Abstract
If there exists, in the spectrum of fluctuations of weather, a period of relatively low amplitude, and if a set of normal values of the right kind can be defined, then dynamical equations for the behaviour of the atmosphere can be used for the numerical prediction of charts meaned over the period of low amplitude.
DOI: https://doi.org/10.3402/tellusa.v6i1.8715 | Journal eISSN: 3035-9554
Language: English
Page range: 23 - 26
Published on: Jan 1, 1954
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1954 R. S. Scorer, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.
