Wave signature in stratospheric aerosols

dc.contributor.author	Ackerman, M.
dc.contributor.author	Lippens, C.
dc.contributor.author	De Muer, D.
dc.date	1985
dc.date.accessioned	2017-06-27T11:33:47Z
dc.date.available	2017-06-27T11:33:47Z
dc.identifier.uri	https://orfeo.belnet.be/handle/internal/5863
dc.description	Regularly spaced vertical structures have been observed in stratospheric aerosols revealed by the observation of scattered sunlight. The simultaneous observations of this phenomenon and of regularly spaced vertical fluctuations of temperature is presented. The aerosol structure is interpreted in terms of particle size as a function of temperature on the basis of the limited theoretical studies available about the effects of temperature and humidity on the growth and optical properties of sulfuric acid‐water dropplets in the stratosphere.
dc.language	eng
dc.title	Wave signature in stratospheric aerosols
dc.type	Article
dc.subject.frascati	Earth and related Environmental sciences
dc.audience	Scientific
dc.source.title	Geophysical Research Letters
dc.source.volume	12
dc.source.issue	7
dc.source.page	445-447
Orfeo.peerreviewed	Yes
dc.identifier.doi	10.1029/GL012i007p00445
dc.identifier.scopus	2-s2.0-84984434637