Introduction to ST-VAL Gary Corlett. ST-VAL The ST_VAL TAG objectives are to – Establish and promote guidelines for satellite SST validation Coordinate.

Slides:



Advertisements
Similar presentations
Use of VOS data in Climate Products Elizabeth Kent and Scott Woodruff National Oceanography Centre, Southampton NOAA Earth System Research Laboratory.
Advertisements

Meteorological Observatory Lindenberg – Richard Assmann Observatory The GCOS Reference Upper Air Network.
Earth Observation Science The ATSR Series, the SST Climate Record and Relevant Validation Programmes for the Future David Llewellyn-Jones.
GHRSST XI Science Team Meeting, ST-VAL, June 2010, Lima, Peru Recent developments to the SST Quality Monitor (SQUAM) and SST validation with In situ.
WMOIOC 1 OOPC-XII, Paris, 2-5 May 2007 DBCP issues for OOPC Boram Lee IOC Secretariat for JCOMM.
Uncertainty estimates in input (Rrs) and output ocean color data: a brief review Stéphane Maritorena – ERI/UCSB.
Earth Observation Science Some Considerations concerning the Physical basis of SST Measurements David Llewellyn-Jones AATSR Principal.
Sandra Castro, Gary Wick, Peter Minnett, Andrew Jessup & Bill Emery.
Long-term radiometric validation of the ATSR SST record using the M-AERI Gary Corlett, David Llewellyn-Jones University of Leicester and Peter Minnett.
Aquarius/SAC-D Mission Validation Working Group Summary Gary Lagerloef 6 th Science Meeting; Seattle, WA, USA July 2010.
Characterizing and comparison of uncertainty in the AVHRR Pathfinder SST field, Versions 5 & 6 Robert Evans Guilllermo Podesta’ RSMAS Nov 8, 2010 with.
Calibration/Validation and Generating Sea- Surface Temperature Climate Data Records: An approach using ship-board radiometry Peter Minnett 1, Gary Corlett.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 NOAA Operational Geostationary Sea Surface Temperature Products from NOAA.
Improved NCEP SST Analysis
1 Overview LTSRF Status GHRSST Reanalysis Example L4 Analyses Future Activities Beijing, October 2006 The GODAE High Resolution.
Determining the accuracy of MODIS Sea- Surface Temperatures – an Essential Climate Variable Peter J. Minnett & Robert H. Evans Meteorology and Physical.
Meteorological Observatory Lindenberg – Richard Assmann Observatory The GCOS Reference Upper Air Network.
MISST FY1 team meeting April 5-6, Miami, FL NOAA: Gary Wick, Eric Bayler, Ken Casey, Andy Harris, Tim Mavor Navy: Bruce Mckenzie, Charlie Barron NASA:
CEOS SST-VC- Status and Issues Craig Donlon and Kenneth S. Casey on behalf of the SST-VC members ESA and NOAA CEOS SIT-29 Meeting CNES, Toulouse, France.
MODIS Sea-Surface Temperatures for GHRSST-PP Robert H. Evans & Peter J. Minnett Otis Brown, Erica Key, Goshka Szczodrak, Kay Kilpatrick, Warner Baringer,
Inter-comparison and Validation Task Team Breakout discussion.
ECOOP-WP3 Better use of remote-sensing data and in situ measurements Francis Gohin, Ifremer T3.1 Optimal synergy between altimetry and tide gauge data.
AN ENHANCED SST COMPOSITE FOR WEATHER FORECASTING AND REGIONAL CLIMATE STUDIES Gary Jedlovec 1, Jorge Vazquez 2, and Ed Armstrong 2 1NASA/MSFC Earth Science.
Page 1© Crown copyright HadISST2: progress and plans Nick Rayner, 14 th March 2007.
DMI-OI analysis in the Arctic DMI-OI processing scheme or Arctic Arctic bias correction method Arctic L4 Reanalysis Biases (AATSR – Pathfinder) Validation.
1 Agenda Review Issues Melbourne, May 2007 Kenneth S. Casey NOAA National Oceanographic Data Center May 2007 Gary Wick, Rapporteur GHRSST-8 Session-8 Reanalysis.
Application of in situ Observations to Current Satellite-Derived Sea Surface Temperature Products Gary A. Wick NOAA Earth System Research Laboratory With.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 In Situ SST for Satellite Cal/Val and Quality Control Alexander Ignatov.
Page 1 Validation Workshop, 9-13 th December 2002, ESRIN ENVISAT Validation Workshop AATSR Report Marianne Edwards Space Research Centre Department of.
AQUA AMSR-E MODIS POES AVHRR TRMM TMI ENVISAT AATSR GOES Imager Multi-sensor Improved SST (MISST) for GODAE Part I: Chelle Gentemann, Gary Wick Part II:
1 Overview LTSRF Status GHRSST Reanalysis Example L4 Analyses Future Activities D.C., Nov 2006 Long Term Stewardship and Reanalysis.
Infrared and Microwave Remote Sensing of Sea Surface Temperature Gary A. Wick NOAA Environmental Technology Laboratory January 14, 2004.
BLUElink> Regional High-Resolution SST Analysis System – Verification and Inter-Comparison Helen Beggs Ocean & Marine Forecasting Group, BMRC, Bureau of.
Andrea Kaiser-Weiss, Melbourne Joint GHRSST Workshop, 6 th March 2012 Experiences with SST profiles from near-surface Argo measurements A. Kaiser-Weiss.
STVAL Report Gary Corlett. Introduction At the 9 th GHRSST Science Team meeting, a proposal was put forward to join together the SSES-WG and the VAL-TAG.
The MODIS SST hypercube is a multi-dimensional look up table of SST retrieval uncertainty, bias and standard deviation, determined from comprehensive analysis.
AQUA AMSR-E MODIS POES AVHRR TRMM TMI ENVISAT AATSR GOES Imager Multi-sensor Improved SST (MISST) for GODAE Part I: Chelle Gentemann, Gary Wick Part II:
Diurnal Variability Working Group: GHRSST-10 Breakout Session Report Chris Merchant Gary Wick.
A comparison of AMSR-E and AATSR SST time-series A preliminary investigation into the effects of using cloud-cleared SST data as opposed to all-sky SST.
QA4EO in 10 Minutes! A presentation to the 10 th GHRSST Science Team Meeting.
Use of high resolution global SST data in operational analysis and assimilation systems at the UK Met Office. Matt Martin, John Stark,
International GHRSST User Symposium Santa Rosa, California, USA 28-29th May 2009 MODIS Sea-Surface Temperatures Peter J Minnett & Robert H. Evans With.
1 March 2011iQuam GHRSST DV-WG, HL-TAG and ST-VAL Meeting 28 February – 2 March 2011, Boulder, CO In situ Quality Monitor (iQuam) Near-real time.
Characterizing and comparison of uncertainty in the AVHRR Pathfinder Versions 5 & 6 SST field to various reference fields Robert Evans Guilllermo Podesta’
Uncertainty estimation from first principles: The future of SSES? Gary Corlett (University of Leicester) Chris Merchant (University of Edinburgh)
New Australian High Resolution AVHRR SST Products from the Integrated Marine Observing System Presented at the GHRSST Users Symposium, Santa Rosa, USA,
ST-VAL Breakout Summary Gary Corlett. ST-VAL Breakout 16:20 Introduction and objectives for session (G Corlett) 16:30 The Data Buoy Co-operation Panel.
Sandra Castro and Gary Wick.  Does direct regression of satellite infrared brightness temperatures to observed in situ skin temperatures result in.
ATSR Re-analysis for Climate (ARC) Chris Merchant The University of Edinburgh.
Establishing by the laboratory of the functional requirements for uncertainty of measurements of each examination procedure Ioannis Sitaras.
Report from breakout session in the High Latitude Working group Prepared by Jacob L. Høyer, Bob Grumbine and Steinar Eastwood.
The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology Systematic biases in satellite SST observations.
L3 PLB May L2 Pre-ProcessedL3 Pre processedL3 (collated)Analysed SST AcronymL2PL3PL3L4 DescriptionNative SST data streams reformatted into netCDF.
Earth Observation Science CEOS Guidelines for the validation of satellite SST Observations David T Llewellyn-Jones &Gary K Corlett Space Research Centre.
Diurnal Variability Analysis for GHRSST products Chris Merchant and DVWG.
Summary of the GHRSST Joint Workshop Melbourne discussion on the Argo near- surface temperature measurements Andrea Kaiser-Weiss, Gary Wick, Carol-Anne.
GHRSST interest in upgraded drifters - Summary from the GHRSST Joint Workshop Melbourne Andrea Kaiser-Weiss, Gary Corlett, Chris Merchant, Piere LeBorgne,
GHRSST 10: Report from Diurnal Variability Working Group Report on activities of the Diurnal Variability Working Group Chris Merchant University of Edinburgh.
May 28-29, 2009GHRSST 2009 International Users Symposium National Oceanic and Atmospheric Administration Group for High Resolution Sea Surface Temperature.
Validation of MTSAT-1R SST for the TWP+ Experiment Leon Majewski 1, Jon Mittaz 2, George Kruger 1,3, Helen Beggs 3, Andy Harris 2, Sandra Castro 4 1 Observations.
SeaDataNet Technical Task Group meeting JRA1 Standards Development Task 1.2 Common Data Management Protocol (for dissemination to all NODCs and JRA3) Data.
Calculation of Sea Surface Temperature Forward Radiative Transfer Model Approach Alec Bogdanoff, Florida State University Carol Anne Clayson and Brent.
Validation status overivew
NOAA Report on Ocean Parameters - SST Presented to CGMS-43 Working Group 2 session, agenda item 9 Author: Sasha Ignatov.
Validation status overivew
Argo Delayed-Mode Salinity Data
Validation of Satellite-derived Lake Surface Temperatures
The SST CCI: Scientific Approaches
Tim Hewison1 (1) EUMETSAT
Committee on Earth Observation Satellites
Presentation transcript:

Introduction to ST-VAL Gary Corlett

ST-VAL The ST_VAL TAG objectives are to – Establish and promote guidelines for satellite SST validation Coordinate discussions on validation techniques Draft a set of common guidelines – Objectively examine GHRSST-PP L2P data and to provide meaningful SSES for users Coordinate and homogenize the quality information in L2P between producersThe

Activities within STVAL The STVAL group’s activities are split into three areas: 1.Validation using in situ thermometry, including QC of in situ data Guidelines for producing match-ups (generation of MDB) Production of SSES Agree common guidelines for SSES 2.Validation using in situ radiometry, including Calibration traceability to standards Guidelines for producing match-ups Inter-comparisons 3.Validation using reference satellite sensor, including QC of reference sensor Methodologies

Directions for remotely sensed SST Away from empirical, towards physics-based Away from coefficients, towards formal inversion Sophisticated cloud detection and treatment of aerosols Resolve (in time) sub-daily variability (diurnal cycle) Decreasing uncertainties in satellite SST estimates - SD and regional bias Increasing scrutiny of drifting buoy and other in situ SSTs

Reference datasets for satellite SST validation Ship-borne radiometers – Traceable to SI; SST-skin; high accuracy; very-poor coverage Argo 3-5 m – Global; acceptable sampling; very-high accuracy (calibration method to be analysed) Drifting buoys – Unknown calibration; global data; SST-depth; good (but variable coverage) GTMBA – Better calibration; SST-1m; acceptable coverage (influenced by data collection) Coastal moorings – Questionable uncertainty; tough areas to validate VOS and VOSclim – Generally poor coverage; very high uncertainty on single sample

Relative errors of satellites and drifting buoy SST AATSR D3 SSTs are the “best” satellite SSTs available and are ±0.13 K (O’Carroll et al.) AVHRR split window will soon give ±0.22 K operationally at M-F (Merchant et al.) Drifting buoys (after QC or using robust statistics) seem to give ±0.2 K “Received wisdom”: buoy thermistors should give ±0.1 K “off the shelf” – Optimistic? Beginning-of-life value? – Rounding to 0.1 K – Point measured at depth being used for 1 km pixel Contribution from geophysical variability? Would we see any difference if buoy calibration were improved?

Interaction with in situ providers Recommendations to DBCP – Now deploying drifters with improved reporting – Project.html Project.html – Now looking at calibration JCOMM SOT – Interact on future requirements – Action to provide validation results as a function of measurement type Argo – Request for un-pumped near-surface profiles

Issues to be addressed How to deal with the SST skin to SST depth Need to deal with time difference Agreed mean drifter depth Which statistics to report Alternate SSES using Level 1b and retrieval uncertainties The evaluation of Argo as a reference source A long-term reference dataset for validation of L2 and higher products

Which Statistics? AATSR V2.0 D3 retrievals versus drifting buoys Normal – Mean:-0.09 K – St.Dev.:0.49 K 3-sigma – Mean:-0.09 K – St. Dev.:0.35 K Robust – Median:-0.08 K – Rob.Sig.:0.33 K Gaussian fit – Mean:-0.07 K – St.Dev.:0.27 K

AATSR v2.0 Skin effect

To skin or not to skin… All IR radiometers are sensitive to the skin SST – Even if retrieval provides sub-skin! Common agreement for skin to sub-skin (buoy depth) adjustment needed – 0.2 K; 0.17 K; 6 ms-1; Craig’s model; etc… – Agreement to ignore DV for SSES

GDS 2.0 SSES (1) Interoperability of many GHRSST data sources provides optimum scientific return Requires uniform method for uncertainty estimation across all data sources Common principles for SSES agreed at GHRSST X and revised at GHRSST XI – Will be maintained on GHRSST website and NOT in GDS 2.0 documentation

GDS 2.0 SSES (2) SSES must – Comprise bias and standard deviation relative to agreed reference source Quality indicator following QA4EO guidelines – Supported by a quality level flag – Be defined according to the SSES Common Principles Maintained on GHRSST website – Be documented and traceable Maintained on GHRSST website

GDS 2.0 SSES (3) SSTs should be the best estimate prior to SSES production – Responsibility of the SST producer – SSES are for users NOT for producers Common scale for quality level – Scale of 2 (worst quality) to 5 (best quality) – Clearly defined for each producer – Derivation of quality indicator to be traceable, i.e. documented and available to users.

SSES Common Principles (1) Content: – A bias (not a correction term) and a standard deviation reflecting the local accuracy (ideally at pixel) of the SST estimate – Application of SSES is consistent with the product definition (skin; sub-skin) At present the reference is drifting buoys – By convention (only really global source)

SSES Common Principles (2) Hierarchical references can be used – Global stats to DRIFTING BUOYS – Regional stats using other reference sources Radiometers GTMBA L4 analyses – PMW only Use of common match-up thresholds – Centre pixel clear; +/- 2 hrs (ideally 30 mins)

SSES Common Principles (3) Continuous fields preferred – No discontinuities between Quality Levels – Discontinuities may be inevitable SSES must be free from diurnal variability – Ideally estimated from night time match-ups L2P producers that provide SST-skin should use, as a minimum, a constant offset of 0.17 K to adjust SST- skin to SST-sub-skin for SSES production. – If sufficiently accurate wind-speed data is available then L2P producers are encouraged to allow for the wind speed dependence of the skin to sub-skin adjustment.

SSES Progress Good progress is being made towards providing uniform SSES across all IR products – Based on presentations in Lima Some incompatibilities with the SSES common principles remain across most products. – Diurnal variability; match-up limits Further iterations and refinements are being sought.

Actions Pierre Le Borgne – To add Bob Evans, Nick Rayner, Dick Reynolds and Gary Wick to the MF buoy blacklist mailing list Bob Evans – To provide details of extra QC steps done to buoy data prior to ingestion into MODIS MDB.

Tasks The exchange of buoy black lists between groups An investigation into the impact of varying QC approaches Separate NRT activities/requirements from offline/CDR requirements. Include moored buoys to QC procedures Assess current buoy coverage and identify areas where additional data are needed for SSES. Consult widely with buoy providers to identify non- GTS historical buoy data, starting with latest ICOADS release.

Tasks Continued refinement and adoption of the SSES common principles Provision of documentation for the website and user manual Peer-review of SSES schemes

Documentation Still an issue – Some schemes have no documentation at all Need to provide guidance for users – For website and user manual SSES schemes should ideally be peer-reviewed

Breakout activities L2P producers: brief summary of SSES scheme for user manual and website – Derivation, application, limitations, examples etc. Future validation – What is required? Multi-sensor match-ups – Benefits for uncertainty estimation The issues list, current SSES approach Any others?