The 5-6 December 1991 FIRE IFO II jet stream cirrus case study: Possible influences of Volcanic Aerosols

• Published in: Journal of the atmospheric sciences 1995-01, Vol.52 (1), p.97-123
• Main Authors: Sassen, Kenneth, Starr, David O'C., Mace, Gerald G., Poellot, Michael R., Melfi, S. H., Eberhard, Wynn L., Spinhirne, James D., Eloranta, E. W., Hagen, Donald E., Hallett, John
• Format: Article
• Language: English
• Subjects: Earth, ocean, space; Environment Pollution; Exact sciences and technology; External geophysics; General properties of the high atmosphere; Physics of the high neutral atmosphere
• ISSN: 0022-4928; 1520-0469
• DOI: 10.1175/1520-0469(1995)052<0097:TDFIIJ>2.0.CO;2

In presenting an overview of the cirus clouds comprehensively studied by ground-based and airborne sensors from Coffeyville, Kansas, during the 5-6 December 1992 Project First ISCCP Region Experiment (FIRE) Intensive Fields Observation (IFO) II case study period, evidence is provided that volcanic aerosols friom the June 1991 Pinatubo eruptions may have significantly influenced the formation and maintenance of the cirrus. Following the local appearance of a spur of stratospheric volcanic debris from the subtropics, a series of jet streaks subsequently conditioned the troposphere through tropopause foldings with sulfur-based particles that became effective cloud-forming nuclei in cirrus clouds. Aerosol and ozone measurements suggest a complicated history of stratospheric-tropospheric exchanges embedded within the upper-level flow, and cirrus cloud formation was noted to occur locally at the boundaries of stratospheric aerosol-enriched layers that became humidified through diffusion, precipitation, or advective processes. Apparent cirrus cloud alterations include abnormally high ice crystal concentrations (up to approximately 600/L), complex radial ice crystal types, and relatively large haze particles in cirrus uncinus cell heads at temperatures between -40 and -50 C. Implications for volcanic-cirrus cloud climate effects and usual (nonvolcanic aerosol) jet stream cirrus cloud formation are discussed.