Abstract
Solar irradiances, atmospheric turbidity and meteorological variables measured at the University of Michigan are analyzed to determine effects of the 30 m wind direction on irradiance and turbidity changes caused by the El Chichon volcanic cloud. Results for the period with the largest volcanic effects, from 26 October 1982 through mid-June 1983, are compared with results for the same eight-month period in 1979--1980, 1980--1981, 1981--1982 and 1983--1984.
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