Lidar observation of sudden increase of aerosols in the stratosphere caused by volcanic injections. II - Sierra Negra event

Physics

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Aerosols, Air Land Interactions, Atmospheric Scattering, Optical Radar, Particle Size Distribution, Stratosphere, Volcanoes, Backscattering, Meridional Flow, Particle Density (Concentration), Stratospheric Warming, Warm Fronts, Yag Lasers

Scientific paper

A striking disturbance in stratospheric aerosols over Fukuoka was observed by Nd-YAG laser radar in December 1979. It began with the appearance of a thin layer of enhanced scattering at an altitude of about 17 km and revealed remarkable variations of the layer in time and height. Measurements at two wavelengths suggest that the aerosols changed in size distribution, and the disturbance is inferred to be due to the Sierra Negra eruption. The integrated aerosol backscattering above the tropopause reached about 0.00008/sr, i.e., some six times that of the Soufriere event when converted to the ruby wavelength. The mean meridional transport speeds of the dust clouds were much larger than ever observed previously and this may be due to the activation of meridional transport associated with the Canadian sudden stratospheric warming in November-December 1979.

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