SST from VIIRS on NPP: prelaunch preparations and post-launch validation Peter J Minnett & Robert H Evans Meteorology & Physical Oceanography Rosenstiel School of Marine and Atmospheric Science University of Miami Miami FL USA Outline • Description of VIIRS – Visible/Infrared Imager/Radiometer Suite • SST retrievals • Cal/Val approach All information about VIIRS is from publicly accessible sources. NASA SST Science Team Meeting Seattle, November 2010 NPP payload From http://modis.gsfc.nasa.gov/sci_team/meetings/201001/presentations/plenary/gleason.pdf NASA SST Science Team Meeting Seattle, November 2010 VIIRS • The Visible/Infrared Imager/Radiometer Suite collects visible/infrared imagery and radiometric data. • Applications include atmospheric clouds, earth radiation budget, clear-air land/water surfaces, sea surface temperature, ocean color, and low light visible imagery. • Primary instrument for satisfying 22 Environmental Data Records (EDRs) and 2 Key Performance Parameters (KPPs): Imagery & sea surface temperature. • Multiple VIS and IR channels between 0.3 and 14 μm • Imagery (I) Spatial Resolution: ~370m @ nadir / 750m @ edge of swath • Moderate (M) Spatial Resolution: ~740m @ nadir / 1500m @ edge of swath • Swath width ~3000km NASA SST Science Team Meeting Seattle, November 2010 VIIRS Components • • • • • Spectral Bands: – Visible/Near IR: 9 plus Day/Night Band – Mid-Wave IR: 8 – Long-Wave IR: 4 Imaging Optics: 18.4 cm Aperture, 114 cm Focal Length Band-to-Band Registration (All Bands, Entire Scan) > 80% per axis Orbital Average Power: 240 W Mass: 275 Kg NASA SST Science Team Meeting Seattle, November 2010 VIIRS innovations • • • • Rotating telescope primary optics Two-sided “Half-Angle Mirror” (HAM) Multiple detectors (16) per spectral band On-board pixel aggregation NASA SST Science Team Meeting Seattle, November 2010 VIIRS NASA SST Science Team Meeting Seattle, November 2010 Risk reduction by using components derived from heritage instruments: • Rotating Telescope from SeaWiFS • Black-body from MODIS • Multiple Focal Plane Arrays and Multiple Detector Assemblies from MODIS NASA SST Science Team Meeting Seattle, November 2010 NASA SST Science Team Meeting Seattle, November 2010 Pixel Aggregation • Each “pixel” has three rectangular detectors in the scan direction • Detectors have a 3x1 aspect ratio • These are aggregated in threes, then twos, then no aggregation, across the scan. • This is an attempt to provide near uniform spatial resolution across the swath. NASA SST Science Team Meeting Seattle, November 2010 VIIRS vs MODIS spatial resolution From http://www.ipo.noaa.gov/ams/2010/posters/AGU_AMS-RAY_NGASVIIRSHeritageSystems-SNODGRASS_GUENTHER_ANDREAS-WE_PRINT-PR.pdf NASA SST Science Team Meeting Seattle, November 2010 VIIRS SST Bands Spectral bands are a subset of MODIS bands GSD = Ground sampling distance These are very promising NASA SST Science Team Meeting Seattle, November 2010 VIIRS SST Uncertainty Estimates • The sources of error the VIIRS SSTs fall into two categories: – associated with imperfections in the instrument – arise from imperfections in the atmospheric correction algorithm. • The instrumental effects include: – The inherent noise in the detectors, the Noise Equivalent Temperature Difference (NEΔT) – Band-to-band registration (BBR) – Modulation Transfer Function (MTF) – Imperfections in the knowledge of angular dependence of the reflectivity of the “Half Angle Mirror” – Calibration errors, such as imperfections in the knowledge of the emissivity and surface temperature of the on-board black body target, and of stray radiation falling on the detectors. • Uncertainties will be established soon after launch using multiple techniques. NASA SST Science Team Meeting Seattle, November 2010 VIIRS SST algorithms Daytime NLSST algorithm: where a0, a1, a2, a3 are coefficients derived by regression analysis, T11 is the measured brightness temperature at 11 µm (VIIRS band M15), T12 is the measured brightness temperature at 12 µm (VIIRS band M16), RSST is a modeled, first guess SST, and z is the sensor zenith angle. Night-time NLSST algorithm: where a0, a1, a2, a3 are coefficients derived by regression analysis (but are different from those in Equation 12), T3.7 is the measured brightness temperature at 3.7 µm (VIIRS band M12). NASA SST Science Team Meeting Seattle, November 2010 Post launch validation The approach will be based on experience gained from AVHRR, (A)ATSR and MODIS, and will involve comparisons with: • Other validated satellite data sets (e.g. AVHRR, AATSR, MODIS…) • Drifting and moored buoys • Ship-based radiometers – M-AERI, M-AERI Mk2, ISAR….. NASA SST Science Team Meeting Seattle, November 2010 SST validation using ship-board radiometers Radiometers installed on ships for the validation of MODIS skin SSTs. Top: the ISAR mounted above the bridge of the M/V Jingu Maru. Middle: M-AERI mounted on the NOAA S Ronald H. Brown. Bottom: M-AERI mounted on an upper deck of the Explorer of the Seas. NASA SST Science Team Meeting Seattle, November 2010 M-AERI validation data M-AERI cruises since the launch of Terra used for the validation of MODIS skin SSTs NASA SST Science Team Meeting Seattle, November 2010 M-AERI Mk 2 NASA SST Science Team Meeting Seattle, November 2010 ISAR VOS cruises for SST validation Real-time transmission of data via Iridium, on-thefly validation is feasible. NASA SST Science Team Meeting Seattle, November 2010 19 SST radiometers - 2009 3rd Miami IR Radiometry Workshop Traceability to SI references is a prerequisite for CDRs 20 Validation with buoys Buoys provide many more opportunities of “matchups ” than radiometers. NASA SST Science Team Meeting Seattle, November 2010 GHRSST Diagnostic Data Set Location of the 250 HR-DDS global data comparison locations for SST in situ and satellite retrievals. NASA SST Science Team Meeting Seattle, November 2010 DDS time series Example of time series of DDS data including multiple satellite data, in situ measurements, NWP analysis fields and OI fields. This allows rapid comparison between VIIRS SSTs and other SSTs. NASA SST Science Team Meeting Seattle, November 2010 In situ data → LUT generation to product validation A Gather in situ 0 1 D Analyze Matchups → Quality Test Hypercube LUT G 2 Process VIIRS SDR → EDR, Diagnostics Analyze Diff wrt Reference, Time Series Hovmueller plots C Acquire, load SDR and reference field inputs Generate extraction files Quality control Buoy MAERI, ISAR Real time or retrospective Process SDR, Navigate → EDR, Matchup records B 1 F E Update L2gen with revised LUT and tables H 2 I Correct algorithm as necessary, update and reprocess 0 Current status at L-351 • • • • • • • • Instrument level T/V testing completed, and some optical cross-talk issues identified – but not expected to be dominant source of SST error Instruments integrated on NPP spacecraft at Ball Aerospace & undergoing testing Post-launch SST validation plans being set up: coordination between May (NAVOCEANO), Ignatov (NOAA –STAR), Emery (U. Colorado) & Evans – Minnett (U Miami) New validation sensors (M-AERI Mk2) being developed Real-time data transmission being tested Software being installed and tested, including match-ups “on the fly” Data streams being established and tested Anticipated validation data: – Satellite fields (MODIS, AVHRR, AATSR) – Buoys – Radiometers (2 M-AERIs; 2 M-AERI Mk2s, 2 ISARS) • Logical framework for feedback to improve retrievals being established NASA SST Science Team Meeting Seattle, November 2010 VIIRS & NPP NASA SST Science Team Meeting Seattle, November 2010 Summary • VIIRS has the potential to provide high quality SSTs. • Post launch validation will focus on comparison with: – Satellite SST fields – Buoys – Radiometers • Contribution to SST CDR requires validation with NIST-traceable radiometers – facilitated through Miami Infrared Radiometry Workshops. NASA SST Science Team Meeting Seattle, November 2010 • Additional slides in reserve NASA SST Science Team Meeting Seattle, November 2010 Major VIIRS Objectives • High resolution imagery with near constant resolution across scan • Increased resolution of SST retrievals • Disaster monitoring (Volcanic ash, Suspended Matter, Floods, Fires, …) • Increased accuracy/resolution of aerosols and cloud properties • Climate relevant accuracies…… NASA SST Science Team Meeting Seattle, November 2010 In situ and proxy data tasks A 1 A 2 In Situ Measurements MAERI In Situ Measurements ISAR A E 1 Matchup database RTE simulation I1 E NASA SST Science Team Meeting Seattle, November 2010 In Situ Measurements MAERI I Telescope / HAM Synchronization Angles Note – successive rotations of the Rotating Telescope Assembly use alternate sides of the HAM Spectral bands are a subset of MODIS bands Silicon PIN Diodes PV HgCdTe (HCT) PV HCT LWIR S/MWIR VIS/NIR FPA VIIRS Bands Band Wavelength (µm) M1 0.412 M2 0.445 M3 0.488 M4 0.555 I1 M5 0.640 0.672 M6 I2 M7 0.746 0.865 0.865 M8 M9 I3 M10 M11 M12 I4 M13 M14 M15 I5 M16 Driving EDRs Gain Lmax Ltyp or Range or Tmax Ttyp EOL Predicts, Nom Tolerance FU w/ MIB Fix, F/: 6.20 SNR @ Ltyp or NEDT(K) @ Ttyp SNR Margin Required Predicted (%) 352 434 23.3 316 717 126.6 380 419 10.3 409 702 71.5 416 562 35.1 414 739 78.6 362 480 32.6 315 685 117.1 119 164 37.6 242 294 21.4 360 549 52.5 199 320 60.7 150 251 67.1 215 462 114.9 340 525 54.5 BOL Predicts, Nom Tolerance FU w/ MIB Fix, F/: 6.20 SNR @ Ltyp or NEDT(K) @ Ttyp SNR Margin Required Predicted (%) 352 451 28.3 316 747 136.2 380 431 13.3 409 722 76.4 416 571 37.3 414 753 82.0 362 486 34.2 315 694 120.0 119 166 39.3 242 297 22.7 360 556 54.3 199 323 62.1 150 252 68.3 215 466 116.6 340 530 55.9 Ocean Color Aerosols Ocean Color Aerosols Ocean Color Aerosols Ocean Color Aerosols Imagery Ocean Color Aerosols Atmospheric Corr'n NDVI Ocean Color Aerosols High Low High Low High Low High Low Single High Low Single Single High Low 135.0 615.0 127.0 687.0 107.0 702.0 78.0 667.0 718.0 59.0 651.0 41.0 349.0 29.0 349.0 44.9 155.0 40.0 146.0 32.0 123.0 21.0 90.0 22.0 10.0 68.0 9.6 25.0 6.4 33.4 1.240 1.378 1.610 1.610 2.250 3.700 3.740 4.050 Cloud Partical Size Cirrus/Cloud Cover Binary Snow Map Snow Fraction Clouds SST Imagery Clouds SST Fires Single Single Single Single Single Single Single High Low 164.9 77.1 72.5 71.2 31.80 353 353 343 634 5.4 6.0 7.3 7.3 0.12 270 270 300 380 74 83 6 342 10 0.396 2.500 0.107 0.423 122 171 123 463 20 0.182 0.549 0.058 0.316 65.2 107.2 1956.7 35.3 95.4 117.4 355.5 85.3 33.8 74 83 6 342 10 0.396 2.500 0.107 0.423 122 171 123 463 20 0.182 0.549 0.058 0.316 65.2 107.2 1956.7 35.3 95.4 117.4 355.5 85.3 33.8 8.550 10.763 11.450 12.013 Cloud Top Properties SST Cloud Imagery SST Single Single Single Single 336 343 340 340 270 300 210 300 0.091 0.070 1.500 0.072 0.067 0.030 0.414 0.029 35.4 133.9 262.5 146.7 0.091 0.070 1.500 0.072 0.067 0.030 0.414 0.029 35.4 132.7 262.5 146.7 Noise Component Breakdown (single sample, no TDI or Aggregation) 1.0 0.9 NASA SST Science Team Meeting Seattle, November 2010 ISAR validation data Real-time transmission of data via Iridium, on-the-fly validation is feasible NASA SST Science Team Meeting Seattle, November 2010 Temperatures are traced to NIST 1. On-board black-body cavities have thermometers calibrated to NISTtraceable thermometers (SSEC) 2. Periodic calibration using a 3rd black body in M-AERI zenith view. 3. Periodic calibration of M-AERI system with a NIST-designed Water-Bath Black-Body target at RSMAS, using NIST-traceable reference thermometers. 4. RSMAS Water-Bath Black-Body target characterized with NIST EOS TXR NASA SST Science Team Meeting Seattle, November 2010 NIST EOS TXR TXR characterizing the RSMAS WBBB NIST water-bath black-body calibration target See: Fowler, J. B., 1995. A third generation water bath based blackbody source, J. Res. Natl. Inst. Stand. Technol., 100, 591-599 NASA SST Science Team Meeting Seattle, November 2010 36 M-AERI Cold finger, Dewar and detectors Aft optics Input aperture Stirling cycle cooler Interferometer NASA SST Science Team Meeting Seattle, November 2010 The innards NASA SST Science Team Meeting Seattle, November 2010 Wavelength calibration Wavelength calibration provided by a HeNe laser NASA SST Science Team Meeting Seattle, November 2010