Simulation of uplooking and downlooking high-resolution radiance spectra with two different radiative transfer models.

Measurements of up-looking spectral radiances measured during the Convection and Moisture Experiment and down-looking spectral radiances measured at one of the Atmospheric Radiation Measurement sites are compared with simulations with use of two different line-by-line models. Simulations are performed in tightly controlled conditions to verify the behavior of the models. Spectra computed at higher samplings are used to study the spectral structure of the differences between simulations and measurements. A revised list of water vapor spectroscopic parameters is used to test the impact of improved spectroscopic data on the accuracy of the line-by-line calculations. The sensitivity of the results to errors that result from uncertainties in the input atmospheric temperature and humidity profiles is also investigated.

[1]  Toth Air- and N(2)-Broadening Parameters of Water Vapor: 604 to 2271 cm(-1). , 2000, Journal of molecular spectroscopy.

[2]  Toth Air- and N(2)-Broadening Parameters of HDO and D(2)O, 709 to 1936 cm(-1). , 1999, Journal of molecular spectroscopy.

[3]  M. Matricardi,et al.  Fast radiative transfer model for simulation of infrared atmospheric sounding interferometer radiances. , 1999, Applied optics.

[4]  K. Jucks,et al.  Model, software, and database for computation of line-mixing effects in infrared Q branches of atmospheric CO2: II Minor and asymmetric isotopomers , 1999 .

[5]  A. A. Chursin,et al.  The 1997 spectroscopic GEISA databank , 1999 .

[6]  Robert A. Toth,et al.  HDO and D(sub 2)O Low Pressure, Long Path Spectra in the 600 to 3100cm Region. I. HDO Line Positions and Strength , 1999 .

[7]  R. Toth Air-and-N(sub 2) Broadening Parameters of HDO and D(sub 2O); 709 to 1936 cm(sup -1) , 1999 .

[8]  Toth Analysis of Line Positions and Strengths of H216O Ground and Hot Bands Connecting to Interacting Upper States: (020), (100), and (001). , 1999, Journal of molecular spectroscopy.

[9]  Laurence S. Rothman,et al.  Reprint of: The HITRAN molecular spectroscopic database and HAWKS (HITRAN Atmospheric Workstation): 1996 edition , 1998 .

[10]  Toth,et al.  Water Vapor Measurements between 590 and 2582 cm-1: Line Positions and Strengths. , 1998, Journal of molecular spectroscopy.

[11]  Laurence S. Rothman,et al.  The HITRAN molecular spectroscopic database and HAWKS (HITRAN atmospheric workstation) , 1998, Defense, Security, and Sensing.

[12]  P. Courtier,et al.  Extended assimilation and forecast experiments with a four‐dimensional variational assimilation system , 1998 .

[13]  Robert A. Toth,et al.  Self-broadened widths and frequency shifts of water vapor lines between 590 and 2400 cm−1 , 1998 .

[14]  S. Hannon,et al.  A compilation of first-order line-mixing coefficients for CO2 Q-branches , 1994 .

[15]  S. Schwartz,et al.  The Atmospheric Radiation Measurement (ARM) Program: Programmatic Background and Design of the Cloud and Radiation Test Bed , 1994 .

[16]  M. Susko,et al.  Operations summary for the convection and moisture experiment (CAMEX) , 1994 .

[17]  J. R. Eyre,et al.  Assimilation of TOVS radiance information through one-dimensional variational analysis , 1993 .

[18]  A Roblin,et al.  Collision-induced absorption in the fundamental band of N(2): temperature dependence of the absorption for N(2)-N(2) and N(2)-O(2) pairs. , 1993, Applied optics.

[19]  V. M. Devi,et al.  THE HITRAN MOLECULAR DATABASE: EDITIONS OF 1991 AND 1992 , 1992 .

[20]  Curtis P. Rinsland,et al.  Stratospheric infrared continuum absorptions observed by the ATMOS instrument , 1989 .

[21]  F. X. Kneizys,et al.  Line shape and the water vapor continuum , 1989 .

[22]  K. Masuda,et al.  Emissivity of pure and sea waters for the model sea surface in the infrared window regions , 1988 .

[23]  C. Boulet,et al.  Temperature dependence of the absorption in the region beyond the 4.3-microm band head of CO(2) . 2: N(2) and O(2) broadening. , 1985, Applied optics.

[24]  R. Rockafellar The multiplier method of Hestenes and Powell applied to convex programming , 1973 .

[25]  G. M. Hale,et al.  Optical Constants of Water in the 200-nm to 200-microm Wavelength Region. , 1973, Applied optics.

[26]  D. Friedman,et al.  Infrared Characteristics of Ocean Water (1.5-15 micro). , 1969, Applied optics.

[27]  P. Edwards,et al.  GENLN2: A general line-by-line atmospheric transmittance and radiance model. Version 3.0: Description and users guide , 1992 .

[28]  William L. Smith,et al.  HIS - A satellite instrument to observe temperature and moisture profiles with high vertical resolution , 1983 .

[29]  F. X. Kneizys,et al.  THEORETICAL LINE SHAPE FOR H 2 O VAPOR; APPLICATION TO THE CONTINUUM , 1980 .

[30]  B. Armstrong Spectrum line profiles: The Voigt function , 1967 .