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File:Зіткнення внутрішніх хвиль із захопленими ядрами.tif

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Snapshots of numerical modeling of collision of internal solitary waves with trapped cores ( cores are visualized by dyed fluid (black and white)).

Summary

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Description
English: In the case of three-layer vertical fluid stratification internal solitary waves can develop recirculating regions, known as “trapped cores". Trapped cores in the ocean may transport mass, including particles as larvae and plankton. At the figure shown frontal collision of such waves, and “trapped cores" are marked by black and white dye. During collision large amplitude internal solitary waves with trapped cores are exposed by Kelvin–Helmholtz instability. More detail about internal solitary waves with trapped cores during collision can be found here: https://www.nonlin-processes-geophys.net/24/751/2017/npg-24-751-2017.pdf
Українська: У випадку тришарової вертикальної стратифікації рідини внутрішні хвилі можуть утворювати зони рециркуляції, відомі як 'захоплені ядра'. Захоплені ядра в океані можуть переносити масу, включно з частинками, такими як личинки та планктон. На малюнку зображено процес фронтального зіткнення таких хвиль, захоплені ядра зафарбовано чорним та білим барвником. Під час зіткнення внутрішні усамітнені хвилі великих амплітуд із захопленими ядрами зазнають нестікості Кельвіна-Гельмгольца. Більш детально про зіткнення внутрішніх хвиль із захопленими ядрами можна знайти тут https://www.nonlin-processes-geophys.net/24/751/2017/npg-24-751-2017.pdf
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Author Kterletska

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