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Measuring weather
Radar systems are always in a state of development and upgrading. In the first half of 2013, the United States completed installation of the newest generation of radar, known as dual-polarized or polarimetric radar. This was an upgrade to the single-polarized radar, or conventional radar, in operation since the late 1980s. Polarization refers to the orientation of the radar pulse waves. Polarization in one direction returns information in only one dimension, precipitation or no precipitation. It cannot differentiate between different types of precipitation, like rain, snow, and hail. Dual polarization produces these types of observations. By comparing data from the horizontally and vertically oriented pulses, we can determine the size and shape of the precipitation particles or even whether they are insects or tornado debris, which leads to a better estimate of precipitation, and therefore potential for flooding, and the ability to better spot tornados at night. Radar is also used on some aircraft. The airplane you see to the left carries the ELDORA (Electra DOppler RAdar) that was developed in part at the National Center for Atmospheric Research in Boulder, Colorado. It is mounted on the rear of the Lockheed P-3 aircraft you see here. Next page -> remote observations, satellite Links and resources |
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