Hamiltonian fluid dynamics and distributed chaos
It is shown that distributed chaos with spontaneously broken time translational symmetry (homogeneity) has a stretched exponential frequency spectrum $E(f) \propto \exp-(f/f_0)^{1/2}$. Good agreement has been established with a laboratory experimental data obtained at large values of Rayleigh number...
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ftdatacite:10.48550/arxiv.1801.07655 2023-05-15T17:30:26+02:00 Hamiltonian fluid dynamics and distributed chaos Bershadskii, A. 2018 https://dx.doi.org/10.48550/arxiv.1801.07655 https://arxiv.org/abs/1801.07655 unknown arXiv arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Fluid Dynamics physics.flu-dyn FOS Physical sciences Preprint Article article CreativeWork 2018 ftdatacite https://doi.org/10.48550/arxiv.1801.07655 2022-04-01T10:04:06Z It is shown that distributed chaos with spontaneously broken time translational symmetry (homogeneity) has a stretched exponential frequency spectrum $E(f) \propto \exp-(f/f_0)^{1/2}$. Good agreement has been established with a laboratory experimental data obtained at large values of Rayleigh number $Ra \sim 3\cdot 10^{14}$ in thermal convection. Applications to geophysical fluid dynamics (temperature dynamics for large cities, the North Atlantic Oscillation index and the Pacific/North American pattern) have been considered. : New data have been added Report North Atlantic North Atlantic oscillation DataCite Metadata Store (German National Library of Science and Technology) Pacific |
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DataCite Metadata Store (German National Library of Science and Technology) |
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unknown |
topic |
Fluid Dynamics physics.flu-dyn FOS Physical sciences |
spellingShingle |
Fluid Dynamics physics.flu-dyn FOS Physical sciences Bershadskii, A. Hamiltonian fluid dynamics and distributed chaos |
topic_facet |
Fluid Dynamics physics.flu-dyn FOS Physical sciences |
description |
It is shown that distributed chaos with spontaneously broken time translational symmetry (homogeneity) has a stretched exponential frequency spectrum $E(f) \propto \exp-(f/f_0)^{1/2}$. Good agreement has been established with a laboratory experimental data obtained at large values of Rayleigh number $Ra \sim 3\cdot 10^{14}$ in thermal convection. Applications to geophysical fluid dynamics (temperature dynamics for large cities, the North Atlantic Oscillation index and the Pacific/North American pattern) have been considered. : New data have been added |
format |
Report |
author |
Bershadskii, A. |
author_facet |
Bershadskii, A. |
author_sort |
Bershadskii, A. |
title |
Hamiltonian fluid dynamics and distributed chaos |
title_short |
Hamiltonian fluid dynamics and distributed chaos |
title_full |
Hamiltonian fluid dynamics and distributed chaos |
title_fullStr |
Hamiltonian fluid dynamics and distributed chaos |
title_full_unstemmed |
Hamiltonian fluid dynamics and distributed chaos |
title_sort |
hamiltonian fluid dynamics and distributed chaos |
publisher |
arXiv |
publishDate |
2018 |
url |
https://dx.doi.org/10.48550/arxiv.1801.07655 https://arxiv.org/abs/1801.07655 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_rights |
arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ |
op_doi |
https://doi.org/10.48550/arxiv.1801.07655 |
_version_ |
1766126888963538944 |