Abstract
Condensation nuclei (CN) were measured in the free troposphere (FT) above the Jungfraujoch (JFJ) high-alpine research station (3454 m; Switzerland) from 4.5 to 12 km asl in a case study on July 30, 1997. Vertical profiles of CN concentration for d ≥ 5 nm (N≥5), d ≥ 15 nm (N≥15) were measured, and indicated that ultrafine CN (UCN; 5 ≤ d ≤ 15 nm; N5-15) exhibited a distinct increase with altitude. Some evidence for near-constant values of d(logCN)/dz within discrete layers was found, which generally coincided with different airmasses as delineated by changes in the lapse rate dθ/dz at ∼ 5.5, 6.4, 9.0 and 10.6 km asl. In addition, CN concentration was mapped over a 40 × 75 km horizontal domain at 8.0 km asl centered above the JFJ. A pronounced variation in N≥5, N≥15 and specific humidity, but not in UCN, exhibited quasi-stationary 2D features and was attributed to the chance encounter of a mountain wave. The case study provides further evidence that the upper FT may be a source of new particles. Copyright 1999 by the American Geophysical Union.
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CITATION STYLE
Nyeki, S., Kalberer, M., Lugauer, M., Weingartner, E., Petzold, A., Schröder, F., … Baltensperger, U. (1999). Condensation Nuclei (CN) and Ultrafine CN in the Free Troposphere to 12 km: A case study over the Jungfraujoch high-alpine research station. Geophysical Research Letters, 26(14), 2195–2198. https://doi.org/10.1029/1999GL900473
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