Deterministic chaos at the ocean surface: applications and interpretations
Ocean surface, grazing-angle radar backscatter data from two separate experiments, one of which provided coincident time series of measured surface winds, were found to exhibit signatures of deterministic chaos. Evidence is presented that the lowest dimensional underlying dynamical system responsibl...
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Copernicus Publications
1998-01-01
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Series: | Nonlinear Processes in Geophysics |
Online Access: | http://www.nonlin-processes-geophys.net/5/13/1998/npg-5-13-1998.pdf |
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doaj-1b87ad8ff25840c28f9cb15f8723597e2020-11-24T23:02:55ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79461998-01-01511326Deterministic chaos at the ocean surface: applications and interpretationsA. J. PalmerC. W. FairallR. A. KropfliOcean surface, grazing-angle radar backscatter data from two separate experiments, one of which provided coincident time series of measured surface winds, were found to exhibit signatures of deterministic chaos. Evidence is presented that the lowest dimensional underlying dynamical system responsible for the radar backscatter chaos is that which governs the surface wind turbulence. Block-averaging time was found to be an important parameter for determining the degree of determinism in the data as measured by the correlation dimension, and by the performance of an artificial neural network in retrieving wind and stress from the radar returns, and in radar detection of an ocean internal wave. The correlation dimensions are lowered and the performance of the deterministic retrieval and detection algorithms are improved by averaging out the higher dimensional surface wave variability in the radar returns.http://www.nonlin-processes-geophys.net/5/13/1998/npg-5-13-1998.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
A. J. Palmer C. W. Fairall R. A. Kropfli |
spellingShingle |
A. J. Palmer C. W. Fairall R. A. Kropfli Deterministic chaos at the ocean surface: applications and interpretations Nonlinear Processes in Geophysics |
author_facet |
A. J. Palmer C. W. Fairall R. A. Kropfli |
author_sort |
A. J. Palmer |
title |
Deterministic chaos at the ocean surface: applications and interpretations |
title_short |
Deterministic chaos at the ocean surface: applications and interpretations |
title_full |
Deterministic chaos at the ocean surface: applications and interpretations |
title_fullStr |
Deterministic chaos at the ocean surface: applications and interpretations |
title_full_unstemmed |
Deterministic chaos at the ocean surface: applications and interpretations |
title_sort |
deterministic chaos at the ocean surface: applications and interpretations |
publisher |
Copernicus Publications |
series |
Nonlinear Processes in Geophysics |
issn |
1023-5809 1607-7946 |
publishDate |
1998-01-01 |
description |
Ocean surface, grazing-angle radar backscatter data from two separate experiments, one of which provided coincident time series of measured surface winds, were found to exhibit signatures of deterministic chaos. Evidence is presented that the lowest dimensional underlying dynamical system responsible for the radar backscatter chaos is that which governs the surface wind turbulence. Block-averaging time was found to be an important parameter for determining the degree of determinism in the data as measured by the correlation dimension, and by the performance of an artificial neural network in retrieving wind and stress from the radar returns, and in radar detection of an ocean internal wave. The correlation dimensions are lowered and the performance of the deterministic retrieval and detection algorithms are improved by averaging out the higher dimensional surface wave variability in the radar returns. |
url |
http://www.nonlin-processes-geophys.net/5/13/1998/npg-5-13-1998.pdf |
work_keys_str_mv |
AT ajpalmer deterministicchaosattheoceansurfaceapplicationsandinterpretations AT cwfairall deterministicchaosattheoceansurfaceapplicationsandinterpretations AT rakropfli deterministicchaosattheoceansurfaceapplicationsandinterpretations |
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1725634599646658560 |