling Mars Human Exploration Strategic Knowledge Gaps with Next Generation Meteorological Instrumentation. S. Rafkin, Southwest Research Institute
Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-
Global Warming: the Basics CSCI 1210 Fall Dimensions of the Problem Climate science Biological science Technology design Technology policy Global.
ASRAE Student Branch meeting Speaker: Kenneth Simpson USGBC – LEED rating system Today at 5 pm ECJ
Météo-France / CNRM – T. Bergot 1) Introduction 2) The methodology of the inter-comparison 3) Phase 1 : cases study Inter-comparison of numerical models.
Chapter 3 Atmospheric Energy and Global Temperatures.
Improving the Mars Thermal 1D Model E. Millour, A Colaitis, F. Forget EXM-AMSA PM6, 7th July 2011.
Radiation balance Any object in the Universe which has a temperature above the temperature "absolute zero" ( degrees Fahrenheit or degrees.
1 Radiative impact of mineral dust on surface energy balance and PAR, implication for land-vegetation- atmosphere interactions Xin Xi Advisor: Irina N.
MCD upgrades and developments Progress Report 24 April2012 Ehouarn Millour, Luca Montabone, François Forget, Arnaud Colaitis, Aymeric Spiga.
What is temperature? Measure of the average random kinetic energy of the molecules of a substance Physical property that determines the direction of heat.
Large Eddy Simulation of Low Cloud Feedback to a 2-K SST Increase Anning Cheng 1, and Kuan-Man Xu 2 1. AS&M, Inc., 2. NASA Langley Research Center, Hampton,
Biometeorology Lecture 2: Surface Energy Balance Professor Noah Molotch September 5, 2012.
Use of Mesoscale and Microscale Results to Improve the Mars Climate Database Near-Surface Variability Model E. Millour, F. Forget, A. Spiga April 6, 2011.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss WG 3: Overview status report COSMO General Meeting, 19.
New Tools and Methods to fully Characterize the Atmospheric Environment for a Martian EDL. Application to the 2016 Exomars Descent Module. François Forget,
Cloud optical properties: modeling and sensitivity study Ping Yang Texas A&M University May 28,2003 Madison, Wisconsin.
Chapter 3 Atmospheric Energy and Global Temperatures
Inverse Estimation of Concrete Properties Andrew Salisbury Civil Engineering November 27, 2006.
A Thermal Plume Model for the Boundary Layer Convection: Representation of Cumulus Clouds C. RIO, F. HOURDIN Laboratoire de Météorologie Dynamique, CNRS,
EUCLIPSE Toulouse meeting April 2012 Roel Neggers Process-level evaluation at selected grid-points: Constraining a system of interacting parameterizations.
Determining surface characteristics at candidate MSL landing sites using THEMIS high-resolution orbital thermal inertia data Robin Fergason Philip Christensen.
Image: January 2004 Blue Marble Composite – Reto Stöckli, NASA Earth Observatory Energy, space, and Earth's effective temperature Unit 1 of Earth’s Thermostat.
Initial Results from the Diurnal Land/Atmosphere Coupling Experiment (DICE) Weizhong Zheng, Michael Ek, Ruiyu Sun, Jongil Han, Jiarui Dong and Helin Wei.
Heat Transfer, Albedo, and the Natural Greenhouse Effect.
© Oxford University Press, All rights reserved. 1 Chapter 3 CHAPTER 3 THE GLOBAL ENERGY SYSTEM.
Internal Flow: Heat Transfer Correlations. Fully Developed Flow Laminar Flow in a Circular Tube: The local Nusselt number is a constant throughout the.
1 ASTR 8000 STELLAR ATMOSPHERES AND SPECTROSCOPY Introduction & Syllabus Light and Matter Sample Atmosphere.
The Cycling of Energy Chapter 3-3 Study Guide. What is heat flow?  The transfer of energy from a warmer object to a cooler object.
Surface Energy Balance (1). Review of last lecture The mission of meteorology is to understand and predict weather- and climate-related disasters (e.g.
Joint AMWG/CVWG Workshop March 6-7, 2003 Improvements in Radiation Processes Bill Collins Andrew Conley, David Fillmore, Julia.
O. Yevteev, M. Shatunova, V. Perov, L.Dmitrieva-Arrago, Hydrometeorological Center of Russia, 2010.
WHERE DOES THE INCOMING SHORTWAVE RADIATION GO TO? The Shortwave Radiation Balance.
TAS-I/ESA Progress Meeting – 11 th July 2012 Design of a new global dust storm scenario for GCM simulations L. Montabone, E. Millour, F. Forget.
Non-ionizing Radiation
Using the Mars climate Database for aerobraking ( km)
Boundary-Layer Meteorology and Atmospheric Dispersion
Surface Energy Budget, Part I
Investigating Cloud Inhomogeneity using CRM simulations.
Coupled atmosphere-ocean simulation on hurricane forecast
Global energy balance SPACE
What is INSOLATION? A Science Sisters Production 2017.
Thermal Response II Current News and Weather Surface Energy Balance
ATOC 4720 class30 1. Energy balance in the troposphere
Geography Atmosphere Introduction to the Atmosphere [Date] Today I will: - Be introduced to the layers of the atmosphere and the global heat budget.
Temperature in a free surface flow
High Resolution regional reanalysis from a Mars GCM and MM
Thermodynamics Atmosphere
Atmospheric Energy Current Weather: Hurricane Dorian Energy Essentials
Presentation transcript:

Atmospheric Environment Characterization in Support of the ESA ExoMars Mission Intercomparison LMD – SwRI models T. Bertrand, S. Rafkin, F. Forget, A. Spiga, E. Millour

Project status November – start Phase 1 : LMD built 1D version for SWRI for radiative transfer synchronisation LMD sent reference profiles December First SWRI profiles received Solving reference time issues (bug, LTST vs LMST, UT versus LT) Investigation on surface temperature disagreement Problem of shortwave flow LMD found a bug in SWRI latitude Tuning the right options in both model (philosophy: LMD fit SWRI)

Project status January Comparison of 1D reference profiles with dust opacities at 0.2, 1, 5 LMD tries to match SWRI dust radiative effects and radiative models by tuning: 1.Dust opacity 2.Dust visible single scaterring albedo ("brightness of the dust") 3.Dust thermal infrared opacity vs visible opacity

Radiative transfer setting – 1D configuration Note : the radiative transfer model used by SWRI (NASA Ames) is known to underestimate dust heating rates. They partly compensate that by using "dark" dust radiative properties. 1D Run parameters – 6 cases:  Comparison LMD – SwRI without tunning  Comparison LMD – SwRI with tunning of dust properties

Comparison LMD – SwRI without tunning Surface flux SW

Comparison LMD – SwRI without tunning Surface flux LW

Comparison LMD – SwRI without tunning Surface temperature

Comparison LMD – SwRI without tunning Temperature profiles

Comparison LMD – SwRI without tunning Temperature profiles

Comparison LMD – SwRI without tunning Temperature profiles

Comparison LMD – SwRI without tunning Temperature profiles

Comparison LMD – SwRI without tunning Temperature profiles

Comparison LMD – SwRI without tunning Temperature profiles

Sensibility to dust opacity Temperature profiles

Sensibility to dust opacity Temperature profiles

Sensibility to dust opacity Temperature profiles

Sensibility to dust brightness Temperature profiles

Sensibility to dust brightness Temperature profiles

Sensibility to dust brightness Temperature profiles

Sensibility to ratio dust thermal IR vs VIS opacity Temperature profiles

Fitting C1 case with the three parameters Temperature profiles

BEST FITS – Case A1 Temperature profiles

BEST FITS – Case A1 Surface temperature

BEST FITS – Case B1 Temperature profiles

BEST FITS – Case B1 Surface temperature

BEST FITS – Case C1 Temperature profiles

BEST FITS – Case C1 Surface temperature

/ Many plots available on:

Conclusion 1D comparisons are globally ok Turbulent diffusion scheme in the boundary layer: fundamental model differences that should be kept in the intercomparison ? Green light has been given to SwRI to start running GCM, Mesoscale and LES models.