 
  
   
    
       Unidata's Integrated Data Viewer  > Getting Started
 
Unidata's Integrated Data Viewer  > Getting Started  
 
2.2 Level II Radar
This section describes how to  create displays from 
WSR-88D Level II data.  The set of steps include:
2.2.0 Accessing WSR-88D Level II Radar Data
 
The Level II data is supplied as volume-scan files,                     
each file having all data from one WSR-88D radar                        
for all sweeps for one "time". Unidata                        
Community sites can receive Level II data using the 
Unidata Local Data Manager (LDM). Archived Level II data is         
available from the  National        
Climatic Data Center (NCDC) (data from NCDC must be un-tarred).
The files should be stored on your file system with each station's files 
in a directory (folder) whose directory name is the station 
4-character ID (e.g., KTLX for Oklahoma City).  In many cases the data
files do not have any location information in them and the IDV uses the
directory name as a first guess at the station location.  Otherwise,
use the Radar Location widget to specify the location.
2.2.1 Choosing Level II Radar Data
 
In the Data Source Chooser
window click on the Radar tab and then the 
Level II tab.
Use the file chooser to find the directory which holds the data you     
want to display. Click on a file name you desire (multiple files can be 
selected with the Shift or Control keys) or select
the latest N files. When you have   
selected all files you need, click the Add Source button.  
2.2.2 Making Level II Radar Displays
 
The data source is shown in the 
Field Selector window. 
Level II     
data has three moments or data types: Reflectivity, RadialVelocity,    
and SpectrumWidth. The IDV has several kinds of displays for Level II  
data. Any of the moments can be shown with any of the displays. Here we 
will use examples showing reflectivity. Clicking on the "Reflectivity"  
entry in the Field panel will show the list of available         
displays in the Displays panel.                                  
2.2.3 2D Displays of Individual Sweeps
 
 Image 3: Level-II 3D Display
Image 3: Level-II 3D Display
The 
Radar Sweep Control 
allows you to change which sweep elevation you want         
to see. You can add range rings with the  menu item. You can modify the range rings with the        
Radar Range Rings      
control.                                                            
2.2.4 3D Displays of Individual Sweeps
 
 Image 4: Level-II 3D Display
Image 4: Level-II 3D Display 
You can use this display to merge radar data display with upper         
air data such as the IDV plots of NOAA Profiler data. Since             
the Earth is projected onto a flat surface in this display,             
the sweep has a shape very close to a rotated parabola. The Radar Sweep Control     
allows you to change which sweep elevation to display.                  
2.2.5 Pseudo-RHI Displays in 2D and 3D
 
|  Image 5: Level-II 2D RHI |  Image 6: Level-II 3D RHI | 
Select RHI in the Displays panel and press Create Display.
RHI plots the data as an colored vertical cross section at the true 
elevations of the beams in 3D space (bottom illustration). This pseudo-RHI is 
constructed from several horizontal sweeps of the radar. You may have to rotate 
the display to see the RHI in 3D. 
 
The beam width is indicated by the vertical extent of each colored 
vertical stripe, corresponding to a bin beam bin sample. Beam overlap is clear. 
Position of the RHI in azimuth can be adjusted by dragging the little box 
on the end of the selector line above the RHI. 
The 2D plot of pseudo-RHI (top illustration) is shown in the RHI Control. That control 
also has an auto-rotate feature. The RHI displays have time animation.  
2.2.6 All Sweeps in 3D
 
 Image 7: Level-II Volume Scan
Image 7: Level-II Volume Scan2.2.7 Radar Isosurfaces in 3D
 
Select "Reflectivity" in the Field panel and select              
Radar Isosurface in the Displays panel. An isosurface
is a 3D analog of a contour line. It shows the location of all data     
with a single data value. Interpolation is used between sweep altitudes 
in the IDV isosurface plot of Level II data. All data in a volume       
scan is used. The example shown is the 50 dBZ isosurface from a line    
of thunderstorms crossing Oklahoma at 1330Z 11 Sept 2003. Vertical      
exaggeration is 13 to 1.                                                
 Image 8: Level-II Isosurface
Image 8: Level-II Isosurface
 
 
 
  
   
    
      Unidata's Integrated Data Viewer  > Getting Started
 
Unidata's Integrated Data Viewer  > Getting Started