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Updated: May 23, 2026

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Published on: February 13, 2018
The wind- and wave-driven inner-shelf circulation
Steven J Lentz1, Melanie R Fewings
1Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA. slentz@whoi.edu
Inner continental shelf circulation is driven by tides, waves, and wind stress. These forces significantly impact marine ecosystems and transport materials between the coast and open ocean.
Area of Science:
- Oceanography
- Coastal dynamics
- Fluid mechanics
Background:
- The inner continental shelf is a dynamic region between the surf zone and the middle shelf.
- Circulation here is influenced by factors often overlooked in deeper waters.
Purpose of the Study:
- To review circulation and momentum balances on the inner continental shelf.
- To highlight the dominant roles of cross-shelf wind and surface gravity waves.
Main Methods:
- Literature review of prior and recent studies.
- Analysis of circulation drivers and momentum balances.
Main Results:
- Cross-shelf wind stress and surface gravity waves are dominant drivers of inner shelf circulation.
- Tides and buoyant plumes also contribute significantly to inner shelf dynamics.
Conclusions:
- Inner shelf circulation connects coastal and open ocean environments.
- Understanding these dynamics is crucial for predicting transport of pollutants, larvae, and nutrients.
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