Transfer of AVHRR SST Pathfinder to NODC to sustain long term production, distribution and archiving Sept 8, 2010 CICS PI Robert Evans, RSMAS/U Miami 305-421-4799,

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Presentation transcript:

Transfer of AVHRR SST Pathfinder to NODC to sustain long term production, distribution and archiving Sept 8, 2010 CICS PI Robert Evans, RSMAS/U Miami , Ken Casey, NODC ext Viva Banzon, NCDC SST CDR Lead ,

What is Pathfinder Daily global SST fields, resolution 4.63km for all of AVHRR 5 channel instruments – N7 to N18; (N19 and Metop future) using consistent calibration and processing methodology. Path group : SDS funded – University of Miami, and NOAA NODC with NCDC collaboration (R. Reynolds). Related activities and support: NASA MEASURES - URI, MIAMI, NODC addition of production and distribution of 1km AVHRR GHRSST, consistent file format, uncertainty reporting

Background CDR – Length, Stability, Accuracy error budget Consistent processing across multiple sensors – Noaa-7 through Noaa-18 (future support for N19, METOP) Full time series reprocessing for each update of algorithm, data quality tests,… Match-up Data base – Sat observations, in situ, ancillary fields (e.g. wind speed, ozone, aerosols, water vapor…) [with P. Minnett] Improved spatial resolution: – 18 -> 9 -> 4km global fields, 1km for LAC/HRPT Improved navigation (on-board clock resets, attitude correction) Improved Ancillary fields, e.g. Reference fields: – From Reynolds 1 o, weekly AVHRR+InSitu – To Reynolds ¼ o, daily V2 with Pathfinder, AMSR, InSitu Pathfinder SST products being integrated into international GHRSST file format– Group (for) High Resolution Sea Surface Temperature Pathfinder Application – order users/month and volume of gigabytes of Pathfinder fields delivered/month ( ) [per K. Casey, NODC]

V5 Path – HadSST2 (night) 5.1 for N7 Operational AVHRR – HadSST2 (night) V5 Path – HadSST2 (day) Operational AVHRR – HadSST2 (day) +N7 +N9 +N11 +N9+N14 +N16+N18 Pathfinder–HADSST2 residuals for 1982 through 2007, provided by Casey and Brandon, NODC

Processing Transfer to NODC SST production software – Level 0/1 through product maps (local and global). Matchup database – Contemporaneous, co- located AVHRR, in situ observations. Methodology for determination of SST equation coefficients. Linux cluster processing environment control scripts.

Pathfinder Process Flow Matchup Database -> Algorithm Coefficient Determination. Quality control -> Test SST retrievals vs in situ. Daily processing for near real time. Track Pathfinder accuracy versus available satellite and L4 analysis products. Update algorithms as needed, e.g. algorithm improvements, calibration updates, ancillary data fields (SST reference field, ice mask). When sufficient improvement is achieved, reprocess historical AVHRR global data.

The SST hypercube (for MODIS, AVHRR and VIIRS) is a multi- dimensional look up table of SST retrieval uncertainty, bias and standard deviation, determined from comprehensive analysis of the MODIS, AVHRR, VIIRS Match-up Data Bases (MDB). The MDB includes contemporaneous, co-located satellite brightness temperature, in-situ buoy and radiometer SST, environmental ‘observations’ from analyzed model or satellite observed fields, satellite viewing geometry, time and location. A series of quality tests is applied to each pixel during processing of the MDB data to identify cloud and dust aerosol contaminated retrievals and assign each pixel to one of several quality levels (0-4 MODIS, VIIRS, 0-8 AVHRR). GHRSST expands the SST processing to include Time and Error fields for each pixel (Mean and S.D.)

Version 6 Pathfinder Improvements Minimize High Latitude Seasonal Oscillation. Approach [LATBAND]: – Estimate Coefficients using 20 o zonal bands centered at the Equator, ± 2.5 o transition between bands – Coefficients estimated monthly and repeat for each year for a given sensor (volcano periods to be handled separately) – Reference SST – Reynolds ¼ o, daily Uses AVHRR, AMSR, Pathfinder and In situ observations Retains high gradient regions in Pathfinder fields New algorithms are first developed and tested for MODIS (improved sensor characterization and more stable operating environment). LATBAND algorithms have been transitioned to AVHRR. LATBAND Layout 40-90°N 20-40°N 0-20°N 20-0°S 40-20°S 90-40°S

Pathfinder V5 and the GCOS SST Intercomparison Facility Project goals: To understand differences between SST analyses and reconstructions with the aim of 1. producing better, long-term SST climate data records, and 2. linking the modern satellite-based records with the historical, primarily in situ-based records. Facility is hosted by NODC and includes 11 products from the international SST community The Pathfinder climatology is used as the common climatology against which all satellite-era SST products in the facility are evaluated, using a set of standard diagnostics, cross-product climatology analyses are also available Intercomparisons have been used to explore specific differences between analyses, e.g. the persistent cold-bias in Pathfinder (see figure below), PV5

Application of LATBAND to NOAA-18 Median of SST residuals (VALIDATION set) by quarter ( ). Each line corresponds to a latitude band. Upper panel corresponds to latitude-specific SST; lower panel is previous SST (CSST). Note high latitude seasonal oscillations Latband implementation removes seasonal residual oscillations Summary statistics for SST residuals, NOAA-18. (11-12μm bands) Pathfinder Algorithm Median Mean StdDev Validation LATBAND (skin) ValidationPathfinder V Pathfinder Version 6 - LATBAND Pathfinder Version 5

Pathfinder – Reynolds V2 OI, ¼ deg, daily, NOAA Night Pathfinder Version 5 monthly coefficients Pathfinder Version 6 LATBAND annual repeating monthly coefficients Both equatorial cold band and mid-latitude warm bands show smaller deviations from Reynolds OI in Pathfinder Version 6 than is seen in Pathfinder Version 5. All processing elements, cloud flagging are the same for the comparisons

Pathfinder Version 6 New algorithm approach (LATBAND) has resulted in a significant reduction of uncertainty in IR satellite SST retrievals. RMS reduced from 0.5 to <0.4 for 11, 12μm band retrievals. LATBAND algorithm approach has been implemented for VIIRS. AVHRR, MODIS and VIIRS satellite observations will be available through community accessible SEADAS programs.

Capabilities added for Pathfinder V6 beyond original proposal in conjunction with K Casey, NODC and P Cornillon, URI Skin SST. Use Reynolds V2 as the reference SST field. Use LATBAND – will need to develop SST coefficients for all NOAA sensors. Uncertainty hypercubes (per sensor), – N7, N9, N11, N12, N14, N15, N16, N17, N18 (9 sets) – Future for N19, METOP. Comparison of Pathfinder V5 and V6 wrt: – Reynolds OI+AVHRR; AVHRR+AMSR [day+night], AVHRR+AMSR [night only] – AMSR3 day average – AATSR monthly average

Path V6 continued SEADAS code base is being used to support MODIS and has been modified to support AVHRR Pathfinder, will facilitate distribution to interested users and algorithm transparency to the community. MODIS LATBAND code recently delivered to GSFC for incorporation into SEADAS. Add GHRSST format output files including hypercube. L2GEN Pathfinder (SEADAS) has been delivered to Ken Casey, has been integrated into current GSFC L2GEN version SeaDAS 6.1. Tested on N16, 17, 18. LATBAND for NOAA sensors has been integrated.

Accomplishments to date Version 1 GAC generation delivered to NODC and tested on one year of data. Clock corrections for early AVHRR instruments, generated. Attitude correction adjustments for 1km processing converted to LINUX. Precision navigation for LAC/GAC tested. Level 3 binning demonstrated. Mapping demonstrated.

Accomplishments, continued Using NOAA-18 data as testbed, processed: – Full day and night granules for a ‘data-day’ – Determined granule sections that constitute complete day and night files – Binned day and night granules into complete files – Mapped equal area files into standard map projection Implemented LINUX cluster processing – Developed processing control scripts – Run N multiple times for validation vs. multiple reference fields – Processing time for 1 year of global GAC is order 75 minutes

Elements for a follow-on proposal Develop ‘SCRIPPS’ L0 ingest capability to read L0 telemetry files. Generate SST retrieval coefficients and uncertainty hypercubes for all AVHRR 5 channel sensors. Add N19 and METOP-A. Validate LAC and GAC processing for all supported sensors. Introduce improved sensor calibration (Harris and Mittaz). Add SeaDAS/L2gen satellite-in situ matchup data extraction. Introduce and transfer unified SST Coefficient estimation code. Improve LATBAND by using 11-12um determined boundaries (Pathfinder 7).

END June – Noaa18 - Cloud filtered – Night – 4Km

Conclusions New algorithm approaches (Latband) has resulted in a significant reduction of uncertainty in IR satellite SST retrievals RMS reduced from 0.5 to <0.4 for 11μm band retrievals Future implementation of 3 band algorithm for MODIS and VIIRS suggests that cold fringes around clouds and aerosols can be detected and correction in these conditions is significantly improved. Latband and 3 band algorithm approaches will be implemented for VIIRS. AVHRR, MODIS and VIIRS satellite observations will be available through community accessible SEADAS programs. Pathfinder processing is being transferred to NODC to ensure continued availability of the multi-decade Pathfinder SST time series.

Comments “Scientifically irrefutable” – there is no such thing “Sensor Use” maturity falls outside scope of any individual product project, so it not something that a PI or product team can realistically strive for… …“Unified and coherent record demonstrated across different sensors” presumes a unifying framework exists. Such a framework exists only for SST (GHRSST), though other communities are beginning to organize. So – parts of this matrix as currently worded are really more of an evaluation of the international community framework, not of a given product’s contribution to it. Recommend changes to text to reflect this idea… for example, change “All relevant research and operational missions; unified and coherent record demonstrated across different sensors” to “Contributes to unified and coherent multi-sensor record based on all relevant research and operational missions” Documentation – no mention of web pages, user manuals, or user services support staff? Unclear about ATDB “vs” peer reviewed descriptions… what if you have peer reviewed papers describing the algorithm, products, etc., but no ATDB?

Application of LATBAND to MODIS AQUA Median of SST residuals (VALIDATION set) by quarter ( ). Each line corresponds to a latitude band. Upper panel corresponds to latitude-specific SST; lower panel is previous SST (CSST). MODIS algorithm produces a ‘skin temperature’ product Note high latitude seasonal oscillations Latband implementation removes seasonal residual oscillations

First global image from SEADAS/LINUX processing AVHRR N18 MODIS AQUA Images are NOT filtered for clouds

Second year, continued Execute pole-finding and granule separating functions. Incrementally transfer processing elements to NODC as they are validated. Implement Pathfinder V6 changes as they become available: – Latband coefficients – Reynolds 1/4°, daily OI – Update Ice mask Process selected portions of the AVHRR record at Miami and NODC and compare.

Second year, continued Begin computation of AVHRR Latband algorithm coefficients. Volcano periods will require additional attention. Update output format to match GHRSST specification. (MEASURES) Add ingest capability for URI legacy 1km input files. (MEASURES)

Third year Complete computation of LATBAND algorithm coefficients. Transfer Match-up database. Transfer of AVHRR LATBAND coefficient estimation process. NODC adds functionality to incorporate additional GHRSST required data fields, metadata. Support ongoing Pathfinder activities at NODC. Update to Pathfinder Version 6, process AVHRR time series: – GAC (SDS funding) NODC – LAC (MEASURES funding) URI

Pf5a0 night Pf6a0 night

END

PATHFINDER SEA SURFACE TEMPERATURE PRODUCT MATURITY VERSION 5 TO VERSION 6 Estimate of current V5 maturity indicated by BLUE (today) outline, future V6 Maturity by GREEN (completion of SDS activity) outline

MaturitySensor Use Algorithm Stability Metadata and QADocumentationValidationPublic Release Science and Applications 1Research Mission Significant changes likely IncompleteDraft ATBDMinimal Limited data availability to develop familiarity Little or none 2Research Mission Some changes expected Research grade (extensive) ATBD Version 1+ Uncertainty estimated for select locations/times Data available but of unknown accuracy; caveats required for use Limited or ongoing 3Research Mission Minimal changes expected Research grade (extensive); Meets International standards Public ATBD; Peer- reviewed algorithm and product descriptions Uncertainty estimated over widely distributed times/ locations by multiple investigators; Differences understood Data available but of unknown accuracy; caveats required for use Provisionally used in applications and assessments demonstrating positive value 4Operational Mission Minimal changes expected Stable, Allows provenance tracking and reproducibility; Meets international standards Public ATBD; Draft Operational Algorithm Description (OAD); Peer reviewed algorithm and product descriptions Uncertainty estimated over widely distributed times/ locations by multiple investigators; Differences understood Data available but of unknown accuracy; caveats required for use Provisionally used in applications and assessments demonstrating positive value 5 All relevant research and operational missions; unified and coherent record demonstrated across different sensors Stable and reproducible Stable, Allows provenance tracking and reproducibility; Meeting international standards Public ATBD, Operational Algorithm Description (OAD) and Validation Plan; Peer-reviewed algorithm, product and validation articles Consistent uncertainties estimated over most environmental conditions by multiple investigators Multi-mission record is publicly available with associated uncertainty estimate Used in various published applications and assessments by different investigators 6 All relevant research and operational missions; unified and coherent record over complete series; record is considered scientifically irrefutable following extensive scrutiny Stable and reproducible; homogeneous and published error budget Stable, Allows provenance tracking and reproducibility; Meeting international standards Product, algorithm, validation, processing and metadata described in peer reviewed literature Observation strategy designed to reveal systematic errors through independent cross-checks, open inspection, and continuous interrogation Multi-mission record is publicly available from Long-Term archive Used in various published applications and assessments by different investigators

Pathfinder Program Flow Ingest GAC, LAC L1b, L0 (telemetry) Geo-location Clock Correction Attitude Correction L1 -> L2 Conversion SST+Quality Find poles Day/night Split into processing segments SpaceBin Swath to Earth located Equal area-4km TimeBin Collect SpaceBin Files into day/night Orbit segments Load input: AVHRR ancillary TimeBin Collect Orbit Segments into Day files TimeBin Collect Day into Weekly or Longer files Determine DataDay Limits PathSpace Lower resolution 25km, 36km, 1deg Map Standard Projections Distribution File cleanup Define processing sequence Data Type (GAC,LAC) Processing Setup Granule Processing ~ 100 minutes of satellite observations Granule Collection Proceed to Next day

Pathfinder – Reynolds V2 OI, ¼ deg, daily, NOAA Day Pathfinder Version 5 monthly coefficients Pathfinder Version 6 LATBAND annual repeating monthly coefficients Both equatorial cold band and mid-latitude warm bands show smaller deviations from Reynolds OI in Pathfinder Version 6 than is seen in Pathfinder Version 5. All processing elements, cloud flagging are the same for the comparisons.