416  High-temperature superconductors
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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.