Isentropic analysis is a common and effective way to diagnose horizontal and vertical motion of the atmosphere, the combination of 3D visualization feature of the IDV and the isentropic analysis helps us better visualize the dynamic and stability of weather phenomenons.
Edit→Remove All Displays and Data
menu item
or the icon in the toolbar to clear them out.
Fields
panel open the 3D grid
node and Derived
node,
scroll down the Derived
node and select Potential Temperature IsoSurface
.
Displays
open Constant Theta Surface Height Plan View
node, and
select Isentropic Topography
and press
Create Display
OK
button to create the display.
Fields
panel open the 3D grid
node and Derived
node,
scroll down the Derived
node and select Potential Temperature IsoSurface Scalar Analysis
.
Displays
open 3D Theta Surface
node, and
select Contours Over Constant Theta Surface
and press
Create Display
Ok
button, a dialog will pop up to allow you to select the
Parameter
field. From the dialog, expand the 3D grid
node and select
the Temperature@Isobaric surface
field and click the OK
button.
Fields
panel open the 3D grid
node and Derived
node,
scroll down the Derived
node and select Potential Temperature IsoSurface Vector Analysis
.
Displays
open Constant Theta Surface Flow Displays
node, and
select Vectors Colored by Speed over Theta Surface
and press
Create Display
Ok
button, a dialog will pop up to allow you to select the
voctor
field. From the dialog, expand the 3D grid
node and
the Derived
node and select the True Wind vectors
field and
click the OK
button.