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On recent (2008–2012) stratospheric aerosols observed by lidar over Japan

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Table 1. Characteristics of two-wavelength polarization lidar systems at Tsukuba and Saga.
Fig. 1. Vertical profiles of the backscattering ratio R (pink line) and total depolarization ratio δ (%) (blue line) at λ 2 = 532 nm over Tsukuba (upper panel) and Saga (lower panel) from June 2011 through January 2012
Fig. 2. Horizontal (upper panel) and vertical (lower panel) projections of isentropic forward trajectories of air parcels initially at an altitude of 17 km over Mt
Fig. 3. Monthly means of geopotential height (m) and wind (m s −1 ) on 100 hPa in June 2011 calculated from NCEP/NCAR reanalysis data
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