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Turbulence structures in a non-stationary marine atmospheric boundary layer
Uppsala University, Disciplinary Domain of Science and Technology, Earth Sciences, Department of Meteorology.
1996 (English)Independent thesis Basic level (degree of Bachelor), 10 credits / 15 HE creditsStudent thesis
Abstract [en]

The vertical structure in the coastal marine atmosphere has been investigated using data from aircraft measurements performed along the Blekinge coast. The present data are from the third of October 1990. The main feature is fairly homogeneous horizontal conditions and a subceeing boundary layer which lowers from 600 meters down to about 50 meters during the day. The turbulence were found to be in a decreasing state. The turbulence parameters were normalized using normal stationary scaling, in order to compare with other results.

Place, publisher, year, edition, pages
1996. , p. 29
National Category
Meteorology and Atmospheric Sciences
Identifiers
URN: urn:nbn:se:uu:diva-392332OAI: oai:DiVA.org:uu-392332DiVA, id: diva2:1348016
Subject / course
Meteorology
Available from: 2019-09-03 Created: 2019-09-03 Last updated: 2019-09-03Bibliographically approved

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UlfAndrae_1996(2773 kB)3 downloads
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d593c930ae5c0a9f7de167b29b13116311d2fc66f0de1ba7d0c99a148481456d87308c670a939a6ec55afcf73157aa7fb3fc83f78c51a3bde8f726c9d4dd97a4
Type fulltextMimetype application/pdf

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