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14,340,000 Yen (FY1998; \4,989,000Yen)
The stratospheric aerosols, which affect the ozone chemistry through the heterogeneous reaction, were observed by the lidar at Wakkanai, Hokkaido, and at Kushiro,Hokkaido during winter. The amount of the stratospheric aerosols ejected by Mt.Pinatubo eruption was decreasing until 1996 and seems to become stable after 1997. Wavelength exponent of backscattering coefficient at 532nm and 1064nm became larger with time; particles with a radius smaller than 0.1μm seem to have become more predominant. The lidar system used at Kushiro was moved to Rikubetsu in November 1997 since observations from here were possible during the summer, and the system was improved to permit automatic observations.
lidar, stratospheric aerosols, backscattering coefficient