Transformation of internal solitary waves at the edge of ice cover
Abstract β β β ≈ 0 for ISWs. In the second series of experiments, a number of keels were located on the underside of the constant-thickness ice layer. The ISW transformation under ridged ice also depends on the blocking parameter β β < 0), more than 40 % of energy is lost on the first keel, while for relatively small keels (β > 0.3), the losses on the first keel are less than 6 %. Energy losses due to all keels depend on the distance between them, which is characterized by the parameter μ, i.e. the ratio of keel depth to the distance between keels. In turn, for a finite length of the ice layer, the distance between keels depends on the keel quantity.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Transformation of internal solitary waves at the edge of ice cover ; volume:31 ; number:2 ; year:2024 ; pages:207-217 ; extent:11
Nonlinear processes in geophysics ; 31, Heft 2 (2024), 207-217 (gesamt 11)
- Creator
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Terletska, Kateryna
Maderich, Vladimir
Tobisch, Elena
- DOI
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10.5194/npg-31-207-2024
- URN
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urn:nbn:de:101:1-2404250419152.650259030860
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 10:57 AM CEST
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Associated
- Terletska, Kateryna
- Maderich, Vladimir
- Tobisch, Elena
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