2003
DOI: 10.1117/12.508544
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Cross-track Infrared Sounder (CrIS) development status

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Cited by 19 publications
(13 citation statements)
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“…To return to the radiance space, multiply by the noise estimate and add mean radiance i R Random noise, filtered out after reconstruction of the original data by truncated set of optimal number of PCs, can be estimated as the standard deviation of the residual errors between the original and reconstructed data: Knowing the total noise and its random component, the correlated component NEdN c can be easily estimated according to the equation (1). In our experience, only one PC needs to be retained to reconstruct typical BB spectra when random noise is dominant or comparable with spectrally correlated noise.…”
Section: Appendix Pca Approach For Instrument Noise Characterizationmentioning
confidence: 99%
See 1 more Smart Citation
“…To return to the radiance space, multiply by the noise estimate and add mean radiance i R Random noise, filtered out after reconstruction of the original data by truncated set of optimal number of PCs, can be estimated as the standard deviation of the residual errors between the original and reconstructed data: Knowing the total noise and its random component, the correlated component NEdN c can be easily estimated according to the equation (1). In our experience, only one PC needs to be retained to reconstruct typical BB spectra when random noise is dominant or comparable with spectrally correlated noise.…”
Section: Appendix Pca Approach For Instrument Noise Characterizationmentioning
confidence: 99%
“…Together, these instruments provide precise measurements of vertical distributions of temperature, moisture, and pressure within the Earth's atmosphere. CrIS is a sophisticated interferometric sounding sensor which accurately measures upwelling infrared radiance at very high spectral resolution [1] . The science heritage for CrIS was derived from the Atmospheric Infrared Radiation Sounder (AIRS) on the NASA EOS Aqua satellite [2] and Infrared Atmospheric Sounding Interferometer (IASI) on the European Metop platform [3] [4] .…”
Section: Introductionmentioning
confidence: 99%
“…The impact is mainly obtained for geopotential height, mean surface level pressure and wind forecast depending on the verification areas. Guidard et al (2011) studied the impact of IASI assimilation in both global and regional Météo-France models. They showed a quite good impact on the forecast skills for large-scale variables such as tropospheric temperature, wind fields and 500 hPa geopotential height both in the global ARPEGE (Action Petite Echelle Grande Echelle) model (Courtier et al, 1991) and the AROME (Actions of Research to Operations at Mesoscale) regional model (Seity et al, 2011).…”
Section: Introductionmentioning
confidence: 99%
“…A huge quantity of improvements have taken place in the first decade of the 21st century with the launch of new infrared (IR) sounders such as the Atmospheric Infrared Sounder (AIRS) in 2002 (Aumann et al, 2003), the Infrared Atmospheric Sounding Interferometer (IASI) in 2006 (Cayla, 2001;Chalon et al, 2001) and the Cross-track Infrared Sounder (CrIS) in 2011 (Glumb et al, 2003). These instruments have drastically raised the amount of information available for meteorological purposes compared to the precedent HIRS (High-resolution Infrared Radiation Sounder) infrared sounder, launched in the late 1970s, which offers 19 IR and 1 visible channels as compared with the thousands of channels available in this new generation of instruments.…”
Section: Introductionmentioning
confidence: 99%
“…Fourier transform spectrometers like Infrared Atmospheric Sounding Interferometer (IASI) [Diebel et al, 1996], Cross-Track Infrared Sounder (CrIS) [Glumb et al, 2003], Geostationary Imaging Fourier Transform Spectrometer (GIFTS) [Smith et al, 2001], and Hyperspectral Environmental Sounder (HES) [Li et al, 2003], and grating spectrometers like the Atmospheric Infrared Sounder (AIRS) [Aumann and Miller, 1995;Rosenkranz and Staelin, 1994] represent the present and the future of the atmospheric remote sensing in the infrared part of the spectrum. The observing capabilities of these systems, in terms of accuracy and spatial resolution of the retrieved geophysical parameters, can be significantly improved by increasing the spectral resolutions and/or enhancing the signal to noise ratios [Smith et al, 1979;Huang et al, 1992;Zhou et al, 2002].…”
Section: Introductionmentioning
confidence: 99%