Real-Time PV Inversion

Due to technical difficulties the daily inversion has been temporarily suspended. (02/23/99)

This page is an attempt to bring an exciting new research topic to the operational environment. If it is your first time here, or if you are confused about something, you may want to take the time to read about the products on this page and the data and methods used to create them.

**4 Panel Balanced Fields vs Complete Fields**
Mean	F0	F6	F12	F18
F24	F30	F36	F42	F48
F0-F48

**4 Panel Piecewise Inversion Maps**
Upper PV Perturbation
F0	F6	F12	F18	F24
F30	F36	F42	F48	F0-F48
Interior PV Perturbation
F0	F6	F12	F18	F24
F30	F36	F42	F48	F0-F48
Surface Theta Perturbation
F0	F6	F12	F18	F24
F30	F36	F42	F48	F0-F48

For more analysis and forecast products from today's ETA model run see the the AOS Department's ETA model products page.

For more analysis and forecast products from today's UWNMS model run see the UW-NMS site or the AOS Department's 4-model comparison page.

Experimental Products (for the .meteor domain only)

Figure:

Hoskins. B. J., M. E. McIntyre, and A. W. Robertson, 1985:
On the use and significance of isentropic potential vorticity maps.
Quart. J. Roy. Meteor. Soc., 111, 877-946.

I am looking for feedback on this page so please write to me!

There have been visitors to this page since 6/20/97.

Sebastien Korner(korner@meteor.wisc.edu)

This work was supported by the National Science Foundation, Division of Atmospheric Sciences, Grant Number ATM-9505849.