Results 221 to 230 of about 28,122 (271)

Oceanic eddy with submesoscale edge drives intense air-sea exchanges and beyond. [PDF]

Sci Rep
Zhu R, Li M, Yang H, Ma X, Chen Z.
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High-resolution modeling of extreme heat events with socioeconomic consideration: a real-case WRF-LES approach. [PDF]

Environ Sci Pollut Res Int
Golbazi M, Liu F, Chen YH, Juliano TW, Richter H.   +4 more
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Turbulent isopycnal mixing dominates thermohaline transformations of intermediate ocean waters. [PDF]

Nat Commun
Sévellec F, Kolodziejczyk N, Portela E.
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Midlatitude mesoscale thermal Air-sea interaction enhanced by greenhouse warming. [PDF]

Nat Commun
Ma X, Zhang X, Wu L, Tang Z, Yang P, Song F, Jing Z, Chen H, Qu Y, Yuan M, Chen Z, Gan B.   +11 more
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How buoyancy-driven circulations shape momentum transport within the convective boundary layer: insights from Doppler lidar

Nuijens L, Neto JD.
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Atmospheric wind energization of ocean weather. [PDF]

Nat Commun
Rai S, Farrar JT, Aluie H.
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The joint effects of planetary <i>β</i>, topography and friction on baroclinic instability in a two-layer QG model. [PDF]

J Fluid Mech
Sterl MF, Palóczy A, Groeskamp S, Baatsen MLJ, LaCasce JH, Isachsen PE.   +5 more
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Unveiling diurnal metamorphosis in the atmospheric boundary layer during an annular solar eclipse through large eddy simulations. [PDF]

Sci Rep
Subrahamanyam DB.
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Vorticity budget analysis of a mesoscale convective vortex during the July 2022 flash flood in Northern Tehran. [PDF]

Sci Rep
Pegahfar N, Gharaylou M, Alizadeh O.
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Modeling mesoscale eddies

Ocean Modelling, 2005
Abstract Mesoscale eddies are not resolved in coarse resolution ocean models and must be modeled. They affect both mean momentum and scalars. At present, no generally accepted model exists for the former; in the latter case, mesoscales are modeled with a bolus velocity u ∗ to represent a sink of mean potential energy.
V.M Canuto, M.S Dubovikov
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