You have requested a machine translation of selected content from our databases. This functionality is provided solely for your convenience and is in no way intended to replace human translation. Neither SPIE nor the owners and publishers of the content make, and they explicitly disclaim, any express or implied representations or warranties of any kind, including, without limitation, representations and warranties as to the functionality of the translation feature or the accuracy or completeness of the translations.
Translations are not retained in our system. Your use of this feature and the translations is subject to all use restrictions contained in the Terms and Conditions of Use of the SPIE website.
21 August 2009Spectral calibration in hyperspectral sounders
It is widely accepted that the knowledge of the frequencies of the spectral response functions (SRF) of the channels of
hyperspectral sounders at the 10 parts per million (ppm) of frequency level is adequate for the retrieval of temperature
and moisture profiles and data assimilation for weather forecasting. However, SI traceability and knowledge at the 1 ppm
level and better are required to separate artifacts in the knowledge of the SRF due to orbital and seasonal instrument
effects from diurnal and seasonal effects due to climate change. We use examples from AIRS to discuss a spectral
calibration that uses the SI traceable upwelling radiance spectra to achieve an absolute accuracy of 0.5 ppm.
The alert did not successfully save. Please try again later.
Evan M. Manning, Hartmut H. Aumann, Robert G. Deen, Yibo Jiang, L. Larrabee Strow, Scott E. Hannon, "Spectral calibration in hyperspectral sounders," Proc. SPIE 7452, Earth Observing Systems XIV, 74520H (21 August 2009); https://doi.org/10.1117/12.826987