WhatsnOKC said:
I'm curious, is this "lack of sampling time" you spoke of the reason the cells look elongated when the antenna turns fast? It almost sounds like it contradicted the "speed of light" comments but I figure the short sampling time means the computer processor just can't handle the amount of data coming in, or am I off base?
This is an effect of physics that is seen in all radars. First of all, keep in mind that the radar sends very short bursts of RF out as it completes a scan. The distance between each pulse sent is very small close to the radar however the distance between pulses/beams increases at a greater distance.
Think of slicing a pie. Start at the center of the pie and then go to the outside edge to make the first cut. Now go back to the center to start the second cut in order to make a slice. You have no choice but to angle the second cut so that the pie slice is triangular. For the next slice of pie, once again, you'll have to angle the cut in order to make a slice of the pie.
So how in does this apply to weather radar? Well, if you draw a circle on a piece of paper to represent the radar scope and then plot each pulse repetition you would see this pie slice effect. You will see that the distance between the beams becomes much greater from each other near the edge of the radar scope. Therefore the range bins are much larger. To compensate for this the radar will fill the entire range bin with the dBZ level that is measured in that beam. This will cause the storm to look elongated since it simply can’t resolve what is happening between the beams at that distance. It is a matter of physics and not whether the radar transmits four times the power of others like KFOR claims to their viewers. All radars are subject to the laws of physics and KFOR’s is not an exception.
To elaborate further on this… next time you see a squall line in western Oklahoma on a radar near Oklahoma City (whether is be KFOR’s new radar or another) notice how when the storms approach the radar site that they appear to break up. In many cases they are not, rather the radar is simply able to resolve the storms better because of smaller range bins and it will become apparent that the squall line is actually made up of smaller individual cells.
I agree with 2112. The National Weather Service’s WSR-88D is much more advanced in that it has several products and algorithms which other radar’s owned by television stations don’t. There are so many products available to NWS meteorologists that the majority of the public would not see by watching KFOR or another television station. These products, and interpolation of the available algorithmic data as well as the ability to see the vertical structure of a storm by taking advantage of the numerous tilts available on the WSR-88D, are vital in the warning decision making process.
In my opinion, the only advantage I see with KFOR’s new radar is it’s location. It is further west than other radars (including the WSR-88D Twin Lakes site). This provides for smaller range bins resulting in better resolution in those areas just a slight bit southwest of where we are used to seeing the best resolution.
Also, to address the comment about the television monitors in the National Weather Service in Norman… they are used during severe weather to view live images such as those from the news helicopters for further verification of what is being seen on radar. Many offices will use the television monitors to simulcast the display of a chosen AWIPS work station for better visibility around the office or to display a rotating sequence of products/images such as satellite imagery and SPC outlooks. They are not used to listen to “what the tv stations are saying about specific storms.”
Sorry for sliding slightly off the topic toward the end.
Randy – K4TVS