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Published byTimothy Dolan Modified over 11 years ago
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New L2P and L3 at MF/CMS P.LeBorgne, F.Orain, A.Marsouin, H.Roquet MF/DP/CMS, Lannion
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New L2P L3 New L2P L3 in MERSEA From MERSEA to MyOcean
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Next L2P 2009: hourly SEVIRI and GOES L2?P (at present internal to CMS/MERSEA) GRIDDED or not?
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L3 at CMS: Present status in MERSEA Le Borgne et al, 2006, Mersea report Polar orbiters: -AATSR -NOAA-17 -NOAA-18 -AMSRE -TMI Geostationary: -GOES-E -SEVIRI Analysis (L4) Other users? Data available in real time through MERSEA (ftp IFREMER) Synthesis + Correction L3
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Method (overview) Sensor i 1)Collection 2)Remapping 3)Synthesis over time 4)Correction Merging L3 (i), unique per sensor L3 (merged) Zone (Atl., global,..) + time window (1day, 3 days,…) Principles: -Synthesize information -Best quality -Traceability at pixel level: Origin (which sensor) Original lat lon Confidence level SSES Applied correction (if any)
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Method : Correction 1) Sensor-AATSR Over the last ~10 days 2) Alalysis of the differences On a 5° grid 3) Interpolation To fine resolution: Correction of the day
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Method : Merging A priori hierarchy of sensors traceability
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L3: validation overview ……… L2PsAATSR L2PsBuoys..MSG L2PsNOAA-17 L2Ps AATSR L3Buoys L3NOAA-17 L3……… L3..MSG L3 UNCORRECTED Merged L3 AATSR L3Buoys L3NOAA-17 L3……… L3..MSG L3 CORRECTED validationcomparisoncorrectioncomparisoncontrolvalidation
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L3: validation results over the Atlantic Validation Control Routine production since 01/01/07
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L3: validation results Comparison with AVHRR18_G Inter Comparison of OSI-SAF products
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L3: correction validation results SEVIRI-AATSR as a function of time and latitude before correction
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L3: correction validation results SEVIRI-ATSR as a function of time and latitude after correction
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From MERSEA … CMS MERSEA database (francoise.orain@meteo.fr) –Available in real time trough the MERSEA ftp site at IFREMER –One year completed by March 2008, –Daily collated for: Polar orbiters: -AATSR -NOAA-17 -NOAA-18 -AMSRE -TMI Geostationary: -GOES-E -SEVIRI Buoys
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…to Myocean MyOcean –Addition of METOP and MODIS SST –Collated down to 0.02 degree resolution –Over the European seas –For fine resolution analysis
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Conclusion Correction with AATSR shows satisfying results in MERSEA Limitations: –Cloud cover ? –Limited swath –Assumptions: large scale (several degrees)/ slowly varying (several days) errors: not right everywhere Do need R&D effort One full year database available next March MyOcean: prototype in construction
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