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© Woodhead Publishing Limited, 2011
and analyzed at 6 minute intervals so as to produce wind profiles. Typical wind
profiles are shown in Plate IV in colour section between pages 244 and 245. In the
profile, the horizontal axis denotes the time (from 5:42 am to 8:00 am with intervals
of every 6 minutes); the vertical axis denotes the height of the sky. The arrow-like
symbols denote the direction and velocity of the wind at the corresponding height
and in the corresponding time interval. The arrowhead denotes the wind direction
(according to the provision: up-north, down-south, left-west, right-east), and the
number of the arrow feather denotes the wind velocity (please refer to the legend).
The frequencies assigned to the wind profiler are in UHF and L band, which
are very crowded and noisy with radio, TV, and mobile communication signals
and therefore the radar is often paralyzed by the interference. This did indeed
happen, especially in or near the cities. For example, the wind profiles presented
in colour Plate IV are actually real observation data recorded by a weather station
in a suburb of Beijing. It is interesting to point out that the detecting range (or the
height above the radar) gradually got shorter (from 3000 m down to 1700 m or so)
after 6:30 am in the morning as people were getting up and more and more
mobile phones were switched on, indicating that the sensitivity of the radar was
affected by increasing interference (colour Plate IV (a)). Eight months later, rapid
growth in the number of mobile phones in Beijing caused the electromagnetic
environment to become much worse. This radar was blocked by the massive
interference noise and totally lost the ability to collect any reliable data, as shown
in colour Plate IV (b).
10.5.2 Laboratory tests of superconducting
meteorological radar
To solve the problem outlined above, it is necessary to employ pre-selective
filters. Unfortunately, due to the extremely narrow bandwidth (≤ 0.5 %), no
conventional device is available. The HTS filter can be designed to have a very
narrow band and very high rejection with very small loss, so it is expected that it
can help to improve the anti-interference ability of the wind profiler, without even
a tiny reduction of its sensitivity. In fact, because the LNA also works at a very
low temperature in the HTS subsystem, the sensitivity of the whole system will
actually increase. To prove this, two stages of experiments have been conducted
and the performance of the conventional wind profiler was compared with the
so-called HTS wind profiler, i.e., the corresponding part (the front-end, i.e., the
LNA) of a conventional radar was substituted by the HTS subsystem. The first
stage experiments are sensitivity comparison tests and anti-interference ability
comparison tests, conducted by measuring the sensitivity and the anti-interference
ability of the filters with quantitative instruments, such as a signal generator and
frequency spectrometer, etc. The second stage experiments are the field trail of a
superconducting meteorological radar with the conventional counterpart, which
will be introduced in the next section.