Title: Measurement of thermal and net radiation
1Measurement of thermal and net radiation
Sd - Solar Diffuse
Sb - Solar Beam
La Sky Thermal
Loe Emitted Outgoing Thermal
Sr - Solar Reflected
Lg Ground Thermal
2Infrared Thermometer (IRT)
- Useful for non-contact measurement of surface T
- IRTs measure F (radiant flux density)
- If IRT sensor surface (generally blackened
thermopile) has e close to 1, then
3Infrared Thermometer (IRT)
Ideally.
4IRT absorption spectrum
- Most IRTs have filters that only pass 8-13 µm
radiation - Why?
Atmospheric Emittance (clear sky)
5Measuring T with IRTs
- IRTs measure radiant flux density (F, W/m2)
- If radiating surface is not a black body, F is
made up of emitted component and reflected
component - Only emitted component affected by T
Total Fseen by IRT Femitted by surface F
emitted by surroundings and reflected
(error)
6Errors in IRT from reflected radiation
From previous slide
What happens if Ti Ts?
7Errors in IRT from reflected radiation
From previous slide
What happens if es 1 ?
8Magnitude of error when e?1 and Ts ? Ti
- Generally less than 1 C under clear skies
- Much less under cloudy skies or indoors
- Correction not needed except in extreme
situations - Well create one of those situations in lab
9Determining emissivity of a surface
Solving our favorite equation for es
So if you can measure TT, Ts, and Ti, you can
calculate es
10Pyrgeometers
- Measure only thermal radiation
- Dome is specially designed to reflect solar and
transmit thermal radiation - Hemispherical view (unlike IRT)
11Measurement of Total Radiation
- Total radiation solar thermal
- Now we need both wavelengths to reach sensing
surface - Still need protection from convection..
- Can we still use a glass dome?
- Can we use black and white sensor?
12Total radiometer
solar in
thermal in
thermal emitted
conduction to base
If you assume as al e 1
C Calibration constant V mV output Need to
know Tb!
13Measurement of Net Radiation
- Rn total incoming total outgoing total
radiation absorbed by surface - Two ways to measure
- Summation of radiation components measured
independently - Net radiometers
14Component Summation
- Most accurate method
- Expensive several thousand for each sensor
15Net Radiometers
- Less Expensive, Less accurate
- Measure temperature difference between upward and
downward facing surface
16Net Radiometers
Rn Sd Ld Su - Lu
Only need to measure mV output to get Rn! (all
emissivity, absorptivity, and Tbase terms cancel
out)
17Calibration of total and net radiometers
- Short wave calibration
- Use a known standard (Eppley or Kipp pyranometer)
- Shade simultaneously on a clear day
- Long wave altered only slightly
- Direct short wave altered equally
- From standard pyranometer you know ?Sb
- From radiometer you know ? mV
- Radiation incident on opposite side must remain
constant
Calibration ?Sb/ ? mV
18Calibration of total and net radiometers
- Long wave calibration
- Alter long wave radiation with a long wave
emitter (radiator) - Need to know
- ? radiator temperature
- Emissivity of radiator
- Plate view factor
- Radiation incident on opposite side must remain
constant
19Calibrating the radiometer for todays lab
?Tradiator measure with IRT or
thermocouple Emissivity radiator painted with
optical black paint, e 0.98 View Factor (F)
d distance between source and sensor L length
of the radiator edges
calibration ? F/?mV
20Todays Lab (contd.)
- Use IRT to measure longwave energy budget for a
person - Pay attention to view factors
- Look at thermal emissivities of different surfaces