Radar stuff... I think a link to the NWS basic info is warranted here since this is a really big subject to cover .... see
Using and Understanding Doppler Radar
I will touch a little on the two radar velocity products... Base and storm relative velocity indicates the speed and general direction of the particles ( insects, birds, ground clutter, moisture etc ) in the air that are seen by the radar. The base velocity ( BV ) is the speed/direction relative to the radar site itself and storm relative velocity ( SRV ) is actually the same data but the speed/direction is relative to the storm cells themselves.
Velocity color tables are often shown using red and green colors but they can be anything that are assigned to them by the person making the color table and can use multiple colors to help delineate the different speeds. When using the more standard red/green colors... red usually indicates winds moving away ( positive numbers ) from the radar site and green is used for winds moving towards ( negative numbers ) the radar site.
On my own color tables that I use ( and made myself ), I begin with the standard red/green and then add additional colors to help delineate between the various EF scale speeds. The following info is the EF scale used to rate tornadoes...
; Tornado EF Scale
; 65-85 mph => EF0
; 86-110 mph => EF1
; 111-135 mph => EF2
; 136-165 mph => EF3
; 166-200 mph => EF4
; 201 + => EF5
;
The tornado wind speeds are giving in what is referred to as "gate to gate" speeds since we are discussing rotating winds. As an example, an EF1 with wind speeds of 100mph... on one side of the tornado the wind is traveling 50mph in one direction and on the other side it's going 50mph in the other direction. Because each side of the tornado is moving in different directions, the velocity colors will be both red and green creating what is called a "couplet" on the radar image. My velocity tables actually go up to +-200mph which is overkill if just used for tornadoes... but I can also use it for tropical storms ( hurricanes etc ) since they have much higher winds. I also have a special set just for hurricanes that is scaled for the CAT wind scale just in case that is what I'm looking at.
Here is a screenshot of one of my radar programs that has 4 panels, each panel having a separate type of radar. The top left panel has a typical base reflectivity ( BR ) showing, the top right has the base velocity ( BV ), the lower left has correlation coefficient ( CC - useful for detecting debris from a tornado ) and the lower right having the storm relative velocity ( SRV ).
This example of a tornado on May 19th, 2013 taken at 6:18pm.
The tornado couplet is seen just NW from Pink, Ok and ESE of the KTLX radar site. Also note there is a lot of "noise" just east of Pink within the large green area, this is caused by the radar having trouble reading the real values in that area due to the density of the tornado itself. The tornado at this point is likely an EF3 or EF4.
( please note that the background color I'm using in this screenshot is a dark gray )
In a couple of the earlier posts, I mentioned that I was making and tweaking on new color tables for my BV and SRV radar. The following screenshot, take earlier in the day from the above shot... shows the same mesocyclone ( aka meso - the type of rotating storm cell that can produce a tornado ) much earlier in it's development. If you locate Blanchard, Ok ( lower left corner of each panel ) and look just to it's NW... you should see a really weak couplet that is shown as dark red and green in the BV panel but in the SRV panel it's seen as dark red to almost an orange.
While it is possible that there may be a funnel ( a tornado that hasn't touched the ground ), it's unlikely and more than likely it's just the rotation in the meso itself starting to show on radar. About 30 minutes later it actually passed over where I was located ( the little red cross on the screen ) and then later developed into the tornado mentioned above. None of the weather news people I was watching mentioned it at all until after it already developed on the east side of Norman, they were busy looking at other areas of rotation that never developed into anything but were closer to Moore and OKC. Luckily, I was paying attention and had managed to get to where I go in times like this... with about 20 minutes to spare.
