Geophysical and Astrophysical Fluid Dynamics

(The TQCC of Geophysical and Astrophysical Fluid Dynamics is 3. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2020-06-01 to 2024-06-01.)
Thermal versus isothermal rotating shallow water equations: comparison of dynamical processes by simulations with a novel well-balanced central-upwind scheme12
Linear water wave interaction with a composite porous structure in a two-layer fluid flowing over a step-like sea-bed11
Nonlinear wind-drift ocean currents in arctic regions9
Eastward-moving equatorial modons in moist-convective shallow-water models8
Instabilities and vertical mixing in river plumes: application to the Bay of Biscay7
Self-similar collapse of three geophysical vortices7
Different approaches in scattering of water waves by two submerged porous plates over an elastic sea-floor6
Generation of waves due to bottom disturbances in a viscous fluid6
On the limitations of magneto-frictional relaxation5
Experiments and long-term high-performance computations on amplitude modulations of strato-rotational flows5
Analysis of mixing structures in the Adriatic Sea using finite-size Lyapunov exponents5
Floating tracer clustering in divergent random flows modulated by an unsteady mesoscale ocean field5
Vortex–wall interaction on the β-plane and the generation of deep submesoscale cyclones by internal Kelvin Waves–current interactions4
Rotating thermal convection: surface turbulence observed with altimetry and thermal radiometry3
Approximation à la Oberbeck-Boussinesq for fluids with pressure-induced stratified density3
Angular momentum transfer in direct numerical simulations of a laboratory model of a tropical cyclone3
A geometric look at MHD and the Braginsky dynamo3
Viscoelastic Taylor–Couette instability in the Keplerian regime3
Rigorous results on conserved and dissipated quantities in ideal MHD turbulence3
Comments on: nonlinear wind-drift ocean currents in arctic regions3