1 / 9

Continuation of ADRICOSM forecasting activities

Continuation of ADRICOSM forecasting activities. Paolo Oddo (INGV) National Institute of Geophysics and Volcanology Istituto Nazionale di Geofisica e Vulcanologia. OUTLINE. The ADRICOSM operational system Recent improvements New results and validation Conclusion.

inari
Download Presentation

Continuation of ADRICOSM forecasting activities

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. Continuation of ADRICOSM forecasting activities Paolo Oddo (INGV) National Institute of Geophysics and Volcanology Istituto Nazionale di Geofisica e Vulcanologia

  2. OUTLINE • The ADRICOSM operational system • Recent improvements • New results and validation • Conclusion

  3. ADRICOSM operational system • POM Based Code • 5km horiz. Resolution • 21 vertical sigma layers • Smol. Advection scheme

  4. RECENT IMPROVEMENTS

  5. New Results and Validation Summer Winter Climatological (from new sys.) seasonal surface circulation fields.

  6. New Results and Validation Mean and Instantaneous circulation patterns

  7. New Results and Validation T/S diagrams from Obs(dark) and Model (Red). Divided by Year :(2001-2002-2003) and sub-regions: Northern, Middle and Southern Adriatic

  8. New Results and Validation Comparison between surface CHL (Satellite) and model predicted salinity patterns CHL SALT

  9. Conclusions • The ADRICOSM Regional model is operational in both configurations (5km and 2km NO WEB). • Recent model changes have improved numerical results • Comparison with available observation has shown that some old model deficiencies has been fixed.

More Related