1 / 14

G. Haase, T. Landelius and D.M. Michelson

WP2: Extraction of Information from Doppler Winds. G. Haase, T. Landelius and D.M. Michelson. Swedish Meteorological and Hydrological Institute. Doppler wind measurements. Quality control (e.g. de-aliasing). Assimilation into NWP models (e.g. VAD profiles, superobservations …).

nigel-white
Télécharger la présentation

G. Haase, T. Landelius and D.M. Michelson

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. WP2: Extraction of Information from Doppler Winds G. Haase, T. Landelius and D.M. Michelson Swedish Meteorological and Hydrological Institute

  2. Doppler wind measurements Quality control (e.g. de-aliasing) Assimilation into NWP models (e.g. VAD profiles, superobservations …)

  3. Aliasing problem Doppler “dilemma”

  4. De-aliasing algorithm Linear wind model:

  5. De-aliasing algorithm Linear wind model: Map the measurements onto the surface of a torus

  6. Case study Vantaa (Finland): 4 December 1999, 12:00 UTC

  7. Case study Vantaa (Finland): 4 December 1999, 12:00 UTC observed velocity de-aliased velocity

  8. Validation Hemse (Sweden): 2 July 2003, 10:47 UTC Sample size: 388,147 pixels Nyquist velocity: 7.55 m/s

  9. Application 1: Wind profiles (VVP) Vantaa (Finland): 4 December 1999, 12:00 UTC

  10. Application 2: Superobservations Vantaa (Finland): 4 December 1999, 12:00 UTC

  11. Application 2: Superobservations Vantaa (Finland): 4 December 1999, 12:00 UTC observed velocity de-aliased velocity

  12. Summary • accurate & robust post-processing algorithm • (elimination of multiple folding) • no additional wind information needed • (independent data source) • improved quality of wind profiles and superobservations for data assimilation

  13. To do • validate the new de-aliasing algorithm for convective precipitation events • generate de-aliased superobservations: • SMHI & FMI: July 2000 + January 2002 • prepare real-time application

  14. Deliverables • Report: Radar radial wind superobservations • (http://carpediem.ub.es) • Data sets

More Related