Atmospheric Emitted Radiance Interferometer. Part I: Instrument Design
By R. Knuteson, H. Revercomb, F. Best, N. Ciganovich, R. Dedecker, T. Dirkx, S. Ellington, Wayne F. Feltz, R. Garcia, H. B. Howell and 3 more. 2004
276 citations recorded by the source corpus.
Subfields: Aerospace Engineering, Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/ca3904bd810f7f06909175ec0fc52cb6d85cf5c3
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Citations in the corpus
- Information Content and Uncertainties in Thermodynamic Profiles and Liquid Cloud Properties Retrieved from the Ground-Based Atmospheric Emitted Radiance Interferometer (AERI) (2014, methodology): “Operationally, this is computed from the spectral standard deviation of the calibrated imaginary radiance spectrum (Knuteson et al. 2004b).”
- Atmospheric Emitted Radiance Interferometer. Part II: Instrument Performance (2004, methodology): “The design of the AERI instrument meeting the requirements of the ARM Program is described in a companion paper (Knuteson et al. 2004, hereafter referred to as Part I).”
- In-situ measured spectral directional emissivity of snow and ice in the 8-14 μm atmospheric window (2006, methodology): “AERI has been developed to measure the atmospheric downwelling radiance at the surface with a high absolute radiometric calibration of better than 1% (Knuteson et al., 2004a,b).”
- Arctic Mixed-Phase Cloud Properties from AERI Lidar Observations: Algorithm and Results from SHEBA (2005, methodology): “The Atmospheric Emitted Radiance Interferometer (AERI) instrument (Knuteson et al. 2004) makes observations in both of these spectral regions.”