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Relevant Books

114
Chedin, A., M. T. Chahine, and N. A. Scott (Eds), High Spectral Resolution Infrared Remote Sensing for Earth's Weather and Climate Studies, NATA ASI Series, 9, 492pp, 1993.

115
Hobbs, P. V., Aerosol-Cloud-Climate Interactions. Academic Press, New York, 233 pp, 1993.

116
Janssen, M. A., Atmospheric Remote Sensing by Microwave Radiometry. J. Wiley & Sons, New York, 572 pp., 1993.

117
Kunz, K. S., and R. J. Luebbers, The Finite Difference Time Domain Method for Electromagnetics. CRC Press, Florida, 448 pp, 1993.

118
Lenoble, J., Atmospheric Radiative Transfer. A. Deepak Publishing, Virginia, 532 pp.1993.

119
Liou, K. N., Radiation and Cloud Processes in the Atmosphere. Oxford Press, New York, 487 pp, 1992.

120
Mobley, C. D., Light and Water: Radiative Transfer in Natural Waters. Academic Press, California, 592 pp, 1994.

121
Stephens, G. L., Remote Sensing of the Lower Atmosphere: An Introduction. Oxford University Press, New York, 523 pp., 1994.

 
Figure 1: Profile of measured upwelling and downwelling clear sky longwave fluxes measured by radiometers flown on an unmanned aerospace vehicle (UAV) compared to line-by-line model calculations (courtesy of DOE ARM-UAV project).

 
Table 1: An example of spectral band divisions used to model the longwave and shortwave spectral and number of `monochromatic' calculations used in each band for gases given [ Fu and Liou, 1992].

Table 1. An example of spectral band divisions used to model the longwave and shortwave spectral and number of `monochromatic' calculations used in each band for gases given [ Fu and Liou, 1992]. ------------------------------------------------------------------------------ Number of Quadrature Points ------------------------------------------------------------------------------ Spectral HO region (Lines HO (CM) only) CO O CH NO (Continuum) ------------------------------------------------------------------------------ Infrared Spectrum 0-280 8 1 280-400 7 1 400-540 7 1 540-670 5 10 1 670-800 4 8 1 800-980 2 1 980-1100 1 5 1 1100-1250 3 1 1 1 1250-1400 4 1 1 1400-1700 4 1700-1900 3 1900-2200 2 Solar Spectrum 2500-2850 5 2850-4000 12 4000-5250 7 5250-7700 12 7700-14 500 8 ------------------------------------------------------------------------------


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U.S. National Report to IUGG, 1991-1994
Rev. Geophys. Vol. 33 Suppl., © 1995 American Geophysical Union