Numerical studies indicate that interactions between ocean internal gravity waves (especially those <100 km) and geostrophic (or balanced) motions associated with mesoscale eddy turbulence (involving eddies of 100–300 km) impact the ocean's kinetic energy budget and therefore its circulation. Results from these studies have never been confirmed by observations in regional or basin‐scale domains. Here we show that internal gravity waves have a spectral signature on sea‐surface height (SSH) during summer that significantly differs from that of balanced motions. These spectral differences lead us to propose a new dynamical framework that quantifies the interactions between internal gravity waves and balanced motions in physical space from SSH ...
The dynamics of the ocean at a scale < 100km (fine-scales) is currently not well known. This is due ...
The generation of internal gravity waves in the ocean is largely driven by tides, winds, and interac...
High‐resolution global ocean models forced by atmospheric fields and tides are beginning to display ...
WOS:000483812500036International audienceNumerical studies indicate that interactions between ocean ...
Internal gravity waves (IGWs) and balanced motions (BMs) with scales < 100‐km capture most of the ve...
Understanding how kinetic energy (KE) is exchanged across scales and eventually dissipated remains a...
We study the mesoscale to submesoscale (10-300 km) dynamics of the upper ocean, with particular atte...
The dynamics of the ocean at a scale < 100km (fine-scales) is currently not well known. This is due ...
The ocean\u27s interior is filled with waves that can only exist because the ocean is vertically str...
AbstractWe aim to diagnose internal gravity waves emitted from balanced flow and investigate their r...
Internal gravity waves play a fundamental role in the dynamics of stably stratified regions of the ...
Internal gravity waves play a major role in the energetics of oceanic circulation. Powered by energy...
International audienceOceanic fronts with lateral scales less than 20 km are now known to be one of ...
The article offers information on the meeting “Interactions between Internal Gravity Waves and Meso/...
The dynamics of the ocean at a scale < 100km (fine-scales) is currently not well known. This is due ...
The generation of internal gravity waves in the ocean is largely driven by tides, winds, and interac...
High‐resolution global ocean models forced by atmospheric fields and tides are beginning to display ...
WOS:000483812500036International audienceNumerical studies indicate that interactions between ocean ...
Internal gravity waves (IGWs) and balanced motions (BMs) with scales < 100‐km capture most of the ve...
Understanding how kinetic energy (KE) is exchanged across scales and eventually dissipated remains a...
We study the mesoscale to submesoscale (10-300 km) dynamics of the upper ocean, with particular atte...
The dynamics of the ocean at a scale < 100km (fine-scales) is currently not well known. This is due ...
The ocean\u27s interior is filled with waves that can only exist because the ocean is vertically str...
AbstractWe aim to diagnose internal gravity waves emitted from balanced flow and investigate their r...
Internal gravity waves play a fundamental role in the dynamics of stably stratified regions of the ...
Internal gravity waves play a major role in the energetics of oceanic circulation. Powered by energy...
International audienceOceanic fronts with lateral scales less than 20 km are now known to be one of ...
The article offers information on the meeting “Interactions between Internal Gravity Waves and Meso/...
The dynamics of the ocean at a scale < 100km (fine-scales) is currently not well known. This is due ...
The generation of internal gravity waves in the ocean is largely driven by tides, winds, and interac...
High‐resolution global ocean models forced by atmospheric fields and tides are beginning to display ...