
REINHARDT System- und Messelectronic GmbH
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MWS3_e Page 9
geändert am 03.11.2015 von DO
Manual MWS 3 & 485-Sensors
3.2.4 The Wind Speed sensor
is made up of an anemometer with optical scanning. Wind speed is measured without touch using
an optical detector. A peak detector finds every wind peak and hands them on the measuring
software. An average value is determined within the respective memory intervals and is reset
each time the software stores onto the harddisk. The sensor identifiers are WG for wind speed,
WS for wind peak and WD for wind average.
Range: in km/h from 0 to 200 km/h with ± 2.5 km/h measuring accuracy, (display also in m/s,
miles/h, Knot or Beaufort), starting speed < 0.8 m/s.
As we have a very comfortable, 3-fold way of measuring wind speed with current wind speed
(WG), average wind speed (WD) and wind peaks (WS), you can conform your wind measurement
to your very needs.
Please note that dependent on the current winds, the 3 different methods of measuring wind
speed can result in very differing graphs: When measuring WG, only a current value is written
in the selected measuring interval, when measuring WD and WS, there is continuous evaluation
and the whole measuring period is monitored.
Unit [km/h]
3.2.5 The Wind Direction sensor
There is a weather vane with a precision magnetical encoder and a rotation angle of 360 ° for
measuring wind direction. Wind direction is given in °, with 90° being East, 180° being South,
270° being West and 0 ° being North.
Range: in 360 °, measuring accuracy 5 °, starting speed, < 0.8 m/s, hysteresis < 5°.
Output is performed as WR (winddirection).
Unit [°]
3.2.6 The Clouds sensor WKS 485
The Cloudssensor detects if there are clouds or not using a thermopile.
If the sensor detects clouds in it's field of view, the sensor with the identifier WK has got the
value 1, if the sensor detects no clouds, this value is 0.
An additional internal signal is used to calculate the cloud's base using a special formula.
This formula calculates the cloud's base as follows: T(h) = T0- h * y,
where T(h) is the cloud's temperature, T0is the ambient temperature of the sensor, h is the alti-
tude and y is the temperature gradient in [K/m].
The temperature gradient y is the cooling down in [K) per metre altitude. The value of this gradi-
ent is depending on the humidity of the air (dry adiabatic lapse rate or wet-adiabatic lapse rate).
The wet-adiabatic lapse rate is app. 5*10-3 Km-1, the dry adiabatic lapse rate is app. 10-2 Km-1.
For the exact weather conditions in the athmospere are mostly not known, meteorologists calculate
with an average value of 6.5*10-3 Km-1, this means a cooling down of app. 6.5°C per kilometer.
This value also is used calculating the cloud's base within the WKS 485.
Finally the sensor with the identifier WU contains the cloud's base in [m].
The calculation of the cloud base by this formula can be faulty due to influences caused by different
weather situations and must not be used for security-related measurements, (i.e. air traffic, ...)!