@MISC{Merrelli12theatmospheric, author = {Aronne Merrelli}, title = {THE ATMOSPHERIC INFORMATION CONTENT OF EARTH’S FAR INFRARED SPECTRUM}, year = {2012} }
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Abstract
A key component of the modern Earth observation system is the Mid-Infrared (MIR) hyper-spectral sounder. Operational instruments on polar orbiting satellites are collecting a continuous record of highly accurate infrared spectra with a wide variety of applications in geoscience. Al-though some research instrumentation early in the development of the meteorological satellite used Far-Infrared (FIR) sensitive detectors, the primary focus of infrared instrumentation has been the MIR region. Recent developments in FIR instrumentation and a renewed interest in the FIR for climate applications has brought attention to this underexplored part of Earth’s Infrared spectrum. The information content of Earth’s FIR spectrum is investigated within a modeling frame-work that simulates satellite observations of FIR and MIR spectra at hyperspectral resolution. The framework allows for direct comparison of the two spectral ranges, which can quantify the po-tential benefits of combining FIR spectral observations with the state of the art MIR observations. The framework is first applied to investigate the information content for retrieving the vertical tem-perature and water vapor profile in clear sky conditions. The FIR shows additional sensitivity to upper tropospheric and lower stratospheric water vapor, and a slight but consistent vertical resolu-tion advantage relative to the MIR. By extending the simulation framework to include layer clouds