Abstract
The following questions are central in studies of the global circulation:
-
Is the mean flow influenced by atmospheric waves like gravity waves or Rossby waves? And if so, how?
-
Vice versa, how does the mean flow influence the waves?
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Notes
- 1.
It is not required here that the streamfunction is real-valued. As we will see below, real-valued fields are obtained from superposing WKB solutions with opposite wavenumbers and with complex-conjugate amplitudes.
- 2.
A corresponding generalization is possible.
- 3.
Here the asterisk does not indicate the complex conjugate.
- 4.
In the mesosphere higher up small-scale gravity waves play the dominant role. In the present formulation their influence can be captured via corresponding forcing \(\langle F\rangle \ne 0\) and heating \(\langle Q\rangle \ne 0\).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
Copyright information
© 2022 Springer-Verlag GmbH Germany, part of Springer Nature
About this chapter
Cite this chapter
Achatz, U. (2022). The Interaction Between Rossby Waves and the Mean Flow. In: Atmospheric Dynamics. Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-63941-2_8
Download citation
DOI: https://doi.org/10.1007/978-3-662-63941-2_8
Published:
Publisher Name: Springer Spektrum, Berlin, Heidelberg
Print ISBN: 978-3-662-63940-5
Online ISBN: 978-3-662-63941-2
eBook Packages: Life Science and Basic Disciplines (German Language)