To understand Doppler radial velocity patterns, one first has to consider the geometry of a radar scan. Normally the radar beam is pointedat an elevation angle greater than zero so that the beam, as it moves awayfrom the radar, moves higher and higher above the surface of the earth.Because of this geometry, radar returns originating from targets near theradar represent the low-level wind field, while returns from distant targetsrepresent the wind field at higher levels.
On a radar PPI display, the distance away from the radar at thecenter of the display represents both a change in horizontal distance and achange in vertical distance. To determine the wind field at a particularelevation above the radar, one must examine the radial velocities on a ring at a fixed distance from the radar. The exact elevation representedby a particular ring depends upon the elevationangle of the radar beam.
In the examples below, idealized Doppler radial velocity patterns wereconstructed with a computer assuming simple vertical wind field patterns.These simplified radial velocity patterns can help us understand the morecomplicated patterns that are associated with storm motions. Doppler velocity patterns (right) correspond to vertical wind profiles (left),where the wind barbs indicate wind speed and direction from the ground up to 24,000 feet. Negative Doppler velocities (blue-green) are toward the radar and positive (yellow-red) are away. The radar locationis at the center of the display.
Image by:Brown & Wood
For this first example,wind direction is constant with height, but wind speed increases from20 knots at the ground to 40 knots at 24,000 feet. Note on the radial velocityfield that the maximum inbound velocity is to the west and maximum outboundto the east while to the north and south the radar measures zero radial velocity. This is because the winds are perpendicular to the radar beam whenviewed to the north or south.
Image by:Brown & Wood
In the second example, the winds increase from 20 to 40 knots betweenzero and 12,000 feet and then decrease again to 20 knots at 24,000 feet.The wind direction again is constant.The radar beam intersects the 12,000 foot level along a ring half-way acrossthe radar display. This is where we see the maximum inbound and outbound velocities.
Image by:Brown & Wood
In the third example, we see a wind field which changes direction fromnorth to south but has a constant speed at all heights. The zero radialvelocity line now bends so that it is everywhere perpendicular to the windfield. The maximum radial velocities are observed where the radar beam points directly toward or away from the wind direction.
Image by:Brown & Wood
In our fourth example, we see the same effect but in this case, the flowis confluent instead of difluent.
 Imagery | Terms for usingdata resources.CD-ROM available. |  directional shear |
