Abstract
A polar low development is described. The development started in a low-level shear zone in the Norwegian Sea on 29 February 1984. A large cloud cluster was built up. It broke up into several pieces. Two of these minor clusters moved closely together in the low-level wind field towards the south. When they reached a strong upper level shear zone near the Norwegian coast, they suddenly developed into a mature polar low.
DOI: https://doi.org/10.3402/tellusa.v39i4.11763 | Journal eISSN: 3035-9554
Language: English
Page range: 326 - 333
Submitted on: Jun 24, 1986
Accepted on: Oct 30, 1986
Published on: Jan 1, 1987
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1987 Åsmund Rabbe, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.