This information was provided by Paroscientific, Inc. Precision Pressure Instrumentation.
This
report describes the calculations required for determining the
dew point temperature, using the measured temperature of the RTD
sensor and relative humidity sensor.
The algorithm is based on the Magnus-Tetens formula, over
the range
|
0°
C < T < 60°
C |
|
0.01
< RH < 1.00 |
|
0°
C < Td
< 50°
C |
where T is the measured temperature [°C]
RH is the measured relative humidity
and Td
is the calculated dew point temperature [°C]
The dew point temperature is
|
|
(1) |
|
|
(2) |
| with
a = 17.27 |
|
| and
b=237.7 [°C] |
The uncertainty in
the calculated dew point temperature is ±0.4°
C.
The
measured atmospheric pressure is the sum of two terms, the
partial pressure of dry air (pa)
and the partial pressure of water vapor (pw).
The water vapor pressure is a function of temperature,
and the dew point temperature (Td),
which is defined as the temperature at which the air is
saturated with water vapor.
Given
the measured temperature (T) and the measured relative humidity
(RH), it is possible to calculate the dew point temperature.
The present calculation limits the dew point to values
above freezing. This
provides for a more efficient calculation, although over a
limited range.
Definition & Limits
T
The measured temperature of the RTD sensor;
0°
C < T < 60°
C
Td
The calculated dew point temperature;
0°
C < Td
< 50°
C
RH
The measured relative humidity of the RH sensor;
0.01 < RH < 1.00
pws
The vapor saturation pressure
pw
The vapor pressure
|
|
|
with
a=17.27 |
|
b=237.7 |
|
and Td
is in °C. |
The vapor pressure
is related to the relative humidity and vapor saturation
pressure by
![]()
When
the air is saturated the relative humidity is equal to 100%, and
the temperature is equal to the dew point temperature, which
allows us to solve for the dew point temperature.
where
Uncertainty of Dew Point Temperature
The
uncertainty in the measured dew point temperature is a function
of the measured temperature and relative humidity and the
uncertainties associated with those measurements.
The uncertainty in
the measured dew point temperature is
where
s2Td
is the uncertainty in the calculated dew point temperature
s2T
is the uncertainty in the measured temperature
s2RH
is the uncertainty in the measured relative humidity
and
assuming no cross-correlated uncertainties.
Taking
the appropriate derivatives and collecting the terms, we find
the uncertainty in the calculated dew point temperature to be
Letting
the parameters be
T
= 60°
C, temperature range
RH=1.00
(100%), relative humidity range
sT
= 0.1°
C, uncertainty in the measured temperature
sRH
= 0.02 (2%), uncertainty in the measured relative humidity
The information on this website was provided by National Weather Service of Birmingham, AL
Heat index or HI is sometimes referred to as the "apparent Temperature". The HI, given in degrees F, is a measure of how hot it feels when relative humidity (RH) is added to the actual air temperature.
The following equation approximates the heat index. There are many assumptions made produce this, far too many to list here. The equation was obtain by multiple regression analysis and there is a ±1.3 degree °F error.
HI = -42.379 + 2.04901523T + 10.1433127R - 0.22475541TR
- 6.83783x10 -3 T 2 - 5.481717x10 -2 R 2
+ 1.22874x10 -3 T 2R + 8.5282x10 -4 TR 2
- 1.99x10 -6 T 2 R 2
where
The previous table was outdated and has been replaced by the following. Thanks to Lans Rothfusz, MIC at NWS Tulsa, OK for the following table.
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