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Spectroscopic inferences from HIS measurements of atmospheric thermal emissionRadiometrically accurate observations of the earth's emission spectrum from 3.8 to 16.6 microns have been made using the High-resolution Interferometer Sounder (HIS) to look downward from the NASA U2/ER2 aircraft or upward from the ground. These observations have been used to demonstrate the substantially improved vertical resolution of temperature and water vapor soundings derived from high resolution spectra (resolving power from 1800 to 3800), as compared to soundings from the low resolution filter radiometer observations used in current satellite sounders. The HIS observations have also demonstrated that Fourier Transform Infrared (FTIR) instruments are especially well suited to absolute emission measurements of broad spectral bands at high resolution. A fundamental advantage of FTIR instruments for accurate calibration is wavelength integrity, the same property which has made FTIR the standard for very high resolution absorption measurements. The long wavelength part of a HIS downwelling radiance spectrum is compared to a calculated spectrum. The calculation uses the AFGL HITRAN/86 line file and FASCOD2 line-by-line program with atmospheric state data from in situ measurements. In general, agreement between HIS and FASCOD2 spectra is remarkably good, a tribute to the current state of spectral line files and line-by-line codes. Reproducible differences between HIS observations and FASCOD2 line-by-line calculations lead to the following conclusions: (1) The FASCOD2 water vapor continuum in the longwave window region from 10 to 13 microns (750 to 1000 cm(exp -1)) gives reasonable agreement with radiance observations; (2) The model H2O continuum from 7 to 8 microns (1250 to 1425 cm(exp -2)) needs adjustment to reduce its contribution by about 60 percent; (3) CO2 absorption in the region from 13.1 to 14.3 microns (700 to 760 cm(exp -1)) is too small in the model; and (4) Water vapor line strengths in the region from 8.1 to 9.1 microns (1100 to 1230 cm(exp -1)) need to be increased about 30 percent.
Document ID
19920024852
Acquisition Source
Legacy CDMS
Document Type
Other
Authors
Revercomb, H. E.
(Wisconsin Univ. Madison, WI, United States)
Knuteson, R. O.
(Wisconsin Univ. Madison, WI, United States)
Smith, W. L.
(Wisconsin Univ. Madison, WI, United States)
Woolf, H. M.
(National Oceanic and Atmospheric Administration Madison, WI., United States)
Howell, H. B.
(National Oceanic and Atmospheric Administration Madison, WI., United States)
Date Acquired
September 6, 2013
Publication Date
December 1, 1991
Publication Information
Publication: Determination of Atmospheric Moisture Structure and Infrared Cooling Rates from High Resolution MAMS Radiance Data
Subject Category
Geophysics
Accession Number
92N34096
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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