Atmospheric Radiation: Progress and Prospects Proceedings of by Kuo-Nan Liou, Zhou Xiuji

By Kuo-Nan Liou, Zhou Xiuji

A selection of paperbounds offered on the Beijing foreign Radiation Symposium. The Symposium supplied a discussion board for clinical exchanges between scientists in China and out of the country within the fields of atmospheric radiation, distant sensing, and weather functions. The shows and discussions on the Symposium serious about the demanding situations and clients for atmospheric radiation relating to distant sensing, climate prediction and weather reviews.

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Additional resources for Atmospheric Radiation: Progress and Prospects Proceedings of the Beijing International Radiation Symposium Beijing, China, August 26–30, 1986

Example text

The empirical formula is written as follows (3) Q=Q0 Ca+b(1-fi)), one only from corrected daytime the in where fi is the ten-day mean cloud cover instanteneous cloud cover in the mid-afternoon (Shen et. , 1987), and Q is the mean ten-day total amount of global radiation at a 2° x 2° grid. , the western Plateau and the north side of Plateau. Table 2 gives correlation coefficients, empirical coefficients, and relative errors for both regions. Surface Albedo The weighted mean method that was designed by Xie (1984) and used in QXPMEX is used to determine the mean surface albedo at a 2° x 2° grid.

The accuracy could be improved by using additional data. But an accurate navigation is also required. Further, and possibly operational, analyses are highly desirable to obtain time series on the solar hPating of the Tibetan Plateau, but also of other areas seen from 50 Model Result. ,. , • At 2000 . t. / / . / / / ,, . =;;1 . ,. • ! / / / ·' '1 1000 J/cm 2 PYRANOMETER Fig. 4. MEASUREMENT Comparison between model results and ground-based measurements. Monthly averages of daily sums for 40 stations in July 1983.

High priority test areas include the western Pacific Ocean and the Tibetan Plateau. (2)Regional experimel)ts to develop and test new cloud and radiation parameterization methods for climate models. (3)Global and regional intercomparisons between climatologies of cloud parameters derived from satellites and from atmospheric general circulation models. (4)Systematic computations of the downward radiation flux over the ocean surface, based on visible and infrared radiance data from operational geostationary and low earth-orbit satellites.

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