sst quality monitor (squam): focus on suomi npp viirs
DESCRIPTION
2012 EUMETSAT Meteorological Satellite Conference 3 – 7 September, 2012, Sopot, Poland. SST Quality Monitor (SQUAM): Focus on Suomi NPP VIIRS. www.star.nesdis.noaa.gov/sod/sst/squam. Prasanjit Dash 1,2 and Alexander Ignatov 1 1 NOAA/NESDIS, Center for Satellite Applications & Research (STAR) - PowerPoint PPT PresentationTRANSCRIPT
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 1
2012 EUMETSAT Meteorological Satellite Conference
3 – 7 September, 2012, Sopot, Poland
SST Quality Monitor (SQUAM):Focus on Suomi NPP VIIRS
Prasanjit Dash1,2 and Alexander Ignatov1
1NOAA/NESDIS, Center for Satellite Applications & Research (STAR)2Colorado State Univ, Cooperative Institute for Research in the Atmosphere (CIRA)
Objective: A global, web-based, community, quasi NRT, monitor for SST producers & users !
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 2
Major SST data providers: Projects and international group
Contributions/Support
Level-2 SST: VIIRS/AVHRR/MODIS- NESDIS SST Team : ACSPO (GAC: 5 platforms, FRAC: MetOp-A, VIIRS: NPP, MODIS: Terra/Aqua)- P. LeBorgne: O&SI SAF MetOp-A FRAC- D. May, B. McKenzie: NAVO SEATEMP- S. Jackson: IDPS (NPP)
Level-3 SST: AVHRR:- K. Casey, R. Evans, J. Vazquez, E. Armstrong: PathFinder v5.0
Level 4 SSTs:- R. Grumbine, B. Katz: RTG (Low-Res & Hi-Res)- R. Reynolds, V. Banzon: OISSTs (AVHRR & AVHRR+AMSRE)- M. Martin, J. R. Jones: OSTIA foundation, GHRSST Median Product Ensemble, OSTIA Reanalysis- D. May, B. McKenzie: NAVO K10- J.-F. Piollé, E. Autret : ODYSSEA- E. Maturi, A. Harris, J. Mittaz: POES-GOES blended- B. Brasnett: Canadian Met. Centre, 0.2 foundation- Y. Chao: JPL G1SST- H. Beggs: ABOM GAMSSA- M. T. Chin, J. Vazquez, E. Armstrong: JPL MUR
L4s in SQUAM pipeline:J. Hoyer:DMI OISST; S. Ishizaki:MGDSST; C. Gentemann:RSS products; J. Cummings:NCODA
GHRSST support: - Craig Donlon, Peter Minnett, Alexey Kaplan
Definitions of levels:L2: at observed pixels (satellite)L3: gridded with gaps (satellite)L4: gap-free gridded, time-averaged
CMC
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SST datasets available in community
Level 4Reynolds (AVHRR; +AMSR-E*)
RTG (Low, High Resolution), GSI
OSTIA, Operational + Retro (UKMO)
ODYSSEA (France)
GMPE (GHRSST)
NAVO K10
NESDIS POES-GOES Blended
JPL G1SST, JPL MUR
NCODA (NRL)
CMC 0.2 (Canada)
GAMSSA (Australia)
MGDSST (JAXA, Japan)
RSS (MW, MW+MODIS)
DMISST (Danish Met. Inst.)
In situSources-GTS, ICOADS, GODAE/FNMOC
Platforms-Drifters, Moorings, Ships, ARGO Floats
Quality Control-May be unavailable or non-uniform
Level 2/3Polar-AVHRR (NESDIS, NAVO, O&SI SAF, U. Miami, NODC)-VIIRS (NESDIS, IDPS),MODIS,ATSR,-Microwave
Geostationary-GOES (NESDIS, NAVO, O&SI SAF)-SEVIRI (NESDIS, O&SI SAF)-MTSAT (NESDIS, JAXA)
- SST community is data-rich
- Are these products self-consistent? Cross-consistent?
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SQUAM Objectives and Methodology
Cross-evaluate all major global SST products and validate against consistent reference standard, in near-real time
Report summary performance statistics online
SQUAM is organized into three major modules: L2, L3, and L4
The diagnostics aimed at assessing (relative) performance of
o Cloud mask
o SST Algorithm
o Ice-mask ..
Methodology
Analyze global differences, ΔTS = TS minus expected TR
• Evaluate global maps for “uniformity”
• Evaluate distributions for Normality (X~N(µ,σ))
• Compare and Trend Gaussian parameters in time
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NPP VIIRS(TS) – Drifters(TR):
Conventional Val wrt. In situ SST:
- Sparse (voids), geographically non-uniform
- Quality non-uniform & sub-optimal
- Number of Match-ups ~2,000/Night
NPP VIIRS(TS) – OSTIA(TR):
Using L4:
- Complements traditional in situ VAL
- Global snapshot, in near-real time
- Number of Match-ups 90,000,000/Night
Choice of expected state: In situ or L4?
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SQUAM Interface
Locate this website: Google: “SST + SQUAM”, the first hit
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L2/3 SQUAMΔTS (TS - TR) analyzed:
Maps
Histograms
Time series (Gaussian moments, outlier info, double differences)
Dependencies (on geophysical & observational parameters)
Hovmöller Diagrams (Time series of dependencies)
The SST Quality Monitor (SQUAM)Journal of Atmospheric & Oceanic Technology, 27, 1899-1917, 2010
(GHRSST ST-VAL)
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L2/L3 SQUAM: Maps Histograms Time-series Dependencies
Hovmöller
• The Suomi National Polar Partnership (NPP) satellite launched in Oct 2011
• Cryoradiator Doors opened on 18 Jan 2012• VIIRS Global SST Products produced since 23 Jan 2012
ACSPO and IDPS: Two SST processing systems applied to the same satellite data
– ACSPO (Advanced Clear-Sky Processor for Oceans) - NOAA– IDPS (Interface Data Processing Segment) – NPOESS Contractor,
transitioning to NOAA
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 9
L2/L3 SQUAM: Maps Histograms Time-series Dependencies
Hovmöller
NIGHT: ACSPO VIIRS L2 minus OSTIA L4, 13 August 2012
• Deviation from TR is flat & close to 0• Residual Cloud/Aerosol leakages seen in the Tropics
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 10
L2/L3 SQUAM: Maps Histograms Time-series Dependencies
Hovmöller
NIGHT: IDPS VIIRS L2 minus OSTIA L4, 13 August 2012
• More Cloud leakages in IDPS than in ACSPO Two processors applied to the same satellite dataMore HR Level-2 SST analyses at:http://www.star.nesdis.noaa.gov/sod/sst/squam/HR/
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 11
L2/L3 SQUAM: Maps Histograms Time-series Dependencies
Hovmöller
NIGHT: ACSPO VIIRS L2 minus OSTIA L4, 13 August 2012
• Shape close to Gaussian• Domain and performance stats close to expected
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L2/L3 SQUAM: Maps Histograms Time-series Dependencies
Hovmöller
• IDPS confidently clear sample ~27% larger• Shape less Gaussian (negative skewness, increased kurtosis)• Increased Std Dev/Robust Std Dev; Larger fraction of outliers
NIGHT: IDPS VIIRS L2 minus OSTIA L4, 13 August 2012
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 13
L2/L3 SQUAM: Maps Histograms Time-series Dependencies
Hovmöller
# (%ACSPO) Min/ Max Mean/ STD Med/ RSD Skew/ Kurt
ACSPO 93.2 M (100%) -7.3/ +15.3 -0.01/0.58 +0.01/0.45 +0.7/ +9.0
IDPS 118.3 M (127%) -17.1/+26.7 -0.23/0.89 -0.18/0.47 -1.64/+32.3
Summary stat of ΔT = “VIIRS minus OSTIA” SST for 13 Aug 2012(expected ~0)
• IDPS SST domain +27% larger than ACSPO
• IDPS performance statistics degraded, compared to ACSPO
• Gap between Conventional and Robust stats wider in IDPS - More outliers
IDPS/ACSPO Analyses routinely performed in SQUAM
Comparisons with other AVHRR and MODIS products are also done
VIIRS, MODIS, and AVHRR SST products are being improved
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 14
L2/L3 SQUAM: Maps Histograms Time-series Dependencies
Hovmöller
SST Std Dev from OSTIA for VIIRS, AVHRR, MODIS
•AVHRR and MODIS closely track each other•ACSPO VIIRS is consistent with MODIS/AVHRR•So far, IDPS VIIRS EDR shows larger Std Dev than ACSPO
NPP JPSS
Warm-Up Cool-Down Event
IDPS shows larger Std Dev
Loss of Envisat
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Inter-compare L4 SSTs using similar diagnostics:
maps, histograms, time series, Hovmöller
All analyses are done in two modes:
including and excluding ice fields (if ice flags available)
Validate consistently against quality controlled in situ data
Group for High Resolution Sea Surface Temperature (GHRSST) analysis fields inter-comparisons—Part 1: A GHRSST multi-product ensemble (GMPE)Deep Sea Research Part II:, 77-80, 21-30, 2012
Group for High Resolution Sea Surface Temperature (GHRSST) analysis fields inter-comparisons—Part 2: Near real time web-based level 4 SST Quality Monitor (L4-SQUAM)Deep Sea Research Part II:, 77-80, 31-43, 2012
L4 intercomparison
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 16
http://www.star.nesdis.noaa.gov/sod/sst/squam/L4/
L4 SQUAM: Maps Histograms Time-series Hovmöller
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 17
Summary and Future Work
SQUAM currently monitors major global polar L2/3 SST products from VIIRS, MODIS, and AVHRR, and 14 L4 SST products
Two VIIRS SST products were added in Jan 2012: ACSPO and IDPS
ACSPO SST is consistent with AVHRR/MODIS family, IDPS SST is less accurate
Work is underway to improve both VIIRS SST products, and reconcile
Future data additions in SQUAMo Polar: MODIS MOD29/MYD28 and (A)ATSR
o Geostationary: MSG, MTSAT, GOES – Preparation for GOES-R
o Remaining L4 SSTs
Work with community towards Improved self- and cross-consistency of SST productso Improve cloud masks, SST algorithms, sensor calibration
o Explore SST diurnal variability models
o Understand relative merit and differences of products, and reconcile
o Facilitate blending towards improved analyses, forecast, and climate
THANK YOU!
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BACK UP Slides
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SQUAM web
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Role / Responsibility
NOAA/POES and NASA/EOS
NPOESS JPSS
Platform, Launch Vehicle
Private Industry Private Industry Private Industry
Instruments Private Industry Private Industry Private Industry
Algorithms Government Private IndustryIn transition to Government
Data Products Government Private Industry IPO/NPOESS
Cal/Val Government Private Industry Government
Archival & Distribution
Government Government Government
JPSS Data Products:IDPS – Interface Data Processing Segment
Algorithms: IPO/NPOESS (Northrop Grumman Aerospace Systems) Operational Products: IPO/NPOESS (Raytheon) IDPS (RDRs, SDRs, EDRs)
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 21
L2/L3 SQUAM: Maps Histograms Time-series Dependencies
Hovmöller
High Res. L2 SST mean differences:VIIRS, AVHRR, MODIS
-ACSPO VIIRS is consistent with MODIS & AVHRR
- IDPS VIIRS EDR shows larger diff (also Std Dev; not shown)
L2 vs. in situ driftersnight, ~1500-2000/day
NPP JPSS
Warm-Up Cool-Down Event
L2 vs. OSTIAnight, ~50-100mi/day
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NIGHT STD DEV wrt. OSTIA L4
• AVHRR & MODIS SSTs are consistent• ACSPO VIIRS is consistent with MODIS & AVHRR • IDPS VIIRS EDR shows larger STD DEV
Warm-Up Cool-Down Event
IDPS shows larger STD DEV
L2/L3 SQUAM: Maps Histograms Time-series Dependencies
Hovmöller
2012 EUMETSAT Met. Sat. Conf., 6-Sep-2012, Sopot, Poland 23
DAY STD DEV wrt. OSTIA L4
Warm-Up Cool-Down Event
IDPS shows much larger STD DEV
• AVHRR & MODIS SSTs are consistent• ACSPO VIIRS is consistent with MODIS & AVHRR • IDPS VIIRS EDR shows much larger STD DEV
L2/L3 SQUAM: Maps Histograms Time-series Dependencies
Hovmöller
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L2/L3 SQUAM: Maps Histograms Time-series Dependencies
HovmöllerPla
tform
sYear
Wind Speed (ms-1)
NOAA-17 mid-morning platform - Diurnal warming suppressed
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“OISST – CMC” mean zonal difference
Year
Latitude
More combinations at: http://www.star.nesdis.noaa.gov/sod/sst/squam/L4/
Diff. in ice mask
HL issues
L4 SQUAM: Maps Histograms Time-series Hovmöller
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Mean
Year
Std
Dev
Year
wrt drifters wrt drifters
DOI_AVDOI_AARTG_HRRTG_LRGOESPOESOSTIAOSTIA_RANCMC 0.2NAVO K10GAMSSAODYSSEAGMPEG1SSTMUR
Reynolds OISST (AVHRR)Reynolds OISST (+ AMSR-E)Real Time Global high resolutionRTG low resolutionBlended POES and GOESOperational SST and Sea ice analysisOSTIA Reanalysis (retro)Canadian Met. Centre 0.2 degreeNAVOCEANO 1/10 degreeMERSEA IFREMER/CERSATAustralian BOMGHRSST Median Ensemble ProductJPL 1km G1SSTJPL Multi scale ultra high res. SST
Roughly, L4 products form 3 major groups(when compared against GMPE):
DOI_AV, DOI_AA, RTG_LR, NAVO K10,
G1SST
RTG_HR, GOES-POES blended (with seasonal variation between: RTG_HR, RTG_LR)
OSTIA, CMC, GAMSSA & GMPE
Too many products busy .. Interactive plots available online
L4 SQUAM: Maps Histograms Time-series Hovmöller