Results 41 to 50 of about 632,255 (202)
We formulate an idealised model of convective overshoots that hydrate the tropical tropopause layer. We consider large‐eddy simulations of a turbulent buoyant plume that penetrates into a stably stratified layer carrying temperature‐dependent tracers that represent water vapour and ice.
Charles W. Powell +2 more
wiley +1 more source
Macroscopic Convective Fluid Flows Arising From Binding of Ions and Small Molecules to Proteins
The interaction of ions or small molecules with proteins causes convective flows due to the displacement of water from the hydration shell. As shown, the replacement of the nickel ion removed from urease by EDTA pre‐treatment results in binding‐induced convective fluid flow.
Shanid Babu Shrestha +4 more
wiley +1 more source
Boussinesq-Peregrine water wave models and their numerical approximation
© 2020 Elsevier Inc. In this paper we consider the numerical solution of Boussinesq-Peregrine type systems by the application of the Galerkin finite element method.
Dimitrios Mitsotakis (8510154) +5 more
core +1 more source
Layered Radial Aquifer Model for Open‐Pit Mine Closure with Managed Aquifer Recharge
A radially symmetric layered aquifer model (unconfined–aquitard–confined) coupled to a pit‐lake water balance is developed to screen managed aquifer recharge (MAR) after open‐pit mine closure. Dimensionless type curves quantify trade‐offs between pit recovery time, pumping/recycling, and unconfined mounding as functions of aquifer time scales, aquitard
Behzad Ataie Ashtiani
wiley +1 more source
The two-dimensional films, flowing down an inclined, non-uniformly heated substrate are studied. The results contain the new mathematical models developed with the help of the long-wave approximation of the Navier-Stokes and heat transfer equations or ...
Goncharova Olga, Rezanova Ekaterina
doaj +1 more source
Approximation of ill-posed boussinesq equations [PDF]
In this paper we compare the dynamics on the centre manifold of the solutions of an ill-posed Boussinesq equation with a well-posed version. We show that the dynamics in the centre manifold of the ill-posed equation tracks the dynamics of the well-posed equation. Our results give partial justification to the long-wave perturbation theory.
Diogo A. Gomes, Claudia Valls
openaire +1 more source
Stability of Viscous Three‐Dimensional Stratified Couette Flow via Dispersion and Mixing
ABSTRACT This article explores the stability of stratified Couette flow in the viscous 3d$3d$ Boussinesq equations. In this system, mixing effects arise from the shearing background, and gravity acts as a restoring force leading to dispersive internal gravity waves.
Michele Coti Zelati +2 more
wiley +1 more source
A numerical investigation of high-Reynolds-number constant-volume non-Boussinesq density currents in deep ambient [PDF]
The time-dependent behaviour of non-Boussinesq high-Reynolds-number density currents, released from a lock of height h0 and length x0 into a deep ambient and spreading over horizontal flat boundaries, is considered.
S. BALACHANDAR +6 more
core +1 more source
Stability Estimates of Optimal Solutions for the Steady Magnetohydrodynamics-Boussinesq Equations
This paper develops the mathematical apparatus of studying control problems for the stationary model of magnetic hydrodynamics of viscous heat-conducting fluid in the Boussinesq approximation.
Gennadii Alekseev, Yuliya Spivak
doaj +1 more source
Scattering Of Internal Waves By Vertical Barrier In A Channel Of Stratified Fluid
The problem of two dimensional internal wave scattering by a vertical barrier in the form of a submerged plate, or a thin wall with a gap in an exponentially stratified fluid of uniform finite depth bounded by a rigid plane at the top, is considered in ...
P. Dolai
doaj +1 more source

