
User Guide
13
in the air has not changed. Thus, the amount of water vapour in the air, relative
to saturation, has decreased.
Because of the inverse relationship between relative humidity and air
temperature, finding the mean relative humidity is meaningless. A more useful
quantity is the mean vapour pressure. The mean vapour pressure can be
computed on-line by the datalogger (Example 3).
Table 8. Wiring for Vapour Pressure Examples
Description Colou
CR1000 CR10(X)
Temperature White SE 2 (1L) SE 3 (2H)
Relative Humidity Green SE 1 (1H) SE 4 (2L)
Signal Reference Blue AG
Jumper from
SW12V Control
N/A C1
Powe
Red SW12 V SW12 V
Power Ground Black AG
Shield Clear G
NOTE: These wire colours differ from HMP45C probes supplied in the USA.
CR1000 Program that Computes Vapour Pressure and Saturation Vapour Pressure
'CR1000 program that calculates Vapour Pressure
Public AirTC
Public RH
Public RH_Frac, e_Sat, e_kPa
DataTable(Temp_RH,True,-1)
DataInterval(0,60,Min,0)
Average(1,AirTC,IEEE4,0)
Sample(1,RH,IEEE4)
Sample(1,e_kPa,IEEE4)
EndTable
BeginProg
Scan(1,Sec,1,0)
'HMP45C Temperature & Relative Humidity Sensor measurements AirTC and RH:
SW12 (1 )
Delay(0,150,mSec)
VoltSE(AirTC,1,mV2500,2,0,0,_50Hz,0.1,-40.0)
VoltSE(RH,1,mV2500,1,0,0,_50Hz,0.1,0)
SW12 (0)
If RH>100 And RH<108 Then RH=100
'Calculate Vapour Pressure
'Convert RH percent to RH Fraction
RH_Frac = RH * 0.01
'Calculate Saturation Vapour Pressure
SatVP(e_Sat, AirTC)
'Compute Vapour Pressure, RH must be a fraction
e_kPa = e_Sat * RH_Frac
CallTable(Temp_RH)
NextScan
EndProg
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