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Detection of El Chichon volcanic aerosol in the antarctic stratosphere

Journal Article · · Antarct. J. U.S.; (United States)
OSTI ID:7120376
Following four major volcanic eruptions during the period from 1980 to 1982, culminating in that of El Chichon in Mexico in April 1982, the authors observed that sulfuric acid aerosol levels increased dramatically in the northern hemisphere. In addition, measurements at Laramie, Wyoming indicated that sulfuric acid condensation nuclei (radius equals approximately 0.01 micrometer) were being formed at altitudes of about 30 kilometers in the Arctic, well aster the eruptions. It was theorized that these nuclei were formed from volcanically derived sulfuric acid vapor during large, rapid temperature variations in the polar region, such as those that occur during the winter-spring season. In 1983 the authors proposed to return to Antarctica and conduct a single sounding at McMurdo as early in the summer season as possible. The purpose was twofold. First, they wanted to find out to what extent the El Chichon aerosol had reached the antarctic stratosphere, and second, they wanted to determine whether the proposed mechanism for aerosol production at 30 kilometers was operative over the Antarctic during the corresponding season (winter-spring). To do this in a single sounding, the largest balloon ever used in Antarctica (7230-cubic-meter volume) had to be launched under what was expected to be adverse weather conditions.
Research Organization:
Univ. of Wyoming, Laramie
OSTI ID:
7120376
Journal Information:
Antarct. J. U.S.; (United States), Journal Name: Antarct. J. U.S.; (United States) Vol. 19:5; ISSN AJUSA
Country of Publication:
United States
Language:
English