Letter to the Editor: A strange cloud in the Arctic summer stratosphere 1998 above Esrange (68°N), Sweden

• Published in: Annales Geophysicae
• Main Authors: Siebert, J., Timmis, C., Vaughan, G., Fricke, K. H.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Verlag 2000
• Subjects: article; Verlagsveröffentlichung; Arctic; Canada; Esrange; Korovin; Aleutian Islands
• Online Access: https://doi.org/10.1007/s00585-000-0505-0; https://noa.gwlb.de/receive/cop_mods_00036792; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00036746/angeo-18-505-2000.pdf; https://angeo.copernicus.org/articles/18/505/2000/angeo-18-505-2000.pdf

When the University of Bonn lidar on the Esrange (68°N, 21°E), Sweden, was switched on in the evening of July 18, 1998, a geometrically and optically thin cloud layer was present near 14 km altitude or 400 K potential temperature, where it persisted for two hours. The tropopause altitude was 4 km below the cloud altitude. The cloud particles depolarized the lidar returns, thus must they have been aspherical and hence solid. Atmospheric temperatures near 230 K were approximately 40 K too high to support ice particles at stratospheric water vapour pressures of a few ppmv. The isentropic back trajectory on 400 K showed the air parcels to have stayed clear of active major rocket launch sites. The air parcels at 400 K had traveled from the Aleutians across Canada and the Atlantic Ocean arriving above central Europe and then turned northward to pass over above the lidar station. Parcels at levels at ±25 K from 400 K had come from the pole and joined the 400 K trajectory path above eastern Canada. Apparently the cloud existed in a filament of air with an origin different from those filaments both above and below. Possibly the 400 K level air parcels had carried soot particles from forest wild fires in northern Canada or volcanic ash from the eruption of the Korovin Volcano in the Aleutian Islands. Key words: Atmospheric composition and structure (aerosols and particles; biosphere-atmosphere interactions) · Meteorology and atmospheric dynamics (middle atmospheric dynamics)