|
 |
 |
 |
The SBUV/2 is a nadir-pointing nonspatial spectrally scanning ultraviolet radiometer carried in two modules.
The two modules are the Sensor Module with the optical elements/detectors and the Electronics Module. The overall radiometric resolution is approximately 1 nanometer (nm). Two optical radiometers form the heart of the instrument: a monochrometer and a “Cloud Cover Radiometer” (CCR). The monochrometer measures the Earth radiance directly and selectively the Sun when a diffuser is deployed. The CCR measures the 379-nm wavelength and is coaligned to the monochrometer. The output of the CCR represents the amount of cloud cover in a scene and is used to remove cloud effects in the monochrometer data.
The SBUV/2 measures solar irradiance and Earth radiance (backscattered solar energy) in the near ultraviolet spectrum (160 to 400 nm). The following atmospheric properties are measured from this data:
- The global ozone concentration in the stratosphere to an absolute accuracy of
1 percent.
- The vertical distribution of atmospheric ozone to an absolute accuracy of 5
percent.
- The long-term solar spectral irradiance from 160 to 400 nm
Photochemical processes and the influence of “trace” constituents on the ozone
layer.
|
 |
Characteristics
|
Spectral Bands |
Central Wavelength (nm) |
Bandwidth |
|
|
|
|
|
|
1 |
252.00 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
2 |
273.61 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
3 |
283.10 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
4 |
287.70 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
5 |
292.29 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
6 |
297.59 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
|
301.97 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
8 |
305.87 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
9 |
312.57 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
10 |
217.56 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
11 |
331.26 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
12 |
339.89 ± 0.05 |
1 + 0.2, -0 |
|
|
|
|
|
Cloud Cover Radiometrics |
379.00 ± 1 |
3 + 0.3 |
|
Source: NOAA KLM User's Guide |
|