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- Q7883828 subject Q6854368.
- Q7883828 subject Q7157108.
- Q7883828 abstract "In physical oceanography, undertow is the steady current – below the splash zone – which is moving offshore for waves approaching a shore. The undertow is the return flow which compensates for the onshore-directed mean mass flow in zone above the wave troughs. The undertow's flow velocities are generally strongest in the surf zone, where the water is shallow and the waves are high (due to shoaling). Undertow can be physically experienced as the offshore current pull that a person standing in the wave-breaking zone can feel most strongly near their feet, as each breaking wave advances towards them.In popular usage, an undertow is often confused with a rip current. While an undertow occurs everywhere under the shore-approaching waves, rip currents are strong and localized narrow currents occurring at certain locations along the coast.".
- Q7883828 thumbnail Buhr_Hansen_and_Svendsen_ICCE_1984_Fig_1.png?width=300.
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- Q7883828 wikiPageWikiLink Q6854368.
- Q7883828 wikiPageWikiLink Q7157108.
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- Q7883828 comment "In physical oceanography, undertow is the steady current – below the splash zone – which is moving offshore for waves approaching a shore. The undertow is the return flow which compensates for the onshore-directed mean mass flow in zone above the wave troughs. The undertow's flow velocities are generally strongest in the surf zone, where the water is shallow and the waves are high (due to shoaling).".
- Q7883828 label "Undertow (water waves)".
- Q7883828 depiction Buhr_Hansen_and_Svendsen_ICCE_1984_Fig_1.png.