Field test of spectral line intensity parameters for tropospheric water vapor
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Stanley C. Solomon | B. Sierk | Andrew O. Langford | Seth I. Gutman | J. Daniel | S. Solomon | R. Portmann | S. Gutman | B. Sierk | Robert W. Portmann | John S. Daniel | A. Langford | C. S. Eubank | K. H. Holub | S. V. Florek | S. Florek | K. Holub
[1] Effects of improvements in near‐infrared water vapour line intensities on short‐wave atmospheric absorption , 2001 .
[2] V. Ramanathan,et al. Validation of visible/near-IR atmospheric absorption and solar emission spectroscopic models at 1 cm−1 resolution , 2000 .
[3] Albert Arking,et al. The influence of clouds and water vapor on atmospheric absorption , 1999 .
[4] T. Herring,et al. GPS Meteorology: Remote Sensing of Atmospheric Water Vapor Using the Global Positioning System , 1992 .
[5] David A. Newnham,et al. High‐resolution atmospheric absorption by water vapor in the 830–985 nm region: Evaluation of spectroscopic databases , 2001 .
[6] F. X. Kneizys,et al. Line shape and the water vapor continuum , 1989 .
[7] Bernd Sierk,et al. GPS‐meteorology: Impact of predicted orbits on precipitable water estimates , 1999 .
[8] S. Clough,et al. Dry Bias and Variability in Vaisala RS80-H Radiosondes: The ARM Experience , 2003 .
[9] Steven Businger,et al. GPS Meteorology: Direct Estimation of the Absolute Value of Precipitable Water , 1996 .
[10] J. Saastamoinen,et al. Contributions to the theory of atmospheric refraction , 1972 .
[11] J. Saastamoinen,et al. Introduction to practical computation of astronomical refraction , 1972 .
[12] Robert L. Kurucz,et al. The Solar Spectrum: Atlases and Line Identifications , 1995 .
[13] U. Platt,et al. Numerical analysis and estimation of the statistical error of differential optical absorption spectroscopy measurements with least-squares methods. , 1996, Applied optics.
[14] J. Saastamoinen. Contributions to the theory of atmospheric refraction , 1972 .
[15] W. B. Johnston,et al. A coolable long path absorption cell for laboratory spectroscopic studies of gases , 1994 .
[16] J. Haigh,et al. The contribution of unknown weak water vapor lines to the absorption of solar radiation , 1999 .
[17] W. J. van der Zande,et al. Evaluation of spectroscopic databases of water vapor between 585 and 600 nm , 2002 .
[18] Laurence S. Rothman,et al. Reprint of: The HITRAN molecular spectroscopic database and HAWKS (HITRAN Atmospheric Workstation): 1996 edition , 1998 .
[19] Jonathan Tennyson,et al. New studies of the visible and near‐infrared absorption by water vapour and some problems with the HITRAN database , 2000 .
[20] Christian Rocken,et al. GPS/STORM—GPS Sensing of Atmospheric Water Vapor for Meteorology , 1995 .
[21] Jonathan Tennyson,et al. The Water Vapor Spectrum in the Region 8600-15 000 cm(-1): Experimental and Theoretical Studies for a New Spectral Line Database. , 2001, Journal of molecular spectroscopy.
[22] Ulrich Platt,et al. Measurements of Atmospheric Trace Gases by Long Path Differential UV/Visible Absorption Spectroscopy , 1983 .
[23] Jonathan Tennyson,et al. Weak Line Water Vapor Spectra in the Region 13 200-15 000 cm -1 , 2002 .
[24] V. Ramanathan,et al. Warm Pool Heat Budget and Shortwave Cloud Forcing: A Missing Physics? , 1995, Science.
[25] Olga V. Naumenko,et al. The High-Resolution Spectrum of Water Vapor between 11 600 and 12 750 cm-1 , 1985, Journal of molecular spectroscopy.
[26] James B. Burkholder,et al. Absorption measurements of oxygen between 330 and 1140 nm , 1990 .
[27] Roderic L. Jones,et al. Absorption of solar radiation by water vapor in clear and cloudy skies: Implications for anomalous absorption , 2000 .
[28] C. H. Whitlock,et al. Absorption of Solar Radiation by Clouds: Observations Versus Models , 1995, Science.
[29] Simple Monte Carlo methods to estimate the spectra evaluation error in differential-optical-absorption spectroscopy. , 1999, Applied optics.
[30] Lawrence P. Giver,et al. Visible and near-infrared H216O line intensity corrections for HITRAN-96 , 2000 .
[31] R. Toth. Measurements of H216O line positions and strengths : 11 610 to 12 861 cm-1 , 1994 .
[32] Steven Businger,et al. GPS Meteorology: Mapping Zenith Wet Delays onto Precipitable Water , 1994 .