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Changchun Institute of Optics Fine Mechanics and Physics

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1 Changchun Institute of Optics Fine Mechanics and Physics
The technology of a new generation Utraviolet hyperspectral for detecting global ozone profile Changchun Institute of Optics Fine Mechanics and Physics

2 Earth nadir and limb detecting technology Calibration for payload
Content Earth nadir and limb detecting technology UV hyperspectral for detecting ozone profile Calibration for payload

3 Earth nadir and limb detecting technology for UV
Nadir observation Nadir viewing measurements should be used to retrieve total column amounts with high horizontal resolution. Limb observation Limb viewing measurements is particularly suited for the retrieval of profiles with high vertical spatial resolution .

4 Nadir observation instrument
Wavelength band:160 nm nm Wavelength accuracy: 0.02nm Wavelength repeatability:0.035nm Calibration accuracy:3%(relative) Dynamic range:10E5 Stray light:10E-5 SUBS on FY-3 A、B 、C satellite launched in 2007、2010、2012 FY-3 B The projection figure of the ozone in the South Pole for different height layers The projection figure of the ozone in the South Pole measured by FY-3B satellite in 2008

5 UV hyperspectral for detecting ozone profile

6 2. UV hyperspectral for detecting ozone profile
In order to obtain the ozone profile of atmosphere compos- ition and other composition , the observation wavelength is covered from 250nm to 500nm. Composition Wavelength Height Bandwidth Characteristics O3 nm 35-70 km < 1 nm absorbed O 297.3 nm km < 0.4 nm emitted OH 308 nm 60-90 km NO2 nm 15-40 km < 0.7 nm

7 UV hyperspectral for detecting ozone profile
The high spectral resolution (0.4 nm to 0.6 nm), It is a passive remote sensi-ng spectrometer detecting light in the wavelength range from nm to 500nm. Three view Nadir : ±36° Limb : ±10° Sun calibration : 18°×18°

8 UV hyperspectral for detecting ozone profile
This spectral range is divided into three channels, the high S/N values of this instrument allows the measurement for a wide range of ozone. The payload has a two-mirror scan system, allowing nadir and limb scans. The payload has different optical efficiencies for different polarization orientations of incoming radiation.

9 Spatial coverage Nadir light ESM Limb light ASM ESM

10 Calibration for payload

11 Calibration on orbit Radiation Spectrum
Monitor the degradation of optical systems Diffuser Scanning mirror (ASM and ESM) Spectrometer Spectrum Spectrum position The calibration wheel

12 Calibration on the ground
Mercury lamp Spectrum Calibration Wavelength calibration The Wavelength of Mercury lamp Atmospheric Wavelength Vacuum wavelength Intensity Type / 1000 400 15000 320 250 320.82 100 150 2800 750 300 1200 1800 120 4000

13 Calibration on the ground
Spectrum Calibration Spectral calibration device Spectral calibration procedure

14 Calibration on the ground UV-VIS integral sphere
Radiation Calibration UV-VIS integral sphere Radiance calibration Spectral radiance response degree calibration Calibration instrument : UV-VIS integral sphere Standard diffuser Standard spectral radiometer Standard quartz halogen tungsten lamp

15 Calibration on the ground
Radiation Calibration Spectral irradiance response degree calibration Calibration instrument : Standard quartz halogen tungsten lamp Standard xenon lamp Standard diffuser Scanning system azimuth calibration Difference of radiation responsiveness due to difference of the incident angle. Calibration instrument : UV collimator Light source Revolving stage

16 UV hyperspectral for detecting ozone profile
moderately high spectral resolution high radiometric accuracy high spectral stability high dynamic range high signal-to-noise

17 UV hyperspectral for detecting ozone profile
Nadir Limb Object O3 profile O3、NO2、SO2 Wavelength 250~310nm nm Spectral Resolution Nadir Limb Observation Spatial Resolution 34  60 km 3 km IFOV 2.3 º × º Nadir Limb Dynamic Range 105 Calibration Accuracy 2% Stray Light 10-5

18 Polarization

19 Thanks !


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