ARTS - GARLIC - KOPRA
|
|
- Doris Lynch
- 6 years ago
- Views:
Transcription
1 ARTS - GARLIC - KOPRA A Lbl Model Intercomparison Franz Schreier, Sebastián Gimeno García, Mathias Milz, Ajil Kottayil.. DLR Remote Sensing Technology Institute, Oberpfaffenhofen, GERMANY. LTU Lulea University of Technology, Kiruna, SWEDEN ARTS Workshop Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
2 Introduction Motivation Verification and validation: one of the most important steps of code development Quality of radiative transfer models critical for atmospheric remote sensing products Dozen(s) of RT model intercomparisons, incl. Lbl models, e.g. AMILDA: KOPRA vs. GARLIC and some more IRTMW: ARTS vs. GARLIC and some others Kristineberg 9: ARTS vs. KOPRA ARTS GARLIC KOPRA?!?!? Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
3 Outline The codes Lbl Intercomparisons Data and Assumptions Results Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
4 ARTS Atmospheric Radiative Transfer Simulator Originally developed for microwave applications Nadir: AMSU-B, MHS, HIRS,... Limb: Odin, SMILES,... Uplooking: MIAWARA, AMSOS,... Continuum: MT-CKD. S. Bühler, P. Eriksson et al., JQSRT 9, 65 9, 5 P. Eriksson, S. Bühler et al., JQSRT, , Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
5 GARLIC Generic Atmospheric Radiation Lbl Infrared Code Line shapes: Voigt, VanVleck Doppler, Lorentz Line data: HITRAN, HITEMP, GEISA, JPL,... Continua: Geometries: CKD. (H O, CO, N, O ), dry air (Liebe) Limb, uplooking, downlooking (refraction optional) Instruments: Spectral response: FTS, Heterodyne, Fabry Perot,... Field-of-view: Box, Gauss, Trapez,... Implementation: FORTRAN 8, all data read from external files Inversion: Extensions: Jacobians by automatic differentation (multiple) scattering infrared radiative transfer: J. Mendrok: SARTRE approx. spherical geo (GRL 7) M. Vasquez: cloudy exo-planet atmospheres (A&A a,b) F. Schreier et al. JQSRT, 7, 9 5, Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 5
6 KOPRA Karlsruhe Optimized & Precise Radiative transfer Algorithm Originally developed for mid infrared Fourier transform spectroscopy Limb: MIPAS-Envisat, MIPAS-balloon Limb+uplooking: MIPAS-STR, GLORIA Uplooking, solar absorption: FTIR Kiruna non-lte and (single) scattering Continuum: H O: CKD., CO :??, N : Lafferty AO 96, O : Tibault 97 G. Stiller, T. von Clarmann, B. Funke, N. Glatthor, F. Hase, M. Höpfner and A. Linden, JQSRT 7, 9 8, Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 6
7 Outline The codes Lbl Intercomparisons Data and Assumptions Results Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 7
8 AMILDA Advanced MIPAS Level Data Analysis Intercomparison of algorithms and data analysis strategies used by five European groups Series of exercises: from simple cell transmission to more realistic radiance Exercise : Limb with km, apodized FTS line shape, finite field-of-view; H O, CO, O, N O, CH ; HITRAN 98 and CKD-continuum T. von Clarmann et al. JQSRT, 78, 8 7, I [ nw/(cm sr cm ) ] Radiance I [ nw/(cm sr cm ) ] BexpOD trapez-path trapez-laguerre,5.5,6,6.5 KOPRA GARLIC,5,5.5,6,6.5,7 Wavenumber ν [cm ] Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 8
9 IRTMW Intercomparison of 8 µw codes Series of 5 cases, starting with line shape and absorption Full RT incl. FoV and SRF all geometries Case Uplooking RAM-like Temperature TB [K] TB [K] TB [K].5... ARTS dg ARTS 6dg GARLIC dg GARLIC 6dg avint BexpOD Hermite trapez-path trapez-laguerre Wavenumber ν [cm ] avint BexpOD Hermite trapez-path trapez-laguerre Case Downlooking AMSU-like Equivalent Temperature T B [K] T B [K] T B [K] ARTS 8dg 69 ARTS dg GARLIC TL 8dg GARLIC TLdg avint B exp OD Hermite path trapez trapez Laguerre Wavenumber [cm ] C. Melsheimer et al. Radio Science,, RS7, 5 Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 9
10 Kristineberg 9 M. Milz: ARTS IR Application Radiances for one channel Motivation: Nadir sounding with similar geometry as AMSU-B / MHS since early 8 s Conclusion: Good agreement ARTS KOPRA (and LblRTM) Outlook: Update continuum HIRS Channel #7 for all Profiles HIRS Channel #9 for all Profiles HIRS Channel # for all Profiles 8 6 HIRS Channel #8 for all Profiles HIRS Channel # for all Profiles HIRS Channel # for all Profiles Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
11 Outline The codes Lbl Intercomparisons Data and Assumptions Results Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
12 GARAND atmospheres Garand Atmospheres 6 5 Altitude [km] 5 Temperature [K] HO [ppm] 6 8 O [ppm] L. Garand et al. Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
13 HIRS High Resolution Infrared Sounder 9 infrared channel scanning radiometer used for operational atmospheric sounding by NASA/NOAA and EUMETSAT. CO absorption bands for temperature sounding. Also measures water vapour, ozone, N O and cloud and surface temperatures. Radiance [µw / (cm sr cm )] 5 Transmission Response Transmission HO O CO CH CO NOAA7! wavenumber [cm ] Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
14 Further Assumptions HITRAN, main molecules only Continuum: CKD or MT-CKD Voigt line shape (no prefactor) Geometry: nadir (downlooking 8 ), no FoV Surface temperature T surf = T atm ( km) Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
15 Outline The codes Lbl Intercomparisons Data and Assumptions Results Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 5
16 Brightness Temperatures 8 tropical 8 mls 8 mlw arts garlic kopra T B [K] us sas saw T B [K] Remote Sensing Technology Institute Channel # ARTS - GARLIC - KOPRA 6 Fri May :8:
17 Perfect! Thanks for your attention Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 7
18 Perfect! wait a moment whats about the other atmospheres?... and differences etc.??? Remember: IASI etc. have sub-kelvin sensitivity! Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 7
19 First results IRS T [K] Ch # 67 Ch # 5 76 Ch # 8 Ch # Ch # 68 Ch # 6 7 Ch # 66 Ch #6 Ch # 69 Ch # 7 79 Ch # 59 Ch # n Ch # 7 Ch # 8 9 Ch # 87 Ch #8 5 a g g k k a Ch # 9 Ch # Ch #9 66 Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 8 Fri Feb 6:58:
20 : N + O lines & continuum added in GARLIC T [K] Ch # 67 Ch # 5 76 Ch # 8 Ch #5 5 Ch # 68 Ch # 6 7 Ch # 66 Ch #6 Ch # 69 Ch # 7 79 Ch # 59 Ch #7 9 n Ch # 7 Ch # 8 9 Ch # 87 Ch #8 5 a g g k k a Ch # 9 Ch # Ch #9 66 Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 9 Fri Feb 6:7:8
21 Channel : ARTS GARLIC Channel Channel Similar absorption: CO > H O > O > N O Mostly stratospheric emission Continuum & H O irrelevant Q-branch, convolution,...?? Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
22 Channel : ARTS GARLIC Channel Channel Similar absorption: CO > H O > O > N O Mostly stratospheric emission Continuum & H O irrelevant Q-branch, convolution,...?? NOAA5-HIRS for KOPRA!!! Response.. HIRS Normalized Response Functions noaa5/ch noaa5/ch noaa5/ch noaa5/ch noaa5/ch5 noaa5/ch6 noaa7/ch noaa7/ch noaa7/ch noaa7/ch noaa7/ch5 noaa7/ch Wavenumber [cm ] Fri Jun 6 :: Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
23 Channel 5, 6, and 7: GARLIC KOPRA CO H O > O > N O Mostly free troposphere emission (Weighting functions peak at 8 and km for 78 and 75 cm ) Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
24 Channel 8 and 9: ARTS KOPRA Weak absorption transparent down to troposphere Continua and/or H O?? Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
25 Without continuum? ARTS vs. GARLIC ARTS GARLIC: no Continuum Differences mostly <.5 K What is special with atm # Channels: 8, 9,, 7, 8, 9 (9,, 8, 9, 5, 66 cm ) What is special with channel 59 cm? ARTS GARLIC: with Continuum.5 T [K] T [K] Atmosphere # Atmosphere # Thu Jun 5 7:5:9 Thu Jun 5 7::9 Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
26 Without continuum? GARLIC vs. KOPRA Garand Atmospheres Good agreement (.9 K) in channel KOPRA failed for atm #,, 5, 5 z[km] GARLIC KOPRA: no Continuum 6 8 T[K] Thu Jun 5 :: 5 Garand Atmospheres T [K] 5 5 z [km] 6 Atmosphere # Thu Jun 5 7::9 e 6 e 5 e e e HO [ppv] Thu Jun 5 :58:6 Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
27 What s common and what s different? ARTS GARLIC KOPRA S(T ) conversion semi-tips Atmos TIPS Weak lines? all rejection? Line wings 5 cm??? cm, H O: 5 cm Continuum MT-CKD. CKD. CKD.,... Inhomogeneous Path? quadrature B linear τ layers?? Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 5
28 Conclusions and Outlook max T ka =. K in channel 5 cm (channel ignored) No code is the best for all channels and/or atmospheres max Tag = +. K in 66 cm max Tgk = +.5 K in channel 5 cm Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 6
29 Conclusions and Outlook max T ka =. K in channel 5 cm (channel ignored) No code is the best for all channels and/or atmospheres max Tag = +. K in 66 cm max Tgk = +.5 K in channel 5 cm Use another code (e.g. LblRTM) as reference? NO! Include more codes? hmmmm? Use common absorption coefficients Plot differences vs. (min, max, delta,... ) temperature, H O,... Compare monochromatic spectra and/or transmission Open questions Continuum Lines strength T conversion Line wing cut-off (CO at cm ) Weak line suppression Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 6
30 Outline 5 Appendix More T Difference Plots Weighting and Response Functions Continua Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 7
31 Max. Temperature Delta in Layer T [K] Ch # 67 Ch # 5 76 Ch # 8 Ch # Ch # 68 Ch # 6 7 Ch # 66 Ch # Ch # 69 Ch # 7 79 Ch # 59 Ch # T max [K] Ch # 7 Ch # 8 9 Ch # 87.5 Ch # a g g k k a Ch # 9 Ch # Ch # Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 8 Tue Feb 6 7::56
32 T [K] Brightness Temperature Difference vs Minimum Temperature Ch # 67. Ch # 5 76 Ch # 8 Ch # Ch # 68 Ch # 6 7 Ch # 66 Ch # Ch # 69 Ch # 7 79 Ch # 59 Ch #7 9.5 Ch # 87 Ch # Ch #8 5 Ch # T min [K].5.5 Ch # 7 Ch # a g g k k a Ch # 9 Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 9 Mon Feb 5 :5:
33 T [K] Brightness Temperature Differences vs. Surface Temperature Ch # 67 Ch # 5 76 Ch # 8 Ch # Ch # 68 Ch # 6 7 Ch # 66 Ch # Ch # 69 Ch # 7 79 Ch # 59 Ch # T surf [K].5.5 Ch # 7 Ch # Ch # 87 Ch #8 5.5 a g g k k a Ch # 9 Ch # Ch #9 66 Remote Sensing Technology Institute ARTS - GARLIC - KOPRA Mon Feb 5 5:8:
34 Brightness Temperature Differences vs Temperature Range T [K] Ch # 67 Ch # 5 76 Ch # 8 Ch # Ch # 68 Ch # 6 7 Ch # 66 Ch # Ch # 69 Ch # 7 79 Ch # 59 Ch # T max T min [K].5.5 Ch # 7 Ch # Ch # 87 Ch #8 5.5 a g g k k a Ch # 9 Ch # Ch #9 66 Remote Sensing Technology Institute ARTS - GARLIC - KOPRA Mon Feb 5 5:5:
35 T [K] Ch # 67. Ch # 5 76 Ch # 8 Ch #5 5 6 Brightness Temperature Difference vs Water Column... Ch # 68 Ch # 6 7 Ch # 66 Ch # Ch # 69 Ch # 7 79 Ch # 59 Ch #7 9 6 H O [kg/m ] Ch # 87 Ch # Ch #8 5 Ch #9 66 Ch # 7 Ch # a g g k k a Ch # 9 6 Remote Sensing Technology Institute ARTS - GARLIC - KOPRA Mon Feb 5 ::6
36 Weighting Functions s I(ν, s) = B(ν, T ) T (ν, s ) s ds Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
37 Response Functions HIRS Normalized Response Functions HIRS Normalized Response Functions.6 noaa5/ch7 noaa5/ch8 noaa5/ch9 noaa5/ch noaa7/ch7 noaa7/ch8 noaa7/ch9 noaa7/ch. noaa5/ch noaa5/ch noaa7/ch noaa7/ch Response. Response Wavenumber [cm ] HIRS Normalized Response Functions Fri Jun 6 :5:5 5 6 Wavenumbers [cm ] HIRS Normalized Response Functions Fri Jun 6 :7:. noaa5/ch noaa5/ch noaa5/ch5 noaa5/ch6 noaa7/ch noaa7/ch noaa7/ch5 noaa7/ch6.. noaa5/ch7 noaa5/ch8 noaa5/ch9 noaa7/ch7 noaa7/ch8 noaa7/ch9. Response. Response... 5 Wavenumber [cm ] Fri Jun 6 :: Wavenumber [cm ] Fri Jun 6 ::9 Remote Sensing Technology Institute ARTS - GARLIC - KOPRA
38 CO Continua Remote Sensing Technology Institute ARTS - GARLIC - KOPRA 5
WP1100 Radiative Transfer
HGF PEL Atmosphere Workshop II WP1100 Radiative Transfer Past and Future Franz Schreier, Mayte Vásquez, Thomas Trautmann Sebastián Gimeno García, Pascal Hedelt. DLR Remote Sensing Technology Institute
More informationInfrared radiance modelling and assimilation
Infrared radiance modelling and assimilation Marco Matricardi ECMWF Workshop on the Radiation in the Next Generation of Weather Forecast Models 21-24 May 2018 ECMWF - Reading - UK Radiative transfer models
More informationObservations 3: Data Assimilation of Water Vapour Observations at NWP Centres
Observations 3: Data Assimilation of Water Vapour Observations at NWP Centres OUTLINE: Data Assimilation A simple analogy: data fitting 4D-Var The observation operator : RT modelling Review of Radiative
More informationRetrieval of upper tropospheric humidity from AMSU data. Viju Oommen John, Stefan Buehler, and Mashrab Kuvatov
Retrieval of upper tropospheric humidity from AMSU data Viju Oommen John, Stefan Buehler, and Mashrab Kuvatov Institute of Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 2839 Bremen, Germany.
More informationIntercomparison of Three Microwave/Infrared High Resolution Line-by-Line Radiative Transfer Codes
Intercomparison of Three Microwave/Infrared High Resolution Line-by-Line Radiative Transfer Codes Franz Schreier a,, Mathias Milz b, Stefan A. Buehler c, Thomas von Clarmann d a DLR German Aerospace Center,
More informationLong-term validation of MIPAS ESA operational products using MIPAS-B measurements: L1v7/L2v8 T, H 2 O, and O 3
Long-term validation of MIPAS ESA operational products using MIPAS-B measurements: Lv/L2v T, O, and Gerald Wetzel, Michael Höpfner, and Hermann Oelhaf CCN #: Report to Lv/L2v DDS validation T+ O (instead
More informationInfrared remote sensing of atmospheres of Earth-like planets
Infrared remote sensing of atmospheres of Earth-like planets Feasibility of Atmospheric Retrievals Betreuer: Franz Schreier Abteilung: Atmosphärenprozessoren Deutsches Zentrum für Luft und Raumfahrt, Oberpfaffenhofen-Weßling,
More informationMEASUREMENTS AND MODELLING OF WATER VAPOUR SPECTROSCOPY IN TROPICAL AND SUB-ARCTIC ATMOSPHERES.
MEASUREMENTS AND MODELLING OF WATER VAPOUR SPECTROSCOPY IN TROPICAL AND SUB-ARCTIC ATMOSPHERES. J.P. Taylor, T.J. Hewison, A. McGrath and A. Vance. Airborne Remote Sensing Group, The Met Office, Y70 Building,
More informationASSESSMENT OF THE GEISA AND GEISA/IASI SPECTROSCOPIC DATA QUALITY: trough comparisons with other public database archives
ASSESSMENT OF THE GEISA AND GEISA/IASI SPECTROSCOPIC DATA QUALITY: trough comparisons with other public database archives N. Jacquinet-Husson, N.A. Scott, A. Chédin, R. Armante Laboratoire de Météorologie
More informationMillimetre-wave Limb Sounding
Millimetre-wave Limb Sounding Lecture by B.Kerridge, RAL ESA Advanced AtmosphericTraining Course 15-20 th Sept 2008, Oxford Contents 1. Principles of mm-wave sounding Radiative transfer & spectroscopy
More informationCOMBINED OZONE RETRIEVAL USING THE MICHELSON INTERFEROMETER FOR PASSIVE ATMOSPHERIC SOUNDING (MIPAS) AND THE TROPOSPHERIC EMISSION SPECTROMETER (TES)
COMBINED OZONE RETRIEVAL USING THE MICHELSON INTERFEROMETER FOR PASSIVE ATMOSPHERIC SOUNDING (MIPAS) AND THE TROPOSPHERIC EMISSION SPECTROMETER (TES) Claire Waymark, Anu Dudhia, John Barnett, Fred Taylor,
More informationSpectroscopic database GEISA-08 : content description and assessment through IASI/MetOp flight data
Spectroscopic database GEISA-08 : content description and assessment through IASI/MetOp flight data Jacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A. Laboratoire de Météorologie
More informationJOINT RETRIEVAL OF CO AND VIBRATIONAL TEMPERATURE FROM MIPAS-ENVISAT
JOINT RETRIEVAL OF CO AND VIBRATIONAL TEMPERATURE FROM MIPAS-ENVISAT Joanne Walker and Anu Dudhia Atmospheric, Oceanic and Planetary Physics, Oxford Universtity, UK ABSTRACT MIPAS is a limb viewing fourier
More informationRTMIPAS: A fast radiative transfer model for the assimilation of infrared limb radiances from MIPAS
RTMIPAS: A fast radiative transfer model for the assimilation of infrared limb radiances from MIPAS Niels Bormann, Sean Healy, and Marco Matricardi European Centre for Medium-range Weather Forecasts (ECMWF),
More informationThe Retrieval of Infrared Cooling Rate Profiles from Thermal Infrared Remote Sounder Radiance Measurements
The Retrieval of Infrared Cooling Rate Profiles from Thermal Infrared Remote Sounder Radiance Measurements Daniel Feldman Candidacy Presentation May 13, 2005 Outline 1. Background 2. Motivation 3. Cooling
More informationВЛИЯНИЕ ТОЧНОСТИ СПЕКТРОСКОПИЧЕСКОЙ ИНФОРМАЦИИ В ЗАДАЧАХ МОНИТОРИНГА МЕТАНА
ВЛИЯНИЕ ТОЧНОСТИ СПЕКТРОСКОПИЧЕСКОЙ ИНФОРМАЦИИ В ЗАДАЧАХ МОНИТОРИНГА МЕТАНА М.Ю.Катаев, А.В.Никитин Институт оптики атмосферы СО РАН INFLUENCE OF THE SPECTROSCOPIC INFORMATION ACCURACY IN TASKS OF THE
More informationN. Jacquinet-Husson, N.A. Scott, A. Chédin, R. Armante, K. Garceran, Th. Langlois.
Assessing Spectroscopic Parameter Archives for the Second Generation Vertical Sounders Radiance Simulation: Illustration through the GEISA/IASI database N. Jacquinet-Husson, N.A. Scott, A. Chédin, R. Armante,
More informationRadiative transfer modeling in the far-infrared with emphasis on the estimation of H2O continuum absorption coefficients
Applied Spectroscopy Radiative transfer modeling in the far-infrared with emphasis on the estimation of H2O continuum absorption coefficients Guido Masiello, Carmine Serio DIFA, University of Basilicata,
More informationJacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A.
Jacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A. Laboratoire de Météorologie Dynamique Atmospheric Radiation Analysis Group Ecole Polytechnique 91128, Palaiseau, France http://ara.lmd.polytechnique.fr
More informationPrinciples of Radiative Transfer Principles of Remote Sensing. Marianne König EUMETSAT
- Principles of Radiative Transfer Principles of Remote Sensing Marianne König EUMETSAT marianne.koenig@eumetsat.int Remote Sensing All measurement processes which perform observations/measurements of
More informationValidation of H2O line and continuum spectroscopic parameters in the far infrared wave number range
Applied Spectroscopy Validation of H2O line and continuum spectroscopic parameters in the far infrared wave number range Guido Masiello, Carmine Serio CNISM, National Interuniversity Consortium for the
More informationComparison of AMSU-B Brightness Temperature with Simulated Brightness Temperature using Global Radiosonde Data
Comparison of AMSU-B Brightness Temperature with Simulated Brightness Temperature using Global Radiosonde Data V.O. John, S.A. Buehler, and M. Kuvatov Institute of Environmental Physics, University of
More informationOutline. December 14, Applications Scattering. Chemical components. Forward model Radiometry Data retrieval. Applications in remote sensing
in in December 4, 27 Outline in 2 : RTE Consider plane parallel Propagation of a signal with intensity (radiance) I ν from the top of the to a receiver on Earth Take a layer of thickness dz Layer will
More informationComposition and structure of the atmosphere. Absorption and emission by atmospheric gases.
Lecture 3. Composition and structure of the atmosphere. Absorption and emission by atmospheric gases. 1. Structure and composition of the Earth s atmosphere. 2. Properties of atmospheric gases. 3. Basic
More informationAircraft and satellite hyperspectral measurements investigating the radiative impact of atmospheric water vapour
Aircraft and satellite hyperspectral measurements investigating the radiative impact of atmospheric water vapour S. M. Newman 1, A. Larar 2, W. L. Smith 3, K. P. Shine 4, I. V. Ptashnik 4, F. I. Hilton
More informationLecture 3. Composition and structure of the atmosphere. Absorption and emission by atmospheric gases.
Lecture 3. Composition and structure of the atmosphere. Absorption and emission by atmospheric gases. 1. Structure and composition of the Earth s atmosphere. 2. Properties of atmospheric gases. 3. Basic
More informationAn Alternate Algorithm to Evaluate the Reflected Downward Flux Term for a Fast Forward Model
An Alternate Algorithm to Evaluate the Reflected Downward Flux Term for a Fast Forward Model Introduction D.S. Turner Meteorological Service of Canada Downsview, Ontario, Canada In order to assimilate
More informationAircraft and satellite hyperspectral measurements investigating the radiative impact of atmospheric water vapour
Aircraft and satellite hyperspectral measurements investigating the radiative impact of atmospheric water vapour Stuart Newman and co-workers ITSC-17, Monterey, 14-20 April 2010 Acknowledgements Many thanks
More informationRadiance Data Assimilation. Andrew Collard Environmental Modeling Center NCEP/NWS/NOAA With input from: John Derber
Radiance Data Assimilation Andrew Collard Environmental Modeling Center NCEP/NWS/NOAA With input from: John Derber Outline Introduction Different types of satellite data. Basic theory of satellite observations
More informationHigh Sensitivity Gas Sensor Based on IR Spectroscopy Technology and Application
PHOTONIC SENSORS / Vol. 6, No. 2, 2016: 127 131 High Sensitivity Gas Sensor Based on IR Spectroscopy Technology and Application Hengyi LI Department of Electronic Information Engineering, Jincheng College
More informationRecent spectroscopy updates to the line-by-line radiative transfer model LBLRTM evaluated using IASI case studies
Recent spectroscopy updates to the line-by-line radiative transfer model LBLRTM evaluated using IASI case studies M.J. Alvarado 1, V.H. Payne 2, E.J. Mlawer 1, J.-L. Moncet 1, M.W. Shephard 3, K.E. Cady-Pereira
More informationImpact of Spectroscopic Parameter Archive on Second Generation Vertical Sounders Radiance Simulation: the GEISA/IASI Database as an example
Impact of Spectroscopic Parameter Archive on Second Generation Vertical Sounders Radiance Simulation: the GEISA/IASI Database as an example N. Jacquinet-Husson, N.A. Scott, A. Chédin, R. Armante et co-authors
More informationComparison of AIRS and AMSU-B monthly mean estimates of upper tropospheric humidity
GEOPHYSICAL RESEARCH LETTERS, VOL.???, XXXX, DOI:10.1029/, Comparison of AIRS and AMSU-B monthly mean estimates of upper tropospheric humidity M. Milz Department of Space Science, Luleå University of Technology,
More informationEmission Limb sounders (MIPAS)
Emission Limb sounders (MIPAS) Bruno Carli ENVISAT ATMOSPHERIC PACKAGE MIPAS Michelson Interferometric Passive Atmospheric Sounder GOMOS Global Ozone Monitoring by Occultation of Stars SCIAMACHY Scanning
More informationMonday, Oct. 2: Clear-sky radiation; solar attenuation, Thermal. nomenclature
Monday, Oct. 2: Clear-sky radiation; solar attenuation, Thermal nomenclature Sun Earth Y-axis: Spectral radiance, aka monochromatic intensity units: watts/(m^2*ster*wavelength) Blackbody curves provide
More informationCOMPARISONS OF MIPAS O 3 PROFILES WITH GROUND-BASED MEASUREMENTS
COMPARISONS OF MIPAS O 3 PROFILES WITH GROUND-BASED MEASUREMENTS T. Blumenstock (1), S. Mikuteit (1), F. Hase (1), I. Boyd (2), Y. Calisesi (3), C. DeClercq (4), J.-C. Lambert (4), R. Koopman (5), S. McDermid
More informationAbsorption Line Physics
Topics: 1. Absorption line shapes 2. Absorption line strength 3. Line-by-line models Absorption Line Physics Week 4: September 17-21 Reading: Liou 1.3, 4.2.3; Thomas 3.3,4.4,4.5 Absorption Line Shapes
More informationA tool for IASI hyperspectral remote sensing applications: The GEISA/IASI database in its latest edition
A tool for IASI hyperspectral remote sensing applications: The GEISA/IASI database in its latest edition N. Jacquinet-Husson, C. Boutammine, R. Armante, L.Crépeau, A. Chédin, N.A. Scott, C. Crevoisier,
More informationRadiation in the Earth's Atmosphere. Part 1: Absorption and Emission by Atmospheric Gases
Radiation in the Earth's Atmosphere Part 1: Absorption and Emission by Atmospheric Gases Electromagnetic Waves Electromagnetic waves are transversal. Electric and magnetic fields are perpendicular. In
More informationAssimilation of Cloud-Affected Infrared Radiances at Environment-Canada
Assimilation of Cloud-Affected Infrared Radiances at Environment-Canada ECMWF-JCSDA Workshop on Assimilating Satellite Observations of Clouds and Precipitation into NWP models ECMWF, Reading (UK) Sylvain
More informationOn the simulation of up-looking and down-looking high-resolution radiance spectra
2QWKHVLPXODWLRQRIXSORRNLQJDQG GRZQORRNLQJKLJKUHVROXWLRQUDGLDQFH VSHFWUDXVLQJWZRGLIIHUHQWUDGLDWLYH WUDQVIHUPRGHOV 5RODQGR5L]]L 0DUFR0DWULFDUGLDQG )HUHQF0LVNROF]L 5HVHDUFK'HSDUWPHQW 'HSWRI3K\VLFV8QLYHUVLWjGHJOL6WXGL%RORJQD,WDO\
More informationCOMPARISON OF SIMULATED RADIANCE FIELDS USING RTTOV AND CRTM AT MICROWAVE FREQUENCIES IN KOPS FRAMEWORK
COMPARISON OF SIMULATED RADIANCE FIELDS USING RTTOV AND CRTM AT MICROWAVE FREQUENCIES IN KOPS FRAMEWORK Ju-Hye Kim 1, Jeon-Ho Kang 1, Hyoung-Wook Chun 1, and Sihye Lee 1 (1) Korea Institute of Atmospheric
More informationBlackbody radiation. Main Laws. Brightness temperature. 1. Concepts of a blackbody and thermodynamical equilibrium.
Lecture 4 lackbody radiation. Main Laws. rightness temperature. Objectives: 1. Concepts of a blackbody, thermodynamical equilibrium, and local thermodynamical equilibrium.. Main laws: lackbody emission:
More informationAtmospheric Measurements from Space
Atmospheric Measurements from Space MPI Mainz Germany Thomas Wagner Satellite Group MPI Mainz Part 1: Basics Break Part 2: Applications Part 1: Basics of satellite remote sensing Why atmospheric satellite
More informationRTTOV 10 Theory & Exercise
RTTOV 10 Theory & Exercise Ø Overview of RTTOVS Radiative Transfer Model q Gases Absorption (water Vapor & other trace gases) q Aerosol/Clouds Scattering and Absorption q Surface Emissivity/Reflectivity
More informationModerate Spectral Resolution Radiative Transfer Modeling Based on Modified Correlated-k Method
Moderate Spectral Resolution Radiative Transfer Modeling Based on Modified Correlated-k Method S. Yang, P. J. Ricchiazzi, and C. Gautier University of California, Santa Barbara Santa Barbara, California
More informationVALIDATION OF MIPAS ON ENVISAT BY CORRELATIVE MEASUREMENTS OF MIPAS-STR
VALIDATION OF MIPAS ON ENVISAT BY CORRELATIVE MEASUREMENTS OF MIPAS-STR G.Y. LIU, C.E. BLOM, T. GULDE, C. KEIM, M. HÖPFNER, P. LOËS, C. PIESCH, C. SARTORIUS Forschungszentrum Karlsruhe / Universität Karlsruhe
More informationCLOUD DETECTION AND DISTRIBUTIONS FROM MIPAS INFRA-RED LIMB OBSERVATIONS
CLOUD DETECTION AND DISTRIBUTIONS FROM MIPAS INFRA-RED LIMB OBSERVATIONS J. Greenhough, J. J. Remedios, and H. Sembhi EOS, Space Research Centre, Department of Physics & Astronomy, University of Leicester,
More informationRetrieval Algorithm Using Super channels
Retrieval Algorithm Using Super channels Xu Liu NASA Langley Research Center, Hampton VA 23662 D. K. Zhou, A. M. Larar (NASA LaRC) W. L. Smith (HU and UW) P. Schluessel (EUMETSAT) Hank Revercomb (UW) Jonathan
More informationRadiative transfer theory (Pure gas atmosphere)
Radiative transfer theory (Pure gas atmosphere Bruno Carli Radiative transfer equation The radiative transfer equation states that the specific intensity of radiation I( (defined as the energy flux per
More informationPerformance of the line-by-line radiative transfer model (LBLRTM) for temperature and species retrievals: IASI case studies from JAIVEx
Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics Performance of the line-by-line radiative transfer model (LBLRTM) for temperature
More informationSatellite Radiance Data Assimilation at the Met Office
Satellite Radiance Data Assimilation at the Met Office Ed Pavelin, Stephen English, Brett Candy, Fiona Hilton Outline Summary of satellite data used in the Met Office NWP system Processing and quality
More informationGEISA 2013 Ozone and related atmospheric species contents description and assessment
GEISA 2013 Ozone and related atmospheric species contents description and assessment N. Jacquinet-Husson C. Boutammine, R. Armante, L.Crépeau, A. Chédin, N.A. Scott, C. Crevoisier, V.Capelle, A. Bouhdaoui
More informationRepresentative wavelengths absorption parameterization applied to satellite channels and spectral bands
This is an almost final version of the paper J. Gasteiger, C. Emde, B. Mayer, R. Buras, S.A. Buehler, and O. Lemke. Representative wavelengths absorption parameterization applied to satellite channels
More informationVALIDATION OF MIPAS CH 4 PROFILES BY STRATOSPHERIC BALLOON, AIRCRAFT, SATELLITE AND GROUND BASED MEASUREMENTS
VALIDATION OF MIPAS CH 4 PROFILES BY STRATOSPHERIC BALLOON, AIRCRAFT, SATELLITE AND GROUND BASED MEASUREMENTS C. Camy-Peyret (1), S. Payan (1), G. Dufour (1), H. Oelhaf (2), G. Wetzel (2), G. Stiller (2),
More informationAn assessment of the accuracy of the RTTOV fast radiative transfer model using IASI data
An assessment of the accuracy of the RTTOV fast radiative transfer model using IASI data Marco Matricardi, Tony McNally ECMWF Reading, Berkshire, UK Abstract IASI measurements of spectral radiances made
More informationJacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A.
Jacquinet-Husson N., Capelle V., Crépeau L., Scott N.A., Armante R., Chédin A. Laboratoire de Météorologie Dynamique Atmospheric Radiation Analysis Group Ecole Polytechnique 91128, Palaiseau, France http://ara.lmd.polytechnique.fr
More informationSatellite data assimilation for Numerical Weather Prediction II
Satellite data assimilation for Numerical Weather Prediction II Niels Bormann European Centre for Medium-range Weather Forecasts (ECMWF) (with contributions from Tony McNally, Jean-Noël Thépaut, Slide
More informationLine shape modeling and application to remote sensing
Line shape modeling and application to remote sensing Dr. Ha Tran Senior Researcher at CNRS, Paris, France Laboratoire de Météorologie Dynamique Sorbonne Université, Ecole Polytechnique, Ecole Normale
More informationOutcomes of a workshop aimed at improved understanding of biases found in analysis of 183 GHz observations
Outcomes of a workshop aimed at improved understanding of biases found in analysis of 183 GHz observations She did all the hard work! Many thanks to all the participants from: LATMOS, Institute Pierre
More informationValidation of IASI level 1 and level 2 products using IASI-balloon
Validation of IASI level 1 and level 2 products using IASI-balloon C. Camy-Peyret, S. Payan, Y. Té, P. Jeseck, J. Bureau and I. Pépin / LPMAA D. Blumstein / CNES B. Tournier, D. Coppens, / Noveltis Outline
More informationTHE Tropospheric Emission Spectrometer (TES), launched. Forward Model and Jacobians for Tropospheric Emission Spectrometer Retrievals
1308 IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, VOL. 44, NO. 5, MAY 2006 Forward Model and Jacobians for Tropospheric Emission Spectrometer Retrievals Shepard A. Clough, Mark W. Shephard, John
More informationDescription of radiation field
Description of radiation field Qualitatively, we know that characterization should involve energy/time frequency all functions of x,t. direction We also now that radiation is not altered by passing through
More informationAssimilation of MIPAS limb radiances at ECMWF using 1d and 2d radiative transfer models
Assimilation of MIPAS limb radiances at ECMWF using 1d and 2d radiative transfer models Niels Bormann, Sean Healy, Mats Hamrud, and Jean-Noël Thépaut European Centre for Medium-range Weather Forecasts
More informationSome challenges in assimilation. of stratosphere/tropopause satellite data
Some challenges in assimilation of stratosphere/tropopause satellite data Authors: W.A. Lahoz and A. Geer Data Assimilation Research Centre, University of Reading RG6 6BB, UK Thanks to: ASSET partners,
More informationRadiative Transfer and Surface Properties Working Group Report
Radiative Transfer and Surface Properties Working Group Report October 29, 2015 ITSC-20 October 28 November 3, 2015 Lake Geneva, Wisconsin USA Topics Covered Scattering RT intercomparison Line-by-line
More informationGLORIA- an airborne imaging FTS
Mahesh Kumar Sha for the GLORIA team, IMK-ASF, KIT, Karlsruhe, Germany KIT University of the State of Baden-Wuerttemberg and National Research Center of the Helmholtz Association www.kit.edu GLORIA Team
More informationLambertian surface scattering at AMSU-B frequencies:
Lambertian surface scattering at AMSU-B frequencies: An analysis of airborne microwave data measured over snowcovered surfaces Chawn Harlow, 2nd Workshop on Remote Sensing and Modeling of Land Surface
More informationPreface to the Second Edition. Preface to the First Edition
Contents Preface to the Second Edition Preface to the First Edition iii v 1 Introduction 1 1.1 Relevance for Climate and Weather........... 1 1.1.1 Solar Radiation.................. 2 1.1.2 Thermal Infrared
More informationEUMETSAT Polar System (EPS)
EUMETSAT Polar System (EPS) Synergetic Operational Earth Observations with the EPS/MetOp System Dieter Klaes EPS Programme Scientist Outline 1. Introduction 2. EPS System and Observations 3. Outlook 1.
More informationCathryn Fox, Juliet Pickering Jon Murray, Alan Last.
Cathryn Fox, Juliet Pickering Jon Murray, Alan Last c.fox11@imperial.ac.uk Campaign overview Cirrus Coupled Cloud-Radiation Experiment Aims: to understand the link between cirrus microphysical properties
More informationRadiative Transfer in the Atmosphere
Radiative Transfer in the Atmosphere Lectures in Brienza 19 Sep 2011 Paul Menzel UW/CIMSS/AOS Outline Radiation Definitions Planck Function Emission, Absorption, Scattering Radiative Transfer Equation
More informationAircraft Validation of Infrared Emissivity derived from Advanced InfraRed Sounder Satellite Observations
Aircraft Validation of Infrared Emissivity derived from Advanced InfraRed Sounder Satellite Observations Robert Knuteson, Fred Best, Steve Dutcher, Ray Garcia, Chris Moeller, Szu Chia Moeller, Henry Revercomb,
More informationWater Pressure Broadening: A Never-ending Story
Water Pressure Broadening: A Never-ending Story Georg Wagner, Manfred Birk DLR Remote Sensing Technology Institute, Oberpfaffenhofen, Germany Remote Sensing Technology Institute 1 Requirements Database
More informationArctic Clouds and Radiation Part 2
Arctic Clouds and Radiation Part 2 Glen Lesins Department of Physics and Atmospheric Science Dalhousie University Create Summer School, Alliston, July 2013 No sun Arctic Winter Energy Balance 160 W m -2
More informationA New Microwave Snow Emissivity Model
A New Microwave Snow Emissivity Model Fuzhong Weng 1,2 1. Joint Center for Satellite Data Assimilation 2. NOAA/NESDIS/Office of Research and Applications Banghua Yan DSTI. Inc The 13 th International TOVS
More informationESA Ozone Climate Change Initiative: combined use of satellite ozone profile measurements
ESA Ozone Climate Change Initiative: combined use of satellite ozone profile measurements V.F. Sofieva, E. Kyrölä, J. Tamminen, S. Tukiainen, J. Hakkarainen Finnish Meteorological Institute, Finland G.
More informationAll-sky assimilation of MHS and HIRS sounder radiances
All-sky assimilation of MHS and HIRS sounder radiances Alan Geer 1, Fabrizio Baordo 2, Niels Bormann 1, Stephen English 1 1 ECMWF 2 Now at Bureau of Meteorology, Australia All-sky assimilation at ECMWF
More informationRetrieval of tropospheric water vapour by using spectra from a microwave spectro-radiometer at 22 GHz
Retrieval of tropospheric water vapour by using spectra from a microwave spectro-radiometer at 22 GHz René Bleisch, Niklaus Kämpfer, Dominik Scheiben Institute of Applied Physics, University of Bern ISTP,
More informationEPS-SG Candidate Observation Missions
EPS-SG Candidate Observation Missions 3 rd Post-EPS User Consultation Workshop Peter Schlüssel Slide: 1 EPS-SG benefits to activities of NMSs Main Payload High-Resolution Infrared Sounding Microwave Sounding
More informationPhysical Basics of Remote-Sensing with Satellites
- Physical Basics of Remote-Sensing with Satellites Dr. K. Dieter Klaes EUMETSAT Meteorological Division Am Kavalleriesand 31 D-64295 Darmstadt dieter.klaes@eumetsat.int Slide: 1 EUM/MET/VWG/09/0162 MET/DK
More informationRemote Sensing: Introduction
Curso Intensivo sobre Asimilación de Datos 27 de Octubre - 7 de Noviembre de 2008 Aula Magna, Pabellon I, Ciudad Universitaria Buenos Aires, Argentina Remote Sensing: Introduction Inés Velasco Departamento
More informationFORMAT-EO SCHOOL GREENHOUSE GAS REMOTE SENSING PROFESSOR JOHN REMEDIOS DR. HARTMUT BOESCH
FORMAT-EO SCHOOL GREENHOUSE GAS REMOTE SENSING PROFESSOR JOHN REMEDIOS DR. HARTMUT BOESCH EOS-SRC, Dept. of Physics and Astronomy, University of Leicester What is covered in this lecture? Climate, radiation
More informationANNALS OF GEOPHYSICS, 56, Fast Track-1, 2013; /ag-6326
ANNALS OF GEOPHYSICS, 56, Fast Track-1, 2013; 10.4401/ag-6326 Validation of the IASI operational CH 4 and N 2 O products using ground-based Fourier Transform Spectrometer: preliminary results at the Izaña
More informationSpaceborne Hyperspectral Infrared Observations of the Cloudy Boundary Layer
Spaceborne Hyperspectral Infrared Observations of the Cloudy Boundary Layer Eric J. Fetzer With contributions by Alex Guillaume, Tom Pagano, John Worden and Qing Yue Jet Propulsion Laboratory, JPL KISS
More informationFuture Opportunities of Using Microwave Data from Small Satellites for Monitoring and Predicting Severe Storms
Future Opportunities of Using Microwave Data from Small Satellites for Monitoring and Predicting Severe Storms Fuzhong Weng Environmental Model and Data Optima Inc., Laurel, MD 21 st International TOV
More informationInstrumentation planned for MetOp-SG
Instrumentation planned for MetOp-SG Bill Bell Satellite Radiance Assimilation Group Met Office Crown copyright Met Office Outline Background - the MetOp-SG programme The MetOp-SG instruments Summary Acknowledgements:
More informationTopics: Visible & Infrared Measurement Principal Radiation and the Planck Function Infrared Radiative Transfer Equation
Review of Remote Sensing Fundamentals Allen Huang Cooperative Institute for Meteorological Satellite Studies Space Science & Engineering Center University of Wisconsin-Madison, USA Topics: Visible & Infrared
More informationVALIDATION OF SCIAMACHY OZONE COLUMN DENSITIES AND PROFILES USING GROUND-BASED FTIR AND MILLIMETER WAVE MEASUREMENTS
VALIDATION OF SCIAMACHY OZONE COLUMN DENSITIES AND PROFILES USING GROUND-BASED FTIR AND MILLIMETER WAVE MEASUREMENTS G. Kopp (1), Th. Blumenstock (1), E. Brinksma (2), H. Eskes (2), A. Griesfeller (1),
More informationThe potential impact of ozone sensitive data from MTG-IRS
The potential impact of ozone sensitive data from MTG-IRS R. Dragani, C. Lupu, C. Peubey, and T. McNally ECMWF rossana.dragani@ecmwf.int ECMWF May 24, 2017 The MTG IRS Long-Wave InfraRed band O 3 Can the
More informationRTTOV-10 SCIENCE AND VALIDATION REPORT
Date : 23/1/2012 RTTOV-10 SCIENCE AND VALIDATION REPORT Roger Saunders 1, James Hocking 1, Peter Rayer 1, Marco Matricardi 2, Alan Geer 2, Niels Bormann 2, Pascal Brunel 3, Fatima Karbou 3 and Filipe Aires
More informationENVISAT VALIDATION RESULTS OBTAINED WITH LPMA AND IASI-BALLOON FTIR
ENVISAT VALIDATION RESULTS OBTAINED WITH LPMA AND IASI-BALLOON FTIR G. Dufour (1), S. Payan (1), Y. Té (1), P. Jeseck (1), V. Ferreira (1), C. Camy-Peyret (1), M. Eremenko (1, *), A. Butz (2), K. Pfeilsticker
More informationIRFS-2 instrument onboard Meteor-M N2 satellite: measurements analysis
IRFS-2 instrument onboard Meteor-M N2 satellite: measurements analysis Polyakov A.V., Virolainen Ya.A., Timofeyev Yu.M. SPbSU, Saint-Petersburg, Russia Uspensky A.B., A.N. Rublev, SRC Planeta, Moscow,
More informationATMOS 5140 Lecture 7 Chapter 6
ATMOS 5140 Lecture 7 Chapter 6 Thermal Emission Blackbody Radiation Planck s Function Wien s Displacement Law Stefan-Bolzmann Law Emissivity Greybody Approximation Kirchhoff s Law Brightness Temperature
More informationInfrared quantitative spectroscopy and atmospheric satellite measurements
Infrared quantitative spectroscopy and atmospheric satellite measurements Jean-Marie Flaud Laboratoire Interuniversitaire des Systèmes Atmosphériques CNRS, Universités Paris Est Créteil et Paris Diderot
More informationLecture 19: Operational Remote Sensing in Visible, IR, and Microwave Channels
MET 4994 Remote Sensing: Radar and Satellite Meteorology MET 5994 Remote Sensing in Meteorology Lecture 19: Operational Remote Sensing in Visible, IR, and Microwave Channels Before you use data from any
More informationAPPLICATIONS WITH METEOROLOGICAL SATELLITES. W. Paul Menzel. Office of Research and Applications NOAA/NESDIS University of Wisconsin Madison, WI
APPLICATIONS WITH METEOROLOGICAL SATELLITES by W. Paul Menzel Office of Research and Applications NOAA/NESDIS University of Wisconsin Madison, WI July 2004 Unpublished Work Copyright Pending TABLE OF CONTENTS
More informationLecture 4: Meteorological Satellites and Instruments. Acknowledgement: Dr. S. Kidder at Colorado State Univ.
Lecture 4: Meteorological Satellites and Instruments Acknowledgement: Dr. S. Kidder at Colorado State Univ. Homework for the Spring Break: get some tangible, preliminary results for your final project.
More informationMEASURING TRACE GAS PROFILES FROM SPACE
MEASURING TRACE GAS PROFILES FROM SPACE Caroline Nowlan Atomic and Molecular Physics Division Harvard-Smithsonian Center for Astrophysics Collaborators: Kelly Chance, Xiong Liu, Gonzalo Gonzalez Abad,
More informationLunar Eclipse of June, 15, 2011: Three-color umbra surface photometry
Lunar Eclipse of June, 15, 2011: Three-color umbra surface photometry Oleg S. Ugolnikov 1, Igor A. Maslov 1,2, Stanislav A. Korotkiy 3 1 Space Research Institute, Russian Academy of Sciences, Russia 2
More information