Page1 SCIAMACHY Calibration Review – ESTEC – 9 - 13 Sept 2002 SCIAMACHY Tangent Height Verification H.Bovensmann University of Bremen Institute of Remote.

Slides:



Advertisements
Similar presentations
Proposed new uses for the Ceilometer Network
Advertisements

SCIAMACHY LoS Mispointing Modelling M. Gottwald & E. Krieg – DLR-IMF - DLR/IFE IUP-IFE, Bremen, 30 November 2006.
PAGE1 S CHOOL M ANAGEMENT S YSTEM BACK NEXT EXIT Deltasoft STUDENT INFORMATION SYSTEM Student Information System School.
SCIAMACHY Calibration Review, ESTEC, 11 September 2002 Tilstra, De Graaf, Stammes First verification of SCIAMACHY’s polarisation measurements Gijs Tilstra,
Validation of SCIA’s reflectance and polarisation (Acarreta, de Graaf, Tilstra, Stammes, Krijger ) Envisat Validation Workshop, Frascati, 9-13 December.
Products from the OMPS Limb Profiler (LP) instrument on the Suomi NPP Satellite Pawan K. Bhartia Earth Sciences Division- Atmospheres NASA Goddard Space.
PAGE1 S CHOOL M ANAGEMENT S YSTEM BACK NEXT EXIT Deltasoft  STUDENT EXAMINATION SYSTEM Student Examination System School.
GOME-2 polarisation data and products L.G. Tilstra (1,2), I. Aben (1), P. Stammes (2) (1) SRON; (2) KNMI GSAG #42, EUMETSAT,
1 st post launch SCIAMACHY calibration & Verification Meeting L1b Astrium Friedrichshafen – Germany 24 July 2002 First Level 1b Spectral Calibration analysis.
GOME-2 FM3 (Metop-A) Instrument Review, EUMETSAT, Darmstadt, June 2012 Slide: 1 Rűdiger Lang, Rose Munro, Antoine Lacan, Richard Dyer, Marcel Dobber, Christian.
Simultaneous profile measurements of BrO, OClO and NO 2 in the polar vortex Chris Sioris and Kelly Chance Smithsonian Astrophysical Observatory.
SCILOV-10 Validation of SCIAMACHY limb operational NO 2 product F. Azam, K. Weigel, Ralf Bauer, A. Rozanov, M. Weber, H. Bovensmann and J. P. Burrows ESA/ESRIN,
SCILOV-10 Validation of SCIAMACHY limb operational BrO product F. Azam, K. Weigel, A. Rozanov, M. Weber, H. Bovensmann and J. P. Burrows ESA/ESRIN, Frascati,
Envisat Symposium, April 23 – 27, 2007, Montreux bremen.de SADDU Meeting, June 2008, IUP-Bremen Cloud sensitivity studies.
METO 621 CHEM Lesson 7. Albedo 200 – 400 nm Solar Backscatter Ultraviolet (SBUV) The previous slide shows the albedo of the earth viewed from the nadir.
Microwindow Selection for the MIPAS Reduced Resolution Mode INTRODUCTION Microwindows are the small subsets of the complete MIPAS spectrum which are used.
Institut für Umweltphysik/Fernerkundung Physik/Elektrotechnik Fachbereich 1 Retrieval of SCIAMACHY limb measurements: First Results A. Rozanov, V. Rozanov,
CPI International UV/Vis Limb Workshop Bremen, April Development of Generalized Limb Scattering Retrieval Algorithms Jerry Lumpe & Ed Cólon.
Tangent height verification algorithm Chris Sioris, Kelly Chance, and Thomas Kurosu Smithsonian Astrophysical Observatory.
Extracting Atmospheric and Surface Information from AVIRIS Spectra Vijay Natraj, Daniel Feldman, Xun Jiang, Jack Margolis and Yuk Yung California Institute.
A 21 F A 21 F Parameterization of Aerosol and Cirrus Cloud Effects on Reflected Sunlight Spectra Measured From Space: Application of the.
Page 1 ENVISAT SYMPOSIUM - Montreux – 23/27 April 2007 Page 1 Stratospheric Distribution of CO 2 from the MIPAS High-resolution Full Mission Bianca Maria.
ESTEC July 2000 Estimation of Aerosol Properties from CHRIS-PROBA Data Jeff Settle Environmental Systems Science Centre University of Reading.
SADDU meeting, IUP Bremen, June 16/17, 2008 SCIAMACHY limb pointing performance: 2002 – 2008 C. von Savigny 1, M. Gottwald 2, E. Krieg 2, K. Bramstedt.
DOAS Retrievals of Stratospheric O 3 and NO 2 from Odin / OSIRIS Limb-Radiance Measurements Samuel Brohede Craig S. Haley and the Odin team Chalmers University.
Institute for Environmental Physics and Remote Sensing (IUP/ife) Physics/Electrical Engineering 1 K.-U. Eichmann, C. von Savigny, G. Rohen, J. Kaiser,
METO 621 Lesson 27. Albedo 200 – 400 nm Solar Backscatter Ultraviolet (SBUV) The previous slide shows the albedo of the earth viewed from the nadir.
Rachel Klima (on behalf of the MASCS team) JHU/APL MASCS/VIRS Data Users’ Workshop LPSC 2014, The Woodlands, TX March 17,2014 MASCS Instrument & VIRS Calibration.
1 Satellite Remote Sensing of Particulate Matter Air Quality ARSET Applied Remote Sensing Education and Training A project of NASA Applied Sciences Pawan.
Anna Serdyuchenko, Victor Gorshelev, Mark Weber John P. Burrows University of Bremen, Institute for Environmental Physics OSU, Columbus OH, USA1.
Diagnosing Climate Change from Satellite Sounding Measurements – From Filter Radiometers to Spectrometers William L. Smith Sr 1,2., Elisabeth Weisz 1,
Blue: Histogram of normalised deviation from “true” value; Red: Gaussian fit to histogram Presented at ESA Hyperspectral Workshop 2010, March 16-19, Frascati,
Page 1 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Validation of ENVISAT trace gas data products by comparison.
ARCTAS BrO Measurements from the OMI and GOME-2 Satellite Instruments
A. Bracher, L. N. Lamsal, M. Weber, J. P. Burrows University of Bremen, FB 1, Institute of Environmental Physics, P O Box , D Bremen, Germany.
Validation workshop, Frascati, 13 December 2002Page 1 SCIAMACHY products quality and recommendations Based on presentations and discussions during this.
Mark.Weber 1 / GOME2 Error Study: Column Retrieval Overview of Final Presentation (IUP Contribution): Main contribution from IUP.
Page 1ENVISAT Validation Review / GOMOS session - ESRIN – 13th December 2002 ENVISAT VALIDATION WORKSHOP GOMOS Recommendations by the ESL team : Service.
SCIAMACHY long-term validation M. Weber, S. Mieruch, A. Rozanov, C. von Savigny, W. Chehade, R. Bauer, and H. Bovensmann Institut für Umweltphysik, Universität.
IGARSS 2011, July 24-29, Vancouver, Canada 1 A PRINCIPAL COMPONENT-BASED RADIATIVE TRANSFER MODEL AND ITS APPLICATION TO HYPERSPECTRAL REMOTE SENSING Xu.
Institut für Umweltphysik (iup) AMFIC Kick-off Meeting, 26 October 2007, KNMI, The Netherlands Carbon monoxide columns and methane column- averaged mixing.
Harmonizationof GOME, SCIAMACHY, GOME-2 ozone cross-sections Anna Serdyuchenko, John P. Burrows, Mark Weber, Wissam Chehade University of Bremen, Germany.
A new spectroscopic observatory in Créteil to measure atmospheric trace gases in solar occultation geometry C. Viatte, P. Chelin, M. Eremenko, C. Keim,
SATELLITE REMOTE SENSING OF TERRESTRIAL CLOUDS Alexander A. Kokhanovsky Institute of Remote Sensing, Bremen University P. O. Box Bremen, Germany.
Limb Retrieval at IFE/IUP in Bremen Working team: A. Rozanov, K.-U. Eichmann, C. v. Savigny, J. Kaiser Tests based on level 0 data Normalisation by –Solar.
H 2 O retrieval from S5 NIR K. Weigel, M. Reuter, S. Noël, H. Bovensmann, and J. P. Burrows University of Bremen, Institute of Environmental Physics
1 COST 723 WG1 Meeting 1 October 6-7, 2003 University of Bern, CH Availability of UTLS relevant SCIAMACHY data C. von.
Vertical ozone change workshop, Geneva, 2011 SCIAMACHY limb ozone profiles C. von Savigny, A. Rozanov, M. Weber, S. Mieruch, N. Rahpoe, H. Bovensmann and.
High resolution solar reference spectrum Robert Voors KNMI.
The Orbiting Carbon Observatory (OCO) Mission: Retrieval Characterisation and Error Analysis H. Bösch 1, B. Connor 2, B. Sen 1, G. C. Toon 1 1 Jet Propulsion.
Validation of OMPS-LP Radiances P. K. Bhartia, Leslie Moy, Zhong Chen, Steve Taylor NASA Goddard Space Flight Center Greenbelt, Maryland, USA.
Kelly Chance Harvard-Smithsonian Center for Astrophysics Xiong Liu, Christopher Sioris, Robert Spurr, Thomas Kurosu, Randall Martin,
1 Xiong Liu Harvard-Smithsonian Center for Astrophysics K.V. Chance, C.E. Sioris, R.J.D. Spurr, T.P. Kurosu, R.V. Martin, M.J. Newchurch,
TNO Physics and Electronics Laboratory    J. Kusmierczyk-Michulec G. de Leeuw.
Rutherford Appleton Laboratory Requirements Consolidation of the Near-Infrared Channel of the GMES-Sentinel-5 UVNS Instrument: Initial trade-off: Height-resolved.
Global Characterization of X CO2 as Observed by the OCO (Orbiting Carbon Observatory) Instrument H. Boesch 1, B. Connor 2, B. Sen 1,3, G. C. Toon 1, C.
Flight Tests of the Novel TechSat Satellite Ozone Meter Algorithms and Measurement Processing Results M. Guelman, F. Ortenberg, B. Wolfson Asher Space.
Rutherford Appleton Laboratory Requirements Consolidation of the Near-Infrared Channel of the GMES-Sentinel-5 UVNS Instrument: FP, 25 April 2014, ESTEC.
Modeling of spectral fine-structure in GOME spectra Rutger van Deelen Otto Hasekamp Jochen Landgraf KNMI November 29, 2006.
Carbon monoxide from shortwave infrared measurements of TROPOMI: Algorithm, Product and Plans Jochen Landgraf, Ilse Aben, Otto Hasekamp, Tobias Borsdorff,
V2.0 minus V2.5 RSAS Tangent Height Difference Orbit 3761
Absolute calibration of sky radiances, colour indices and O4 DSCDs obtained from MAX-DOAS measurements T. Wagner1, S. Beirle1, S. Dörner1, M. Penning de.
Requirements Consolidation of the Near-Infrared Channel of the GMES-Sentinel-5 UVNS Instrument: FP, 25 April 2014, ESTEC Height-resolved aerosol R.Siddans.
Yoji Hayashi, Ryoichi Imasu Atmosphere and Ocean Research Institute,
Using SCIAMACHY to calibrate GEO imagers
UVIS Data Analysis and Modeling: Saturn FUV images
X. Liu1, C.E. Sioris1,2, K. 11/14/2018 Ozone Profile and Tropospheric Ozone Retrieval from SCIAMACHY Nadir Measurements:
Changchun Institute of Optics Fine Mechanics and Physics
Authors: B.Kerridge, R.Siddans, J.Reburn, B.Latter and V.Jay
Preliminary SCIAMACHY Lunar observations as intercalibration source
Presentation transcript:

page1 SCIAMACHY Calibration Review – ESTEC – Sept 2002 SCIAMACHY Tangent Height Verification H.Bovensmann University of Bremen Institute of Remote Sensing

page2 SCIAMACHY Calibration Review – ESTEC – Sept 2002 Content F Expectations from Instrument On-Ground Verification F General Approach F Limb tangent height verification F Occultation tangent height verification F Summary/Future Work

page3 SCIAMACHY Calibration Review – ESTEC – Sept 2002 On-Ground Verification F IFOV 0.045° (2.8 km) F Absolute pointing knowledge error 0.079° (4.6 km) F Relative pointing knowledge error 0.027° (1.6 km) F Cycle step size error 0.003° (170 m)

page4 SCIAMACHY Calibration Review – ESTEC – Sept 2002 General Approach F Use features in the backscattered or transmitted radiance with well known height dependence u Absorption of O 2 and CO 2 u Scattering and absorption characteristics at 305 nm around 45 km (so-caled „knee“) F Retrieve tangent height from this „features“ F Compare retrieved tangent height to data from L0/L1

page5 SCIAMACHY Calibration Review – ESTEC – Sept 2002 Limb tangent height verification F Idea: In the UV the backscattered radiance has a maximum („Knee“) in the upper stratosphere determined by dominating Rayleigh scattering (number density) above and (optical thick) Ozone absorption below the maximum (Janz et al. 1996) F UV-Knee, Sioris et al. F TRUE (modified Knee), J. Kaiser et al.

page6 SCIAMACHY Calibration Review – ESTEC – Sept 2002 UV limb radiance profiles optical thin optical thick „knee“

page7 SCIAMACHY Calibration Review – ESTEC – Sept 2002 UV-Knee (Sioris et al.) F find the knee heights for each spectral pixel around 305 nm on the original TH grid F find the knee heights simulated by a model (single scattering, O 3 from model atmosphere) F fit a curve to the wavelength (x-axis) vs knee z (y- axis) for the simulation and especially for the vertically undersampled observations (results have also been obtained for knee height vs pointing angle). F compare THs given by the polynomial expressions for observation and model. F Accuracy of better than 220 m is deduced for Orbit 1230

page8 SCIAMACHY Calibration Review – ESTEC – Sept 2002 UV-Knee (Sioris et al.)

page9 SCIAMACHY Calibration Review – ESTEC – Sept 2002 Tangent Height Retrieval by UV-B Exploitation (TRUE) (J. Kaiser et al.) F Generalised Knee Method (Janz et al. 1996) F normalised model spectra (UV-B) for all tangent heights are fitted simultaneously to the measured spectrum by varying: u tangent height (mean and step size), u O 3 concentration profile u pressure profile F Recommended fit interval 289 – 310 nm (ch. 1b)

page10 SCIAMACHY Calibration Review – ESTEC – Sept 2002 Normalised (TH 14, 32 km) Limb Spectra Channel 1 and 2

page11 SCIAMACHY Calibration Review – ESTEC – Sept 2002 TRUE Data Analysis F Up to now data with 1.6 km step size (26. May 2002) were analysed F raw data [counts] are divided by the integration time [s] to yield a flux-like quantity [counts/s] F preliminary dark current correction is performed by subtracting a measurement with 150 km tangent height F normalisation of all spectra to approx. 32 km tangent height (TH 14) eliminates most of the effects of the solar Fraunhofer structure and multiplicative instrumental artefacts

page12 SCIAMACHY Calibration Review – ESTEC – Sept 2002 F theoretical retrieval precision reaches 100 m for tangent heights 33–54 km F For 1.6 km step size measurements the following results were observed: u mean tangent height error: km u tangent height step: km u tangent height step error: km F Method is also sufficient to investigate parallelism of limb azimuth scan F Results consistent with Sioris et al. (220 m accuracy) F Report on methodology and first results is available TRUE Results

page13 SCIAMACHY Calibration Review – ESTEC – Sept 2002 First Results

page14 SCIAMACHY Calibration Review – ESTEC – Sept 2002 Occultation tangent height verification F O 2 B band absorption ch. 4 (690 nm) 10 – 65 km F CO 2 absorption ch. 6 (1560 nm) 10 – 20 km F L0 data Solar Occultations from orbit 514, 947 F L1 data Solar Occultations from orbit 2056 F Systematic shift of approx. 2 km observed w.r.t. L1 data

page15 SCIAMACHY Calibration Review – ESTEC – Sept 2002 Occultation

page16 SCIAMACHY Calibration Review – ESTEC – Sept 2002 Summary F Limb tangent height accurate within 100 – 200 m F Limb pointing performance seems to be an order of magnitude better than predicted from on-ground performance values (SCIA & ENVISAT) F Occultation tangent height shows a systematic deviation of approx. 2 km F Future Work: u Systematic analysis of orbit variations in tangent height u Data Analysis w.r.t. parallelism azimuth scan of limb measurements based on high data rate data with consolidated β-states (T int = s down to 290 nm) u Documentation of results