Effect of the North Equatorial Counter Current on the generation and propagation of internal solitary waves off the Amazon shelf (SAR observations)

Synthetic aperture radar (SAR) imagery from the Amazon shelf break region in the tropical west Atlantic reveals for the first time the two-dimensional horizontal structure of an intense Internal Solitary Wave (ISW) field, whose first surface manifestations are detected several hundred kilometres awa...

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Main Authors: J. M. Magalhaes, J. C. B. da Silva, M. C. Buijsman, C. A. E. Garcia
Format: Article
Language:English
Published: Copernicus Publications 2016-02-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/12/243/2016/os-12-243-2016.pdf
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spelling doaj-67b4acd7e16a4e458160d5f18a6be3ff2020-11-25T01:12:24ZengCopernicus PublicationsOcean Science1812-07841812-07922016-02-0112124325510.5194/os-12-243-2016Effect of the North Equatorial Counter Current on the generation and propagation of internal solitary waves off the Amazon shelf (SAR observations)J. M. Magalhaes0J. C. B. da Silva1M. C. Buijsman2C. A. E. Garcia3CIMAR/CIIMAR – Interdisciplinary Centre of Marine and Environmental Research & Department of Geosciences, Environment and Spatial Planning, University of Porto, Rua dos Bragas 289, 4050-123 Porto, PortugalCIMAR/CIIMAR – Interdisciplinary Centre of Marine and Environmental Research & Department of Geosciences, Environment and Spatial Planning, University of Porto, Rua dos Bragas 289, 4050-123 Porto, PortugalUniversity of Southern Mississippi, Department of Marine Science, 1020 Balch Blvd, Stennis Space Center, MS 39529, USAFederal University of Rio Grande, Av. Itália, 96201-900, Caixa Postal 474, Rio Grande, BrazilSynthetic aperture radar (SAR) imagery from the Amazon shelf break region in the tropical west Atlantic reveals for the first time the two-dimensional horizontal structure of an intense Internal Solitary Wave (ISW) field, whose first surface manifestations are detected several hundred kilometres away from the nearest forcing bathymetry. Composite maps and an energy budget analysis (provided from the Hybrid Coordinate Ocean Model – HYCOM) help to identify two major ISW pathways emanating from the steep slopes of a small promontory (or headland) near 44° W and 0° N, which are seen to extend for over 500 km into the open ocean. Further analysis in the SAR reveals propagation speeds above 3  m  s<sup>−1</sup>, which are amongst the fastest ever recorded. The main characteristics of the ISWs are further discussed based on a statistical analysis, and seasonal variability is found for one of the ISW sources. This seasonal variability is discussed in light of the North Equatorial Counter Current. The remote appearance of the ISW sea surface manifestations is explained by a late disintegration of the internal tide (IT), which is further investigated based on the SAR data and climatological monthly means (for stratification and currents). Acknowledging the possibility of a late disintegration of the IT may help explain the remote-sensing views of other ISWs in the world's oceans.http://www.ocean-sci.net/12/243/2016/os-12-243-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. M. Magalhaes
J. C. B. da Silva
M. C. Buijsman
C. A. E. Garcia
spellingShingle J. M. Magalhaes
J. C. B. da Silva
M. C. Buijsman
C. A. E. Garcia
Effect of the North Equatorial Counter Current on the generation and propagation of internal solitary waves off the Amazon shelf (SAR observations)
Ocean Science
author_facet J. M. Magalhaes
J. C. B. da Silva
M. C. Buijsman
C. A. E. Garcia
author_sort J. M. Magalhaes
title Effect of the North Equatorial Counter Current on the generation and propagation of internal solitary waves off the Amazon shelf (SAR observations)
title_short Effect of the North Equatorial Counter Current on the generation and propagation of internal solitary waves off the Amazon shelf (SAR observations)
title_full Effect of the North Equatorial Counter Current on the generation and propagation of internal solitary waves off the Amazon shelf (SAR observations)
title_fullStr Effect of the North Equatorial Counter Current on the generation and propagation of internal solitary waves off the Amazon shelf (SAR observations)
title_full_unstemmed Effect of the North Equatorial Counter Current on the generation and propagation of internal solitary waves off the Amazon shelf (SAR observations)
title_sort effect of the north equatorial counter current on the generation and propagation of internal solitary waves off the amazon shelf (sar observations)
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2016-02-01
description Synthetic aperture radar (SAR) imagery from the Amazon shelf break region in the tropical west Atlantic reveals for the first time the two-dimensional horizontal structure of an intense Internal Solitary Wave (ISW) field, whose first surface manifestations are detected several hundred kilometres away from the nearest forcing bathymetry. Composite maps and an energy budget analysis (provided from the Hybrid Coordinate Ocean Model – HYCOM) help to identify two major ISW pathways emanating from the steep slopes of a small promontory (or headland) near 44° W and 0° N, which are seen to extend for over 500 km into the open ocean. Further analysis in the SAR reveals propagation speeds above 3  m  s<sup>−1</sup>, which are amongst the fastest ever recorded. The main characteristics of the ISWs are further discussed based on a statistical analysis, and seasonal variability is found for one of the ISW sources. This seasonal variability is discussed in light of the North Equatorial Counter Current. The remote appearance of the ISW sea surface manifestations is explained by a late disintegration of the internal tide (IT), which is further investigated based on the SAR data and climatological monthly means (for stratification and currents). Acknowledging the possibility of a late disintegration of the IT may help explain the remote-sensing views of other ISWs in the world's oceans.
url http://www.ocean-sci.net/12/243/2016/os-12-243-2016.pdf
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