1 / 9

Preliminary Analysis of Koto Tabang Convection using EAR and A03 Instruments

Preliminary Analysis of Koto Tabang Convection using EAR and A03 Instruments. CPEA Meeting, March 28, 2003 T.Kozu 1 , T. Shimomai 1 , H.Hashiguchi 2 , S. Mori 3 , Y.Shibagaki 4 1 Shimane University, 2 Kyoto University, 3 FORSGC, 4 Osaka Electro-Communication University.

idola
Download Presentation

Preliminary Analysis of Koto Tabang Convection using EAR and A03 Instruments

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. Preliminary Analysis of Koto Tabang Convectionusing EAR and A03 Instruments CPEA Meeting, March 28, 2003 T.Kozu1, T. Shimomai1, H.Hashiguchi2, S. Mori3, Y.Shibagaki4 1 Shimane University, 2Kyoto University, 3FORSGC, 4Osaka Electro-Communication University

  2. ORG and WV profiler browse at CPEA A03 Web site http://rslab.riko.shimane-u.ac.jp/CPEA/data/index.html

  3. Rain rate and Radar reflectivity: 03 – 04 LT

  4. EAR vertical beam spectra: Mar. 28, 2002, 03:11 – 03:45 LT

  5. Disdrometer Z-R relationvs. Doppler Spectra

  6. Comparison of ORG and disdrometer data

  7. Radiometer TB’s as a rain detector aloft?

  8. Map for campaign planning

  9. Non-linear least-sq. fit of MST radar Doppler spectra of precipitation Relative Power (dB) Doppler velocity (m/s) The same or an improved algorithm will be employed to both MST radar and EAR.

More Related