Doppler radar uses the Doppler effect to return additional information from a radar system. The Doppler effect shifts the frequency of the radar beam due to movement of the "target", allowing for the direct and highly accurate measurement of speeds. Doppler radars were originally developed for military radar systems, but have since become a part of almost all radar systems, including weather radar and radar guns for traffic police and sports.

Contents

1 Basic concept 2 Doppler radar as weather radar 3 Comparison of Reflectivity and Doppler Velocity 3.1 On the left: 3.2 On the right: 4 External links

Basic concept

Early radar systems send out powerful radio pulses that were reflected off "targets"; the reflected signal was then detected on a separate antenna. Systems soon evolved to use the same antenna to act as both a broadcaster and receiver, with electronics switching between the two modes. These pulse radar systems had several drawbacks, however. Since the system could broadcast and receive at the same time, the pulses had to be fairly short to allow them time to travel out to the target and back, which meant that the total energy reflecting off the target was reduced. The pulses could be extended to return more energy, but this reduced the range. Another problem was that the pulses would reflect off of any solid object, including the ground, so they had to be pointed up in order to detect airborne targets - allowing aircraft to escape detection close to the ground. While this was only a minor problem for ground-based radars, aircraft radars could not see targets below them.

Using the Doppler effect allows both of these problems to be avoided. Instead of sending out pulses, the radio signal is continuous, thereby maximizing the amount of energy returned from the target. For this reason the system was often referred to as continuous-wave radar when it was first being introduced. The target is "seen" because the returned signal will be frequency shifted due to the Doppler effect, allowing it to be picked out of the outbound signal by filtering. Since the amount of shifting is dependent on the relative speed of the target, the minimum detectable speed is a function of the narrowness of the filtering the equipment is capable of.

In aircraft use, the filters can be set to filter out any signal with the exact same speed as the aircraft, thereby filtering out the reflection from the ground. This allows the radar to look straight down, detecting aircraft that were formerly invisible. As with pulse radar systems, many Doppler systems also pulse their signal to allow the use of a single antenna in these roles.

Since the Doppler system requires a speed difference between the antenna and target in order for there to be a phase shift to detect, it is possible to "spoof" them by flying parallel to the radar, or laterally "across the front". For this reason most aircraft radar systems use both the returned pulse and the Doppler shift to detect targets.

Doppler radar as weather radar

A simple weather radar can detect precipitation or objects just by the reflection of microwaves. Most weather radars employ pulsed microwave signals. With more precipitation or a bigger object, there is more reflectivity. As in the case with heavy rain or hail, more signal is reflected back to the radar dish.

In meteorology, the Doppler effect becomes especially useful. While Doppler radar can still detect reflectivity, other information is collected from the returning microwave signal's Doppler shift. The information is then used by computers to derive wind velocity in real time. The velocities that can be detected by a single dish are velocities directed away from the dish or toward the dish (see vector mechanics).

Even though most weather radar has the ability to collect Doppler wind velocities, it is usually not used for display to the public since it is difficult for even the most experienced meteorologist to quickly understand. Typically, research meteorologists depend more heavily on the Doppler data for wind vector retrieval. Also, for example, some products from Doppler data are used to indicate (on the reflectivity display) regions of wind shear. Most TV meteorologists refer to their radar products as "Doppler", when in reality their displays are just reflectivity.

Comparison of Reflectivity and Doppler Velocity

The best way to show the vast difference between the Doppler velocity display of a radar and the normally seen reflectivity display is to directly compare the two products from one radar scan. The following image is a vertical radar sample, or RHI, of a rapidly approaching cold front. Essentially, the cold air is forcing the warm-moist air upward so rapidly, that a fast moving thunderstorm is produced at the edge of the cold front.

The above depicts two products of one radar sampling. This image comes from a Doppler capable weather radar. In other words, the radar is capable of retrieving velocity information as well as reflectivity. The main tricky characteristic of doppler velocity is that the values collected are radial velocities. Meaning that all points on the velocity display are velocities that are going away or toward the radar.

On the left:

The Doppler velocities depict a wind pattern consistent with an updraft. But being so colorful, it loses the interpretation of where the rain is actually falling. However, the radial Doppler velocity is also not a true velocity. It is merely a vector component of the real velocity of the particles that have been detected.

On the right:

This display on the right is really a power return product. However, it is directly related to reflectivity. In this display, the red is actually where the rain is.

External links

• Weather Radar in a Shoe Box (http://avc.comm.nsdlib.org/cgi-bin/wiki_grade_interface.pl?Weather_Radar_In_A_Shoe_Box): A lesson plan from the National Science Digital Library
• Near realtime U.S. National Weather Service radar image (http://weather.noaa.gov/radar/mosaic.loop/DS.p19r0/ar.us.conus.shtml)