D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Generation of Simulated GIFTS Datasets Derek J. Posselt, Jim E. Davies,

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Presentation transcript:

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Generation of Simulated GIFTS Datasets Derek J. Posselt, Jim E. Davies, and Erik R. Olson Cooperative Institute for Meteorological Satellite Studies, Space Science and Engineering Center, University of Wisconsin–Madison

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Purpose Prior to GIFTS launch, a GIFTS-specific forward model and retrieval algorithms must be developed Because there is no existing geosynchronous instrument with sufficient spectral resolution, GIFTS data must currently be simulated with sophisticated mesoscale numerical models GIFTS forward radiative transfer model and retrieval methods are evaluated by comparing retrieved temperature, water vapor, and winds with simulated atmospheric state

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Procedure 1.Produce a highly realistic simulated atmospheric state using a mesoscale numerical model (MM5) 2.Write atmospheric state variables to GIFTS forward model binary ingest format 3.Generate high spectral resolution infrared spectra via forward model calculations performed on simulated temperature, moisture, and condensate fields 4.Retrieve temperature, water vapor and winds from top of atmosphere radiances and compare with original simulated atmosphere to assess retrieval accuracy

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Procedure 1.Produce a highly realistic simulated atmospheric state using a mesoscale numerical model (MM5) 2.Diagnose mean particle size of each MM5 microphysical constituent in each grid box for use in cloudy radiative transfer 3.Write atmospheric state variables to GIFTS forward model binary ingest format 4.Generate high spectral resolution infrared spectra via forward model calculations performed on simulated temperature, moisture, and condensate fields 5.Retrieve temperature, water vapor and winds from top of atmosphere radiances and compare with original simulated atmosphere to assess retrieval accuracy

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Cases 1.IHOP 2002 Convective Initiation: 12 June x 3 GIFTS cubes aerial coverage Highly complex wind and moisture fields Predominantly cloud-free domain before initiation of strong late-day convection 2.Pacific THORPEX 2003 Jet Streak: 12 March x 3 GIFTS cubes aerial coverage Jet streak over central Pacific Ocean Strong vertical wind shear, mix of clouds and clear air

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 IHOP 2002 CI Case: Overview and Objectives Objectives: Demonstrate GIFTS potential to observe moisture convergence prior to convective initiation Demonstrate GIFTS usefulness for observation of fine-scale rapidly-evolving water vapor structures Develop GIFTS-based analysis techniques for CI applications Overview: Environment mostly clear preceding convection Very complex low-level moisture structures and wind fields Convection initiated in the presence of strong convergence along a fine-scale low-level water vapor gradient GOES micron imagery: UTC 12 June 2002

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 MM5 Configuration Configuration details: 4 km grid spacing, 60 vertical levels Initialized 0600 UTC, 24-hour duration Goddard microphysics MRF boundary layer No cumulus parameterization RRTM radiation OSU-Land surface model Nudged toward RUC analyses during 6-hour spin-up period Simulated atmospheric fields generated using the 5 th generation Penn State/NCAR Mesoscale Modeling system (MM5) initialized from 10 km RUC analyses

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Simulated GOES-11 imagery for the full simulation domain

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-11 imagerySimulated GOES-11 imagery 1900 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-11 imagerySimulated GOES-11 imagery 2000 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-11 imagerySimulated GOES-11 imagery 2100 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-11 imagerySimulated GOES-11 imagery 2200 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-11 imagerySimulated GOES-11 imagery 2300 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Cloud and water vapor features Color-shaded plot depicts 2- meter mixing ratio White iso-surfaces encompass cloud boundaries Wind vectors valid at 1.5 km height

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 THORPEX 2003 Jet Streak Case: Overview and Objectives Objectives: Demonstrate GIFTS capabilities with respect to winds over the ocean Compare simulated GIFTS water-vapor winds with winds derived from GOES rapid- scan WIND EXperiment Overview: Mix of clear, low, and high cloud Significant jet streak with winds in excess of 180 knots Domain coverage includes Aqua overpass, ER-2 flight, G4 dropsondes Extensive observations were taken as part of THORPEX, GWINDEX, and NOAA NCEP Winter Storms Research Program GOES micron imagery: 2100 UTC 12 March 2003 – 0400 UTC 13 March 2003

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 MM5 Configuration Configuration details: 36/12/4 km grid spacing, 50 vertical levels Initialized 1200 UTC 11 March, 48-hour duration with 33-hour spinup Goddard microphysics MRF boundary layer Grell cumulus on 36 km and 12 km domains, no cumulus parameterization on 4 km domain RRTM/Dudhia radiation No land-surface model Simulated atmospheric fields generated using the 5 th generation Penn State/NCAR Mesoscale Modeling system (MM5) initialized from 1- degree AVN analyses

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-09 imagerySimulated GOES-09 imagery 2100 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-09 imagerySimulated GOES-09 imagery 2200 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-09 imagerySimulated GOES-09 imagery 2300 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-09 imagerySimulated GOES-09 imagery 0000 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-09 imagerySimulated GOES-09 imagery 0100 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-09 imagerySimulated GOES-09 imagery 0200 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulation Results Observed GOES-09 imagerySimulated GOES-09 imagery 0300 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Future Work Finalize Pacific THORPEX simulation and compare with GWINDEX data Investigate transition to WRF as a replacement for MM5 at smaller spatial scales As computing power grows, generate much finer- resolution datasets (grid spacing < 4 km), as well as much larger spatial coverage (4 x 4 and higher)

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Computing cloudy radiances A method for rapidly computing cloudy radiances has been provided (Yang, 2003). gifstfrte has been modified to accommodate this method. Accuracy of the updated model is being assessed through comparisons with LBLRTM/DISORT (Dave Turner, LBLDIS*). Methods and findings are presented here. *modified for more layers and higher spectral resolution

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Data inputs: prior release Surface conditions Profiles –T, q, O3 Ice and liquid water paths

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Additional data inputs Condensate profiles –Deff –Mixing ratio Previously –Deff(liq) = 2 LWP 1/3 –Deff(ice) = 24 IWP 1/3

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Ensemble Deff

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 How are clouds simulated ? A single cloud layer (either ice or liquid) is inserted at a pressure level specified in the input profile. Spectral transmittance and reflectance for ice and liquid clouds interpolated from multi-dimensional LUT. –Wavenumber (500 – /cm) –observation zenith angle (0 – 80 deg) –D eff (ICE: 10 – 157 um, LIQUID: 2 – 100 um) –OD(vis) (ICE: , LIQUID 0.06 – 150)

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 What is “TRUTH” ? The output of LBLDIS ! –gas layer optical depths from LBLRTM v6.01 –layers populated with particulate optical depths, assymetry parameters and single scattering albedos. –DISORT invoked to compute multiple scattered TOA radiances. –Radiances spectrally reduced to GIFTS channels and converted to brightness temperature.

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Split atmosphere to increase “TRUTH” accuracy Need only execute DISORT to cloud top. Separately compute monochromatic radiances and transmittances above cloud top with LBLRTM. Interpolate DISORT output to LBLRTM TOA output resolution and compute “pseudo” monochromatic TOA radiances. Spectrally reduce to GIFTS channels.

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Simulations performed Nadir view, OD = 0, 0.1, 0.5, 1, 2, 3, 10 um Liquid clouds (Mie spheres, gamma dist.) –1, 2, 3 km cloud top altitude –2, 10, 20, 40 um D eff Ice clouds (Hexagonal ice crystals, gamma dist.) –5, 10, 15 km cloud top altitude –10, 20, 40, 100 um D eff LABELS –“FAST” new method of estimating D eff new cloud property database –“TRUTH” LBLRTM/DISORT

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 LW band

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 SMW band

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 LW band difference spectra

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 LW band difference spectra

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 A realistic profile comparison Header line /abyss/Users/jimd/real_cloud_experiment_v6.01/liq/surf_to_cloud 3 /home/jimd/LBLDIS/single_scat_properties/ssp_db.mie_wat.gamma_sigma_0p100 /home/jimd/LBLDIS/single_scat_properties/ssp_db.mie_ice.gamma_sigma_0p100 /home/jimd/LBLDIS/single_scat_properties/ssp_db.hex_ice.gamma.0p

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 LW spectra comparison

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 giftsfrte status and future An improved method for rapidly computing cloudy radiances has been added to the GIFTS top-of-atmosphere radiance model. Comparisons with a more rigorous model show some increased accuracy - but a cloudy profile test set is needed to quantify the improvement. Future considerations to increase model fidelity: –Surface spectral emissivity –Aerosols –Multi-layer / mixed phase clouds

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Modeling Capabilities We have the capability to produce detailed simulations of the variables that will influence GIFTS data. MURI research primarily uses TOA radiances (the first two steps)

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Goals of simulated data for MURI Provide spectra and images for retrievals –Profiles –Clouds –Winds Capture representative examples of realistic TOA radiances.

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 GIFTS Simulated TOA Radiances Using GIFTS forward radiative transfer model to produce top of atmosphere radiances from simulated atmospheric fields Model Atmosphere Forward Model Radiances

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Wavenumber Animation The advantage of GIFTS IHOP 2 by 3, 4 km dataset at ~5 1/cm resolution. June 12 th, 13:00 UTC Single time step = 1.2 GB of TOA radiance data.

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 SMW Wavenumber Animation IHOP 2 by 3, 4 km dataset at ~5 1/cm resolution. June 12 th, 13:00 UTC

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Thorpex Time Animations Final choice of MM5 run? 7 time steps 3 by 3 array of cubes /cm (window region)

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May wavenumber

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 THORPEX SMW sample Same region 7 time steps /cm

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Fast Model Testing Checking simulated data with line by line and DISORT Drawing a bridge between the simulated data and the field experiment data. –Compare THORPEX results to aircraft and GWINDEX data

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Checking broad features of the spectra –Scanning HIS: similar type of interferometer. Participated in both IHOP and THORPEX –Giftsfrte output from a thick ice cloud in the IHOP simulation –S-HIS data is an average of an area of cirrus coverage (significant lidar attenuation and cold window temps)

D. J. Posselt, J. E. Davies, E. R. Olson3 rd MURI Spring Workshop28-29 May 2003 Questions?