Followup to group meeting of September 27, 2005

Greg, I re-ran the simulation saving restart files, then picked a time (2004112012) and then ran it for 30 minutes with model output every 2 minutes (instead of 6 hours as usual). This was done because in using 6 hour output, we were assuming a constant diabatic pv change for 12 hours essentially. This reduces that to a 4 minute assumption. Also the radiation timestep was set to the model timestep (120 seconds). Below are those same plots from the group meeting except with this new simulation. It looks much better when I calculate advection this time...but the Lagrangian calculation is still pretty far off.
WRF PV profiles: Model output every 2 minutes

Ertel PV vertical profiles. The left plot shows the forward differencing in time, and the right plot shows centered differencing in time. In both plots, the blue line is the pv and the red line is the change in pv. Everything is in PV units.
Vertical profile is of potential vorticity and potential vorticity changes at the potential temperature core (gridpoint) of the vortex (2-minute change) Vertical profile is of potential vorticity and potential vorticity changes at the potential temperature core (gridpoint) of the vortex (4-minute change)
Vertical profile is of potential vorticity and potential vorticity changes averaged within the 280K tropopause potential temperature contour (2-minute change)
Plots without the advection term calculated (Lagrangian calculations). The plot on the left is from following the vortex at a single gridpoint, while the plot on the right is by taking an average within the 280K closed tropopause theta contour.
Change in Ertel PV (centered difference) follwoing vortex core vs. change from diabatic tendencies (full vertical profile) Change in Ertel PV (centered difference) following trop. theta < 280 K vs. change from Instantaneous diabatic tendencies (lower levels vertical profile)
Profiles with the advection term calculated. Uses centered differencing in time and space to estimate. The plot on the left is following a single gridpoint at the core while the plot on the right is by taking an average within the 280K closed tropopause theta contour. The goal here is for the green and red lines to match.
Change in Ertel PV vs. change from diabatic tendencies (gridpoint) Change in Ertel PV vs. change from diabatic tendencies (tropopause theta < 280 K) using only horizontal advection
Change in Ertel PV vs. change from diabatic tendencies (tropopause theta < 280 K) using horizontal and vertical advection.
Difference plots of the above: Difference between the left hand side (red line) and right hand side (green line).
Gridpoint difference plot Closed contour average difference plot
Potential vorticity on select pressure levels.
500:450 hPa EPV 850:800 hPa EPV
500:450 hPa EPV change - (EPV changes from diabatic + (horizontally) advective components) 850:800 hPa EPV change - (EPV changes from diabatic + (horizontally) advective components)
500:450 hPa EPV change - (EPV changes from diabatic + (horizontally + vertically) advective components) 850:800 hPa EPV change - (EPV changes from diabatic + (horizontally + vertically) advective components)
500:450 hPa EPV diabatic changes 850:800 hPa EPV diabatic changes
500 hPa vertial motion (omega) 850 hPa vertical Motion (omega)
500:450 hPa EPV advective (horizontal) changes 850:800 hPa EPV advective (horizontal) changes
500:450 hPa EPV advective (vertical) changes 850:800 hPa EPV advective (vertical) changes
500:450 hPa EPV advective (total) changes 850:800 hPa EPV advective (total) changes