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Internal tide and solitons on the Scotian Shelf: A nutrient pump at work

Sandstrom, H., Elliott, J. A.·1984·Journal of Geophysical Research: Oceans

Abstract

During a measurement program on the Scotian Shelf off Nova Scotia, large amplitude internal waves were observed in the vicinity of the shelf edge. Some were identified positively as solitons. The observations provide insight into the soliton generation process and explain the role they play in the transfer of energy from tides to ocean mixing. It is found that the shoreward propagating energy in the baroclinic tide, which is generated at the shelf edge, is dissipated by way of the large‐amplitude, short internal waves. Based on observed dissipation rates of solitary waves, it is concluded that the associated amount of mixing is sufficient to supply the required nutrients to the euphotic zone.

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Metadata

Authors
Sandstrom, H., & Elliott, J. A.
Venue
Journal of Geophysical Research: Oceans
Published
1984-07-20
Volume
89
Issue
C4
Pages
6415-6426
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2073325260
Cited by
300
References
0
FWCI
12.16
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Internal tide and solitons on the Scotian Shelf: A nutrient pump at work. https://app.cochat.ai/papers/10.1029/jc089ic04p06415
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Sandstrom, H., & Elliott, J. A. (1984). Internal tide and solitons on the Scotian Shelf: A nutrient pump at work. Journal of Geophysical Research: Oceans. https://doi.org/10.1029/jc089ic04p06415

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.