Leica Nova MS60 - Scale Correction

MS60/TS60, Technical Data
83
7.13 Scale Correction
Use of scale
correction
By entering a scale correction, reductions proportional to distance can be taken into
account.
• Atmospheric correction.
• Reduction to mean sea level.
•Projection distortion.
Atmospheric
correction D1
The slope distance displayed is correct if the scale correction in ppm, mm/km, which
has been entered corresponds to the atmospheric conditions prevailing at the time of
the measurement.
The atmospheric correction includes:
• Adjustments for air pressure
•Air temperature
• Relative humidity
For highest precision distance measurements, the atmospheric correction should be
determined with an accuracy of 1 ppm. The following parameters must be redeter-
mined:
• Air temperature to 1 °C
• Air pressure to 3 mbar
• Relative humidity to 20 %
Air humidity The air humidity influences the distance measurement if the climate is extremely hot
and damp.
For high precision measurements, the relative humidity must be measured and
entered along with the air pressure and the temperature.
Air humidity
correction
Index n
The index n is calculated from the formula of the IAG Resolutions (1999), and is valid
for:
ppmAir humidity correction [mm/km]
% Relative humidity [%]
C° Air temperature [°C]
ppm
+5
+1
+2
+3
+4
+0
-10-20 0 10 20 30 40 50 °C
100%
80%
60%
40%
20%
TS_104
Type Index n Carrier wave [nm]
MS60 with R2000
(Wave Form Digitizer)
1.0002863 658
TS60 with R1000
Combined EDM (Phase Shift
/ System Analyzer)
Air pressure p: 1013.25 mbar
Air temperature t: 12 °C
Relative air humidity h: 60 %