The NOAA Dual-Beam UV-Absorption Ozone Photometer (NOAA-O3) is an in situ optical balloon-borne and airborne instrument that measures ozone concentrations in the troposphere and lower stratosphere. It operates at the 254 nm wavelength allowing it to calculate the ozone number density due to the accurate ozone absorption cross section at that wavelength. It has a sampling rate of 2 Hz and a horizontal resolution of 100 to 200 meters at typical research flight speeds.


Instrument Details
- Optical/Photon
- Earth Science > Atmosphere > Air Quality > Tropospheric OzoneEarth Science > Atmosphere > Atmospheric Chemistry > Oxygen Compounds > OzoneEarth Science > Atmosphere > Air QualityEarth Science > Atmosphere > Atmospheric Chemistry
- Lower Stratosphere, Troposphere
- 2 Hz
- 100-200m
- 1180 THz
- https://doi.org/10.1063/1.1137316
Troy Thornberry, Erik Richard
Troy Thornberry, Erik Richard
NOAA
NOAA, FAA
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