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On the Changes in the Spectral Distribution of Kinetic Energy for Twodimensional, Nondivergent Flow

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Fjørtoft, Ragnar·1953·Tellus A: Dynamic Meteorology and Oceanography

Abstract

Total kinetic energy as well as total vorticity squared are integral quantitics which cannot change in the course of time in a twodimensional flow of a homogeneous, nondivergent, and inviscid fluid when the fluid is isolated from the surroundings. The case is considered where the fluid is defined over the total region of thc surface of a sphere. The nature of the changes in time of the spectral distribution of kinetic energy is discussed on the basis of the two conservation requirements mentioned above. It is found that only fractions of the initial energy can flow into sniallcr scales and that a greater fraction simultaneously has to flow to components with larger scales. The upper limits to the flow of kinetic energy into components with scales less than a given one are found. The conservation theorems are also used to discuss the stability of a certain stationary flow for a twodimensional motion which is not necessarily spherical. It is shown how important it is for the proof of stability that not only the kinetic energy of the disturbance is supposed to be small but also its vorticities.In chapter II molecular viscosity is taken into account for the spherical flow. Finally some conclusive remarks are offered regarding the fundamental difference between twoand threedimentional flow.

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Metadata

Authors
Fjørtoft, R.
Venue
Tellus A: Dynamic Meteorology and Oceanography
Published
1953-01-01
Volume
5
Issue
3
Pages
225-230
ISSN
  • 0280-6495 (ISSN-L)
  • 1600-0870
OpenAlex
W2080458140
Cited by
545
References
0
FWCI
1.27
Type
journal article
Language
en
Open access
hybrid

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CoChat. (2026). Citation check: On the Changes in the Spectral Distribution of Kinetic Energy for Twodimensional, Nondivergent Flow. https://app.cochat.ai/papers/10.3402/tellusa.v5i3.8647
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Fjørtoft, R. (1953). On the Changes in the Spectral Distribution of Kinetic Energy for Twodimensional, Nondivergent Flow. Tellus A: Dynamic Meteorology and Oceanography. https://doi.org/10.3402/tellusa.v5i3.8647

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