Search Results - "Kelly, Samuel M."

Global Dynamics of the Stationary M2 Mode‐1 Internal Tide by Kelly, Samuel M., Waterhouse, Amy F., Savage, Anna C.

“…A reduced‐physics model is employed at 1/25° to 1/100° global resolution to determine (a) if linear dynamics can reproduce the observed low‐mode M2 internal…”
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Turbulence and high-frequency variability in a deep gravity current outflow by Nash, Jonathan D., Peters, Hartmut, Kelly, Samuel M., Pelegrí, Josep L., Emelianov, Mikhail, Gasser, Marc

“…Intensive sampling of the deep Mediterranean outflow 70 km W of the Strait of Gibraltar reveals a strong, tidally modulated gravity current embedded with…”
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Direct Observations of Coastally Generated Near‐Inertial Waves During a Wind Event by Kelly, Samuel M., Green, Erica L., Stokes, Ian A., Austin, Jay A., Lucas, Andrew J., Nash, Jonathan D.

“…Wind over the ocean generates near‐inertial velocities. In the open ocean, horizontal variability in the inertial frequency and mesoscale vorticity generate…”
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Internal‐tide interactions with the Gulf Stream and Middle Atlantic Bight shelfbreak front by Kelly, Samuel M., Lermusiaux, Pierre F. J.

“…Internal tides in the Middle Atlantic Bight region are found to be noticeably influenced by the presence of the shelfbreak front and the Gulf Stream, using a…”
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Are Any Coastal Internal Tides Predictable? by NASH, JONATHAN D., SHROYER, EMILY L., KELLY, SAMUEL M., INALL, MARK E., DUDA, TIMOTHY F., LEVINE, MURRAY D., JONES, NICOLE L., MUSGRAVE, RUTH C.

“…Surface tides are the heartbeat of the ocean. Because they are controlled by Earth's motion relative to other astronomical objects in our solar system, surface…”
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Global Dynamics of the Stationary M 2 Mode‐1 Internal Tide by Kelly, Samuel M., Waterhouse, Amy F., Savage, Anna C.

“…A reduced‐physics model is employed at 1/25° to 1/100° global resolution to determine (a) if linear dynamics can reproduce the observed low‐mode M 2 internal…”
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Tide-Topography Coupling on a Continental Slope by Kelly, Samuel M

“…Tide-topography coupling is important for understanding surface-tide energy loss, the intermittency of internal tides, and the cascade of internal-tide energy…”
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