SMOS L2 Ocean Salinity www.argans.co.uk Level 2 Ocean Salinity v63x product design evolution 22 April 2015 ARGANS & SMOS L2OS ESL 1.

Slides:



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

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 – status, 17/09/2008 Level 2 Ocean Salinity Processor Project Status 17 September 2008 Samantha Lavender Paul Spurgeon.
SMOS L2 Ocean Salinity – Reprocessing Level 2 Ocean Salinity Reprocessing 17 September 2008.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity QWG #4 7-9 March 2011 ARGANS & L2OS ESL.
SMOS L2 Ocean Salinity L2OS QWG #4: RFI 7-9 March 2011 ARGANS & L2OS ESL.
SMOS L2 Ocean Salinity L1OP v620 border flag width 23 May 2014 ARGANS & L2OS ESL
SMOS L2 Ocean Salinity Level 2 Ocean Salinity L20S Tool Box Architecture & Release 27 June 2014 ARGANS & SMOS L2OS ESL.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity Processor TDS review 26 January 2009 Samantha Lavender Paul Spurgeon Caesar Mugerin.
SMOS L2 Ocean Salinity Reprocessed constant calibration L1c OTT drift study 13 April 2011 ARGANS & L2OS ESL ascendingdescending.
1 © ACRI-ST, all rights reserved – 2012 Galactic noise model adjustment Jean-Luc Vergely (ACRI-ST) Jacqueline Boutin (LOCEAN) Xiaobin Yin (LOCEAN)
AN INITIAL LOOK AT THE IMPACT OF THE NEW ANTENNA LOSS MODEL Joe Tenerelli SMOS QUALITY WORKING GROUP #4 7-9 March 2011.
SMOS – in situ comparisons J. Boutin*, N. Martin*, O. Hernandez*, N. Reul , G. Reverdin* *LOCEAN,  IFREMER.
F. Wentz, T. Meissner, J. Scott and K. Hilburn Remote Sensing Systems 2014 Aquarius / SAC-D Science Team Meeting November ,
1 MODAPS - Land Processing Status Robert Wolfe and Ed Masuoka Code 619, NASA GSFC Sadashiva Devadiga Sigma Space MODIS Science Team Meeting April 15-17,
SMOS L2 Ocean Salinity L2OS RFI study 9 May 2011 ARGANS & L2OS ESL.
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)
SMOS Ocean Salinity Retrieval Level 3 Marco Talone, Jérôme Gourrion, Joaquim Ballabrera, Marcos Portabella, and the SMOS Barcelona Expert Centre (SMOS-BEC)
Aquarius Status Salinity Retrieval and Applications D. M. Le Vine NASA/GSFC, Greenbelt, MD E. P. Dinnat, G. Lagerloef, P. de Matthaeis, H. Kao, F.
SMOS L2 Ocean Salinity – PM#25 1/20 Level 2 Ocean Salinity May 2013 v600 status v610 planning & schedule Slim-line UDP & improved.
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.
1.STSE 2.Objectives of today 3.Data availability 4.Reprocessing 5.RFI 6.Conferences & user meetings Introduction – SMOS mission status.
About L2OS v6 improvement wrt L2OS v5 N. Martin – J.L. Vergely - J. Boutin Descending orbits results In L2 v6 => latitudinal biases are reduced wrt L2.
Aquarius/SAC-D Mission Mission Simulators - Gary Lagerloef 6 th Science Meeting; Seattle, WA, USA July 2010.
L2OS RFI status Nicolas Lamquin, Jean-Luc Vergely Jacqueline Boutin Paul Spurgeon ICM, Barcelona, 16/17 May 2013.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity status 4 February 2013 ARGANS.
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 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 QWG-5, 30 May- 1 June 2011, ESRIN Ocean Salinity 1 1.Commissioning reprocessing analysis 2.New processor version: improvements and problems detected/solved.
SMOS L2 Ocean Salinity – status, 08/07/2009 Level 2 Ocean Salinity Processor July 2009 Paul Spurgeon Mike McCulloch.
Progress Meeting #27, April 2015, Barcelona SPAIN T3.2 Retrieval algorithm Estrella Olmedo BEC team SMOS Barcelona Expert Centre Pg. Marítim de la.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity Planning the year ahead 21 April 2015 ARGANS & SMOS L2OS ESL 1.
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.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity PM # May 2011 ARGANS & L2OS CLS.
SCIENCE PROCESSING OVERVIEW David Le Vine Aquarius Deputy PI 07 July 2009.
Ocean Salinity validation of mission requirements review / improvements: Points of Reflexion ESL teams Mission Requirements: The so-called GODAE requirements:
25 June 2009 Dawn Conway, AMSR-E TLSCF Lead Software Engineer AMSR-E Team Leader Science Computing Facility.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity PM # November 2010 ARGANS & L2OS LOCEAN, Paris.
SMOS QWG-11, ESRIN 4-5 July 2013 L2OS v600 status and evolution 1 The SMOS L2 OS Team.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity Status 9 February 2015 ARGANS & SMOS L2OS ESL 1.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity L2OS planning 2 July 2014 ARGANS & SMOS L2OS ESL 1.
SMOS AlgoVal meeting #16, Brest, 8-9 July, 2009 Computing Tb BOA and Tb surf C. Gabarró, J. Font SMOS Barcelona Expert Centre Pg. Marítim de la Barceloneta.
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.
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.
EXTENDING THE LAND SEA CONTAMINATION CHARACTERIZATION TO THE EXTENDED ALIAS- FREE FIELD OF VIEW Joe Tenerelli (CLS) and Nicolas Reul (IFREMER) SMOS Quality.
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,
SMOS QWG-6, ESRIN October 2011 OTT generation strategy and associated issues 1 The SMOS L2 OS Team.
USING SMOS POLARIMETRIC BRIGHTNESS TEMPERATURES TO CORRECT FOR ROUGH SURFACE EMISSION BEFORE SALINITY INVERSION.
Workshop Agenda: Day One 9:30 IntroductionLagerloef / Le Vine 9:45 Workshop objectivesG. Feldman 10:00 Overview of the Aquarius Data Processing System:G.
Cal/Val Discussion. Summary No large errors in rain, freshening observed by Aquarius can be significant and real (up to about 3 hours on average after.
Outlier detection in L2OSPP - usefulness in RFI detection- SMOS L2OS Progress Meeting – 21/22 February -BEC.
SMOS Quality Working Group Meeting #2 Frascati (Rome), September 13 th -14 th,2010 SMOS-BEC Team.
SMOS QWG-9, ESRIN October 2012 L2OS: Product performance summary v550 highlights 1 The SMOS L2 OS Team.
T. Meissner and F. Wentz Remote Sensing Systems 2014 Aquarius / SAC-D Science Team Meeting November , 2014 Seattle. Washington,
21-23/04/2015PM27 J-L Vergely, J. Boutin, N. Kolodziejczyk, N. Martin, S. Marchand SMOS RFI/Outlier filtering.
SMOS L2 Ocean Salinity G-POD and L2OS 4 February 2013 ARGANS.
SMOS L2 Ocean Salinity – PM#25 1/20 Level 2 Ocean Salinity May 2013 A3TEC.
SMOS Science Meeting September 2011 Arles, FR Simulating Aquarius by Resampling SMOS Gary Lagerloef, Yann Kerr & Eric Anterrieu and Initial Results.
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.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity L2OS v611 status 12 February 2014 ARGANS & SMOS L2OS ESL.
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.
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.
Presentation transcript:

SMOS L2 Ocean Salinity Level 2 Ocean Salinity v63x product design evolution 22 April 2015 ARGANS & SMOS L2OS ESL 1

SMOS L2 Ocean Salinity When to apply land-sea correction? 2 L2OS TDS (lsc01/2): Outlier detection (decision tree): apply OTT & LSC. Sets measurement, snapshot & RFI flags. If retrieving A3TEC for OTT computation, do not apply OTT or LSC (A3TEC algorithm retrieves OTT) Compute OTT correction per model M1/2/3 (ottTB in AUX_DTBXY: mean forward model OTT TB for all measurements in each snapshot FOV sub-zone, can be compared to modelTB/deltaTB) – not used in retrievals If A3TEC for retrievals, apply OTT & LSC (A3TEC does not retrieve OTT), & compute outlier detection again using new TEC. For each retrieval (M1/2/3 & Acard), apply OTT & LSC per grid point

SMOS L2 Ocean Salinity Design for land-sea correction 3 4 x retrievals in v62x: SSS1/2/3 & Acard 4 threads gives ~12:1 reprocessing performance Convergence algorithm ~28% of processing time Max RAM ~ 6G Land-sea LUT (containing ascending & descending LUTs) is ~2.2G Could split into 2, but no performance advantage Reading land-sea LUT takes ~ 30 seconds, applying LUT very fast. Land-sea LUT is applied at the same time as OTT, before running A3TEC retrieval, measurement selection, & convergence (per forward model). Land-sea LUT adds ~0.9G (not scene dependent).

SMOS L2 Ocean Salinity Options for land-sea correction 4 A.4 x retrievals with land-sea correction applied to SSS1/2/3 & Acard (or a selection of these) (same as May 2011 lsc01/2 TDS) No UDP/DAP format changes required No significant impact on processing performance B.Retrieve SSS with & without land-sea correction: which model? UDP will contain 2 x SSS & Acard Faster processing (only 3 retrievals): 14:1 (M1) or better C.6 x retrievals with & without land-sea correction applied to SSS1/2/3, & Acard UDP will contain 6 x SSS, & Acard Processing performance degraded to 10:1 Best for users: UDP with 1 SSS selected from several (<4) retrievals, & 1 Acard DAP can contain anything – ie all retrieval results All retrievals with land-sea correction applied (via config switch) Need criteria to select which SSS to write into UDP…

SMOS L2 Ocean Salinity SSS1/2/3 are similar due to OTT & land-sea correction 5 SSS1

SMOS L2 Ocean Salinity SSS1/2/3 are similar due to OTT & land-sea correction 6 SSS2

SMOS L2 Ocean Salinity SSS1/2/3 are similar due to OTT & land-sea correction 7 SSS3

SMOS L2 Ocean Salinity Criteria to select a single SSS for UDP 8 Need results from ESL analysis (& JLV T1.3) Criteria could include: Best (lowest) Dg_quality_SSSx Best Dg_chi2/chi2P No poor_retrieval flags raised Classification of geophysical conditions: do some models perform better eg in cold waters or high winds? Or average of all 3 SSS (if no poor quality flags & Dg_quality < 150)?

SMOS L2 Ocean Salinity UDP design n x grid points: Grid point data (6) ID, latitude, longitude, footprint, time, x_swath Science flags (4 x 22) land, rain, ice, sea state, hi/lo wind/SST/SSS Geophysical retrievals (10) SSS1, SSS2, SSS3, Acard & sigmas, WS, SST TB42.5 (8) modelled BTs & sigmas at surface & antenna Product confidence (33) quality index, chi2, chi2P, nIter for SSS1/2/3/Acard Dg_xxx counters (17) Control flags (4 x 30) ignored, valid, range, sigma, chi2, chi2P, sun/moon/gal glint, maxiter, meas min/low, outliers, marq, rough, foam, ecmwf, poor geophysical/retrieval, rfi v62x (208 flags & 58 fields) v63x (54 flags & 59 fields) n x grid points: Grid point data (6) ID, latitude, longitude, footprint, time, x_swath Science flags (1 x 22) land, rain, ice, sea state, hi/lo wind/SST/SSS Geophysical priors & retrievals (4 x 5) SSS, WS, SST, TEC, Acard & sigmas TB42.5 (8) modelled BTs & sigmas at surface & antenna Product confidence (25) quality index, chi2, chi2P, nIter for SSS/Acard Dg_xxx counters (17) Control flags (1 x 32) ignored, valid, range, sigma, chi2, chi2P, sun/moon/gal glint, maxiter, meas min/low, outliers, marq, rough, foam, ecmwf, poor geophysical/retrieval, rfi, model

SMOS L2 Ocean Salinity UDP/DAP format changes: decisions & actions 10 Always apply land-sea correction? Single SSS in UDP? Run all 3 models in convergence algorithm, select ‘best’ SSS?