Abstract
This paper discusses the processes associated with the Central Asian trough in the winter system of planetary long waves. The case study has suggested that air from the convection layer over the Plateau of Iran ascended into the upper troposphere on the eastern side of a deep trough over Soviet Central Asia but the major process associated with the trough appears to have been the invasion of cold air masses from the north.
DOI: https://doi.org/10.3402/tellusa.v22i4.10233 | Journal eISSN: 3035-9554
Language: English
Page range: 399 - 402
Submitted on: Jan 12, 1970
Accepted on: Mar 2, 1970
Published on: Jan 1, 1970
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1970 J. M. Walker, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.