Operational Status:
not on request list but could be available if requested
General Description:
Measures air temperature by comparing air radiance in CO2 4.3 um band with a reference blackbody at near-ambient temperature. Generally unaffected by wetting caused by cloud passes so the main use is anticipated to be in clouds and immediately upon leaving clouds when the Rosemount sensors are affected by wetting or evaporation.
Measurement Characteristics:
- Overall estimate of uncertainty: Approximately 0.3 °C of ATX
- Response time: 0.1 second
- Precision: 0.2 °C, 1 second average.
- Other measurement characteristics (comments on signal/noise, bias limits, etc): The radiance received by the radiometer consists of the radiance of the air parcel extending away from the aircraft with an exponentially-decreasing weighting function. The effective averaging distance is dependent on air density and water droplets (which are opaque to 4.3 um radiation). In clouds, the radiance beyond a few tens of meters is negligible, whereas in clear air at high altitude the radiometer is still slightly sensitive to air temperature hundreds of meters distant. The radiometer is mounted so that it looks horizontally where there is the least temperature gradient. When the aircraft rolls in a turn there is typically a shift in the reported temperature as it looks up or down toward cooler or warmer air. Likewise, when the radiometer looks directly into the sun the reported temperature increases about 20 °C, and is worse at higher altitudes when the suns 4.3 um radiance is less completely absorbed by atmospheric CO2.
