Stratiform vs Convective RefVel stratiform Convall radref Cloud
- Slides: 15
Stratiform vs Convective
Ref+Vel stratiform Conv(all)+ rad_ref Cloud analysis followed by 3 dvar Conv(uv+spd)+rw Only 3 dvar analysis Applied DFI to Qv only, other mosit variable like Qs, Qc, Qr, Qg, Qi are remain unchanged and Temperature tendency added gradually (Current RUC version) CV(Ref+Vel) convective The same above Cld_qv Qcw and Qci use Convective method and Qv using the stratiform or convective method, and all of these based on the classification. The same above Cldall using the stratiform or The same convective method based on above the classification. The same above
Qn (Convective) – Qn (Stratiform) 700 h. Pa
Qn (Convective) – Qn (Stratiform) 500 h. Pa
Qcw (Convective) – Qcw (Stratiform) tmc (Convective) – tmc (Stratiform)
Classify methods • Steiner et al. 1995 (1). Ref. Z 3 km>40 dbz (2). Ref. Z 3 km-Zbg > 10 – Z 2 bg /180 here, Zbg is average of Ref at 3 km height 11 km around the computer grid. (3)any grid point identified as a convective center by one of above two criteria, all surrounding grid points within an intensity-dependent convective radius around that grid point are also included as convective area But considering the grid resolution of RR is 13 km , we only applied the rule (1) and (2).
Observed reflectivity at 3 km from 2006061518 - 2006061618
SHY 95 result
Cold start interval Case name Novar_cold 061515 GSI Cloud analysis First pass Default value Second pass ¼ of default value No gsi Novar_cold 061603 Conv_cold 061515 The same above but cold start from GFS from 061603 stratiform Conv(all) none Conv_cold 061603 Ref_cold 061515 The same above but cold start from GFS from 061603 stratiform Conv(all)+ rad_ref none Cloud analysis followed by 3 dvar Ref_ cold 061603 Ref+Vel_cold 061515 The same above but cold start from GFS from 061603 stratiform Conv(all)+ rad_ref Conv(uv+spd)+rw Cloud analysis followed Only 3 dvar analysis by 3 dvar Ref+Vel_ cold 061603 The same above but cold start from GFS from 061603 DFI Moist variable which applied dfi Wrf office version dfi, with dfi_radar=0 Applied DFI to Qv only, other mosit variable like Qs, Qc, Qr, Qg, Qi are remain unchanged and Temperature tendency added gradually (Current RUC version) The same above
High resolution Lack of data?
- Thunderstorms reach their greatest intensity during the
- Cold front cross section
- Stratiform precipitation
- Orographic lifting
- Cloud formation
- Convective parameterization
- Coefficient
- Petukhov equation
- Chapter 18 moisture clouds and precipitation
- It is the water falling from the atmosphere.
- Localized convective lifting
- Mass flux
- Natural and forced convection examples
- Frontal wedging definition
- Convective sigmets
- Convective heat transfer coefficient formula