1 / 10

ODYSSEA In Arctic

ODYSSEA In Arctic. Emmanuelle Autret, Jean-François Piollé IFREMER/CERSAT, 29280 Plouzané, France Emmanuelle.Autret@ifremer.fr jfpiolle@ifremer.fr. Outline. Method Input validation in Arctic L3S, L4 validation Conclusion. Method (1). GHRSST L2P products.

obert
Download Presentation

ODYSSEA In Arctic

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. ODYSSEA In Arctic Emmanuelle Autret, Jean-François Piollé IFREMER/CERSAT, 29280 Plouzané, France Emmanuelle.Autret@ifremer.fr jfpiolle@ifremer.fr

  2. Outline • Method • Input validation in Arctic • L3S, L4 validation • Conclusion

  3. Method (1) GHRSST L2P products Observation quality control, correction (sses), filtering « re-mapped » L3 products Selection based on proximity to analysis time and best quality « collated monosenso L3C products » (/day /sensor) Pre- processing steps Correction of large scale bias field for each sensor (daily reference: 0.25 gridded field) Intercalibrated collated products (/day /sensor) Merging of composite files « multisensor supercollated L3S products » (/day) Optimal interpolation Multi-sensor analysed field

  4. Method (2) • Bias correction principles: • A daily 0.25° resolution L3 «reference field » is built every day as follows: • 1) Each source is remapped on the 0.25° grid (mean): • 2) A median of selected sensor data is kept at each grid point • 3) An OI is applied to get a complete reference field • 4) The error (correction) is determined as the difference between each sensor and the reference smoothed over 2°.

  5. Ingested Data

  6. AATSR Validation (Arctic) North of 67 N Nighttime drifter measurements only

  7. NOAA-19 Validation (Arctic) North of 67 N Nighttime drifter measurements only

  8. L3S & analysis Validation (Arctic) North of 67 N Nighttime drifter measurements only

  9. Analysis Validation North of 67 N Nighttime drifter measurements only

  10. Conclusion • ODYSSEA uses a multisensor reference • ODYSSEA showed no bias in 2011 • Since then, ODYSSEA shows a seasonal bias: null in Autumn and significantly negative (-0.5K) in February. • bias correction is not efficient in the Arctic • all main sensors show a negative bias

More Related