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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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Lambert reflector, there is no need to measure the brightness of<br />

targets <strong>and</strong> background with a photometer. At the same time, through<br />

the investigation of the properties of quasi-horizontal sky brightness<br />

<strong>and</strong> the reflective properties of airport's cement runways <strong>and</strong> white<br />

marks on the runway, he suggested the concept of "effective<br />

reflectivity"* According to this concept, low visibilitiesdess than<br />

2 kilometers) can be probed^.<br />

3* In the numerical research based on the double scattering<br />

lidar equation*- 21 J, the empirical correction of multiple scattering<br />

was made to the extinction coeficient*- *, so as to raise futher the<br />

probing precision of low visibility.<br />

4. By means of IAG frequency doubling technology^, we adopted<br />

a laser beam with a wavelength of 530 nm; it is closer to the<br />

chromolight that is most sensitive to the human eyes(550nm), so it is<br />

quite favourable for the improvement of probing precision of<br />

visibility.<br />

5. The validating experiments made at airports showed'- 22 *' that<br />

the correlation between the laser probed <strong>and</strong> human eye observed<br />

visibilities is as good as 0.93Cbased on 65 pairs of horizontal<br />

visibility samples). For various ranges of visibility, the errors are<br />

small enough to meet the requirements of aviation. When the<br />

visibility is less than 500 meters, average error is 44 meters. As to<br />

slant visibility, the comparing results of 21 pairs of samples are:<br />

the average error of laser probed visibility <strong>and</strong> human eye observed<br />

slant visual range is 10 percent; the maximum error is 33 percent*<br />

Only two pairs of samples exceed the limitation of aviation for<br />

probing precision of visibility(20 percent).<br />

173<br />

2. Multi-Parameter Remote Sensing of Aerosol Optical Properties<br />

Remote sensing of atmospheric aerosols is better than in-situ<br />

measurements in many situations. It can maintain the natural state of<br />

atmospheric aerosols, <strong>and</strong> produce timely <strong>and</strong> promptly the spatial <strong>and</strong><br />

temporal variation of aerosols. At present, the passive remote<br />

sensing of aerosols is mainly with the solar extinction

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