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Testing the Limits of Surface QG Theory With Deep Learning
Abstract Surface Quasi‐Geostrophic (SQG) theory provides a closed‐form mapping from surface buoyancy to interior stream function under the assumption that interior potential vorticity (PV) vanishes (Q=0) $(Q=0)$. In realistic flows, however, the interior PV is typically nonzero.
Wenyu Shan +5 more
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Distinct impacts of tropical North Atlantic warming flavors on cross-basin tropical cyclone activity. [PDF]
Zhao J +12 more
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Gyroid porous inserts as a novel flow control to mitigate tip vortex cavitation. [PDF]
Berger T, Farhat M.
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Stochastic resonance of rotating particles in turbulence. [PDF]
Wang Z +6 more
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Spin effects in superfluidity, neutron matter, and neutron stars. [PDF]
Sedrakian A, Rau PB.
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THz-induced phonon mode mixing and collective dynamics in a polar nanolattice
Skoropata E +15 more
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On the mass anomaly of potential vorticity vortices
Quarterly Journal of the Royal Meteorological Society, 2015The mass anomaly associated with piecewise constant symmetric potential vorticity (PV) vortices in rotating and stratified fluids is investigated. It is found that the absolute value of this mass anomaly depends linearly on the distance to the vortex centre and is therefore unbounded.
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Vorticity, Potential Vorticity
1992This lecture recalls the basic properties of vorticity and provides a summary of the main conservation laws associated with vorticity and its related quantities. It will be stated as clearly as possible how these different properties are used in industrial situations and in geophysical flows.
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