Galactic noise model adjustment Jean-Luc Vergely (ACRI-ST) Jacqueline Boutin (LOCEAN) Xiaobin Yin (LOCEAN)

Slides:



Advertisements
Similar presentations
Analysis of AMSR-E C & X-band Tb data dependencies with wind & wave characteristics.
Advertisements

1 © ACRI-ST, all rights reserved – 2012 Isotropic RFI detection Jean-Luc Vergely (ACRI-ST) Claire Henocq (ACRI-ST) Philippe Waldteufel (LATMOS)
SMOS L2 Ocean Salinity Commissioning Plan, 07/05/2009 Level 2 Ocean Salinity Processor Commissioning Plan 7 May 2009 ARGANS ACRI-ST ICM-CSIC.
SMOS L2 Ocean Salinity – Reprocessing Level 2 Ocean Salinity Reprocessing 17 September 2008.
1 © ACRI-ST, all rights reserved – 2012 Galactic noise model adjustment Jean-Luc Vergely (ACRI-ST) Jacqueline Boutin (LOCEAN) Xiaobin Yin (LOCEAN)
UPDATE ON BIAS TRENDS, DIRECT SUN CORRECTION, AND ROUGHNESS CORRECTION Joe Tenerelli May 10, 2011.
AN INITIAL LOOK AT THE IMPACT OF THE NEW ANTENNA LOSS MODEL Joe Tenerelli SMOS QUALITY WORKING GROUP #4 7-9 March 2011.
UPDATE ON SMOS LONG-TERM BIASES OVER THE OCEAN AND ROUGH SURFACE SCATTERING OF CELESTIAL SKY NOISE Joe Tenerelli SMOS L2OS Progress Meeting Arles, France,
F. Wentz, T. Meissner, J. Scott and K. Hilburn Remote Sensing Systems 2014 Aquarius / SAC-D Science Team Meeting November ,
Computational Statistics. Basic ideas  Predict values that are hard to measure irl, by using co-variables (other properties from the same measurement.
OSE meeting GODAE, Toulouse 4-5 June 2009 Interest of assimilating future Sea Surface Salinity measurements.
SMOS L1v620-L2v613 versus L1v505- L2v550 validation May 2011 Nicolas Martin, Jacqueline Boutin LOCEAN 26 May 2014.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity L1 -> L2OS tools 12 February 2014 ARGANS & SMOS L2OS ESL.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity Using TEC estimated from Stokes 3 24 October 2012 ACRI-st, LOCEAN & ARGANS SMOS+polarimetry.
1 © ACRI-ST, all rights reserved – 2012 TEC estimation Jean-Luc Vergely (ACRI-ST) Jacqueline Boutin (LOCEAN)
The Aquarius Salinity Retrieval Algorithm Frank J. Wentz and Thomas Meissner, Remote Sensing Systems Gary S. Lagerloef, Earth and Space Research David.
MIRAS performance based on OS data SMOS MIRAS IOP 6 th Review, ESAC – 17 June 2013 Prepared by: J. Font, SMOS Co-Lead Investigator, Ocean Salinity – ICM-CSIC.
1 Analysis of Airborne Microwave Polarimetric Radiometer Measurements in the Presence of Dynamic Platform Attitude Errors Jean Yves Kabore Central Florida.
IFREMER EMPIRICAL ROUGHNESS MODEL Joe Tenerelli, CLS, Brest, France, November 4, 2010.
Sea water dielectric constant, temperature and remote sensing of Sea Surface Salinity E. P. Dinnat 1,2, D. M. Le Vine 1, J. Boutin 3, X. Yin 3, 1 Cryospheric.
BCOR 1020 Business Statistics Lecture 28 – May 1, 2008.
Aquarius/SAC-D Science Meeting Seattle, WA July 2010 College of Engineering Department of Atmospheric, Oceanic & Space Sciences Chris Ruf Space Physics.
L2OS RFI status Nicolas Lamquin, Jean-Luc Vergely Jacqueline Boutin Paul Spurgeon ICM, Barcelona, 16/17 May 2013.
Ifremer Planning of Cal/Val Activities during In orbit commisioning Phase N. Reul, J. Tenerelli, S. Brachet, F. Paul & F. Gaillard, ESL & GLOSCAL teams.
SMOS Validation Rehearsal Campaign Workshop, 18-19/11/2008, Noordwijkerhout, The Netherlands SMOS Validation Rehearsal Campaign Mediterranean flights C.
SMOS L2 Ocean Salinity – PM#25 1/20 Level 2 Ocean Salinity May 2013 OTT post-processor.
MWR Roughness Correction Algorithm for the Aquarius SSS Retrieval W. Linwood Jones, Yazan Hejazin, Salem Al-Nimri Central Florida Remote Sensing Lab University.
SMOS Science Workshop, Arles, th Sept, 2011 IMPROVING SMOS SALINITY RETRIEVAL: SYSTEMATIC ERROR DIAGNOSTIC J. Gourrion, R. Sabia, M. Portabella,
SMOS QWG-5, 30 May- 1 June 2011, ESRIN Ocean Salinity 1 1.Commissioning reprocessing analysis 2.New processor version: improvements and problems detected/solved.
Progress Meeting #27, April 2015, Barcelona SPAIN T3.2 Retrieval algorithm Estrella Olmedo BEC team SMOS Barcelona Expert Centre Pg. Marítim de la.
SMOS SSS and wind speed J. Boutin, X. Yin, N. Martin -Optimization of roughness/foam model -Comparison of new-old ECMWF wind speeds -SSS anomaly in the.
Calibration and Validation Studies for Aquarius Salinity Retrieval PI: Shannon Brown Co-Is: Shailen Desai and Anthony Scodary Jet Propulsion Laboratory,
UPDATE ON THE SUN GLINT Joe Tenerelli Ocean Data Lab SMOS Level 2 OS Progress Meeting 26 SMOS Barcelona Expert Centre Barcelona, Spain April 2015.
7 th SMOS Workshop, Frascati, October /17 AMIRAS campaign Fernando Martin-Porqueras.
A. Montuori 1, M. Portabella 2, S. Guimbard 2, C. Gabarrò 2, M. Migliaccio 1 1 Dipartimento per le Tecnologie (DiT), University of Naples Parthenope, Italy.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity L2OS planning 2 July 2014 ARGANS & SMOS L2OS ESL 1.
1 / 13 Current activities at ICM-SMOS-BEC J. Gourrion, C. Gabarró, R. Sabia, M. Talone, V. González, S. Montero, S. Guimbard, F. Pérez, J. Martínez, M.
SPCM-9, Esac, May 3 rd, 2012 MODEL-INDEPENDENT ESTIMATION OF SYSTEMATIC ERRORS IN SMOS BRIGHTNESS TEMPERATURE IMAGES J. Gourrion, S. Guimbard, R. Sabia,
Dependence of SMOS/MIRAS brightness temperatures on wind speed and foam model Xiaobin Yin, Jacqueline Boutin LOCEAN & ARGANS.
Level 2 Algorithm. Definition of Product Levels LevelDescription Level 1 1A Reconstructed unprocessed instrument data 1B Geolocated, calibrated sensor.
OS-ESL meeting, Barcelona, February nd, 2011 OTT sensitivity study and Sun correction impact J. Gourrion and the SMOS-BEC team SMOS-BEC, ICM/CSIC.
Optimization of L-band sea surface emissivity models deduced from SMOS data X. Yin (1), J. Boutin (1), N. Martin (1), P. Spurgeon (2) (1) LOCEAN, Paris,
Introduction Martin et al. JGR, 2014 CAROLS airborne Tbs indicate slightly lower wind influence than predicted by model 1 at high WS In model 1 previous.
SMOS QWG-6, ESRIN October 2011 OTT generation strategy and associated issues 1 The SMOS L2 OS Team.
Space Reflecto, November 4 th -5 th 2013, Plouzané Characterization of scattered celestial signals in SMOS observations over the Ocean J. Gourrion 1, J.
Sea Surface Salinity as Measured by SMOS and by Surface Autonomous Drifters: Impact of Rain J. Boutin, N. Martin, X. Yin, G. Reverdin, S. Morrisset LOCEAN,
USING SMOS POLARIMETRIC BRIGHTNESS TEMPERATURES TO CORRECT FOR ROUGH SURFACE EMISSION BEFORE SALINITY INVERSION.
SMOS-BEC – Barcelona (Spain) LO calibration frequency impact Part II C. Gabarró, J. Martínez, V. González, A. Turiel & BEC team SMOS Barcelona Expert Centre.
QWG-10 ESRIN 4-6 February 2013 Quality control study for SMOS data / Flags analysis C. Gabarró, J. Martínez, E. Olmedo M. Portabella, J. Font and BEC team.
QWG8, Boutin et al. SMOS and Aquarius: SSS and Wind Effect J. Boutin, X. Yin, N. Martin (LOCEAN, Paris), E. Dinnat (Chapman University/NASA/GSFC), S. Yueh.
Simulator Wish-List Gary Lagerloef Aquarius Principal Investigator Cal/Val/Algorithm Workshop March GSFC.
SMOS QWG-9, ESRIN October 2012 L2OS: Product performance summary v550 highlights 1 The SMOS L2 OS Team.
New model used existing formulation for foam coverage and foam emissivity; tested over 3 half orbits in the Pacific foam coverage exponent modified to.
SMOS mission: a new way for monitoring Sea Surface Salinity? J. Boutin (1) (1) Laboratoire d’Oceanographie et du Climat- Expérimentation et Applications.
T. Meissner and F. Wentz Remote Sensing Systems 2014 Aquarius / SAC-D Science Team Meeting November , 2014 Seattle. Washington,
Estimation of wave spectra with SWIM on CFOSAT – illustration on a real case C. Tison (1), C. Manent (2), T. Amiot (1), V. Enjolras (3), D. Hauser (2),
Level 2 Scatterometer Processing Alex Fore Julian Chaubell Adam Freedman Simon Yueh.
21-23/04/2015PM27 J-L Vergely, J. Boutin, N. Kolodziejczyk, N. Martin, S. Marchand SMOS RFI/Outlier filtering.
A step toward operational use of AMSR-E horizontal polarized radiance in JMA global data assimilation system Masahiro Kazumori Numerical Prediction Division.
Impact of sea surface roughness on SMOS measurements A new empirical model S. Guimbard & SMOS-BEC Team SMOS Barcelona Expert Centre Pg. Marítim de la Barceloneta.
Errors on SMOS retrieved SSS and their dependency to a priori wind speed X. Yin 1, J. Boutin 1, J. Vergely 2, P. Spurgeon 3, and F. Gaillard 4 1. LOCEAN.
UPDATE ON GALACTIC NOISE CORRECTION Joe Tenerelli SMOS Quality Working Group #9 ESA ESRIN 24 October 2012.
Dependence of SMOS/MIRAS brightness temperatures on wind speed: sea surface effect and latitudinal biases Xiaobin Yin, Jacqueline Boutin LOCEAN.
Universitat Politècnica de Catalunya CORRECTION OF SPATIAL ERRORS IN SMOS BRIGHTNESS TEMPERATURE IMAGES L. Wu, I. Corbella, F. Torres, N. Duffo, M. Martín-Neira.
21-23/04/2015PM27 ACRI-ST ARGANS LOCEAN TEC follow-up.
Tests on V500 Sun On versus Sun Off 1)Tbmeas. –Tbmodel in the FOV X. Yin, J. Boutin Inputs from R. Balague, P. Spurgeon, A. Chuprin, M. Martin-Neira and.
(2) Norut, Tromsø, Norway Improved measurement of sea surface velocity from synthetic aperture radar Morten Wergeland Hansen.
Institute of Low Temperature Science, Hokkaido University
Roughness Correction for Aquarius (AQ) Sea Surface Salinity (SSS) Algorithm using MicroWave Radiometer (MWR) W. Linwood Jones, Yazan Hejazin Central FL.
Statistical Methods For Engineers
Presentation transcript:

Galactic noise model adjustment Jean-Luc Vergely (ACRI-ST) Jacqueline Boutin (LOCEAN) Xiaobin Yin (LOCEAN)

Galactic model versus SMOS measurements Modelled signal is underestimated. Bias of about 1 K. Joe Tenerelli (CLS, 2011)

Aim of this study To better understand rugosity in L band To diagnose where the bias comes from To give leads in order to correct the bias To estimate the corrections for some operating points

The way to approach the galactic contribution Semi-empirical approach : to perform a new model. Formalization of the problem and simplification. Extraction of the reflected signal from relevant orbits. Estimation of the parameters of the new model.

Formalization of the problem (1) Model : By hypothesis : St3 and St4 = 0

Formalization of the problem (2) Weighting by the antenna lobe : Ground-antenna transformation

Approximation Assumption : Incident galactic signal is unpolarized : Tbgal_H=Tbgal_V=Tbgal With : Antenna lobe affects in theory directly the bistatic coefficients at the ground level. Approximation : to apply antenna lobe on the galactic map.

Inversion of the forward model (1) Data : SMOS Tbgal_refl_X and Tbgal_refl_Y – flat sea and roughness contribution – OTT – atmospheric contribution Forward model : With b=cos²(a) or b=sin²(a), a being the rotation angle ground->antenna Inversion shall be done at the antenna level : bayesian approach as for SSS retrieval. UNKNOWN : and

Inversion of the forward model (2) Different inversion schemes : -at small rotation angle (TB close to the track) : TBX=TBH and TBY=TBV. Possibility to retrieve independently σ H and σ V. -at high rotation angle : necessity to retrieve σ H and σ V simultaneously -with different parameterizations : different priors. Constraints or not on the integral. Constraint of positivity (non linear process). -considering axisymmetric bistatic coefficients which do not depend on : a/ WS azimuth b/ azimuth direction of the incidence plane according to the celestial sphere. c/ SSS and SST

Tests using simulated data Finding specular reflection points with same relative geometry and same WS Using SMOS data after averaging Deconvolution with strong a priori knowledge Residual TBs Assumptions : incident galactic noise is not polarized. WEF applied before reflection Bistatic retrieval : non parametric Bayesian approach with a priori correlation length.

SMOS data selection 28 descending half orbits in the south pacific in the period 12/09/2010 – 12/10/2010 => strong galactic signal is expected. Selection of data : no contamination by land, TB valid, geometric rotation < 10° : TBH and TBV processed independently. Place the data in (ra, dec, WS, theta) super cube : average and standard deviation in each cell of the cube.

Data presentation (1) SMOS orbit 09/10/2010 Polar XPolar Y

SMOS orbit 09/10/2010 X polar Theory (current model) SMOS residues Data presentation (2) Y polar

Comparison of SMOS data with current model Data presentation (3) X polarY polar

Comparison of SMOS data with current model : orbit with low wind speed. Data presentation (4) X polarY polar

X polar Data presentation (5) Y polar SMOS data according wind speed.

X polar Data presentation (6) Y polar SMOS data according incidence angle (selection in ra/dec toward GC, afFOV)

Data presentation (7) Definition of 20 cells in (WS, theta) space : WS : 4 intervals [1.5m/s 4.5m/s], [1.5m/s 4.5m/s], [1.5m/s 4.5m/s], [1.5m/s 4.5m/s] θ : 5 intervals [0° 10°], [10° 20°], [20° 30°], [30° 40°], [40° 50°] Sampling in the (ra, dec) space : 0.5 °x 0.5 ° boxes Cumul of 28 descending orbits Galactic plane crosses the orbits at different x_swath positions : 12/10/ /09/ /09/2010 RA DEC

Data presentation (8) Data averaging in cells. Polar X Average data. WS = 3m/s, θ=15° Average data. WS = 6m/s, θ=45°

Data presentation (9) Data averaging in cells : Statistic properties. Data number. WS = 3m/s, θ=15° Data number. WS = 6m/s, θ=45°

Data presentation (10) Data averaging in cells : Statistic properties. Exemple of TB histogram from one cell in the cube (ra,dec,WS,theta) Std of histogram is expected to be close to the radiometric noise. Effective std is between 2.3 and 3 K for 100 data => error of the mean is about 0.3 K

Preliminary retrieval results polar H

Preliminary retrieval results polar V

Preliminary retrieval results Data Fitting in polar H (θ=45°)

Preliminary retrieval results Data Fitting in polar V (θ=45°)

Preliminary retrieval results polar Hpolar V Reflection coefficients RH and RV

Bias in the current model : where it comes from ? Bias in the modelled bistatic coefficients ? Wrong assumptions (lobe, axisymmetry) ? Bias in the ECMWF auxiliary data (wind speed) ? Bias in the OTT correction ? Bias in the galactic map ? Bias in the L1 reconstruction ? Bias due to the target heterogeneity ? Other sources ?