1963
DOI: 10.1007/bf02248000
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Local volcanic activity and ice nuclei concentrations on Hawaii

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Cited by 8 publications
(4 citation statements)
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“…Isono et al (1959) found at Tokyo, Japan, the concentration of IN (at −20 • C) to increase to up to 50 IN l −1 above the 5-20 IN l −1 background in air that had been affected by Japanese volcanoes located 110-1180 km upwind. Conversely, Price and Pales (1963) and Hobbs et al (1971) found no evidence for enhanced IN in volcanic effluents, when they sampled on the slopes of Mauna Loa, Hawaii. Measurements in the vicinity of volcanos from aircraft in the plumes of St. Augustine, Alaska (Schnell and Delany, 1976) and of Mt.…”
Section: Discussionmentioning
confidence: 94%
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“…Isono et al (1959) found at Tokyo, Japan, the concentration of IN (at −20 • C) to increase to up to 50 IN l −1 above the 5-20 IN l −1 background in air that had been affected by Japanese volcanoes located 110-1180 km upwind. Conversely, Price and Pales (1963) and Hobbs et al (1971) found no evidence for enhanced IN in volcanic effluents, when they sampled on the slopes of Mauna Loa, Hawaii. Measurements in the vicinity of volcanos from aircraft in the plumes of St. Augustine, Alaska (Schnell and Delany, 1976) and of Mt.…”
Section: Discussionmentioning
confidence: 94%
“…In addition to these surface-derived materials, volcanism is debated as a source of atmospheric ice nuclei. However, evidence for volcanic IN from field measurements of IN so far is conflicting (Isono et al, 1959;Price and Pales, 1963;Hobbs et al, 1971;Schnell and Delany, 1976;Radke et al, 1976). Satellite observations in the South Atlantic and North Pacific (Gasso, 2008) show that natural degassing or weakly explosive volcanoes affect low marine stratocumulus for up to 1300 km downwind by decreasing droplet effective radius and increasing visible brightness, and may add cloud cover in otherwise cloudless areas.…”
Section: Introductionmentioning
confidence: 99%
“…The signal of volcanic ash in our record of atmospheric IN at TO after the air masses had travelled for at least 2200 km is surprisingly pronounced, in particular when seen in the light of the so far inconclusive and conflicting observational evidence that had been available on volcanic ice nuclei. Isono et al (1959) found IN at Tokyo, Japan, (at −20 • C) to increase above the 5-20 IN L −1 background to up to 50 IN L −1 in air that had been affected by Japanese volcanoes located 110-1180 km upwind, whereas others found no evidence for volcanic IN in the effluents of Hawaiian volcanoes (Price and Pales, 1963;Hobbs et al, 1971), of St. Augustine, Alaska (Schnell and Delany, 1976), and of Mt. Baker, Washington (Radke et al, 1976).…”
Section: Resultsmentioning
confidence: 99%
“…Many components of atmospheric IN have been identified, such as minerals of desert dust, bacteria, pollen and plant debris (Pruppacher and Klett, 1997;Szyrmer and Zawadsky, 1997) although for many of them the concentrations and relevance to cloud processes are still unclear (Möhler et al, 2007;DeMott et al, 2010). In addition to these surface-derived sources, volcanism is debated as a source of atmospheric ice nuclei, with conflicting evidence from field measurements (Isono et al, 1959;Price and Pales, 1963;Hobbs et al, 1971;Schnell and Delany, 1976;Radke et al, 1976). Recent satellite observations (Gasso, 2008) show that natural degassing or weakly explosive volcanoes in the South Atlantic and North Pacific affect low marine stratocumulus for up to 1300 km downwind by decreasing droplet effective radius and increasing visible brightness, and may add cloud cover in otherwise cloudless areas.…”
Section: Introductionmentioning
confidence: 99%