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Converging Oceaniac Internal Waves, Somalia, Africa

The arculate fronts of these apparently converging internal waves off the northeast coast of Somalia (11.5N, 51.5E) probably were produced by interaction with two parallel submarine canyons off the Horn of Africa. Internal waves are packets of tidally generated waves traveling within the ocean at varying depths and are not detectable by any surface disturbance.

Date
1988-10-03
Collection
JSC
Archive
NASA Image and Video Library
Type
photograph

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Reason: a NASA work: not copyrighted in the United States.

Read from: NASA media usage guidelines: NASA material is not copyrighted in the US unless noted; no third-party credit or mark found.

Credit line

"Converging Oceaniac Internal Waves, Somalia, Africa" (1988-10-03). NASA/JSC. Public domain. https://images.nasa.gov/details/s26-42-015

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