Results 221 to 230 of about 331,405 (340)
K"ahler Geometry and the Navier-Stokes Equations
, 2005 Ian Roulstone +3 more
openalex +1 more source
On the Rotation‐Induced Pressure‐Strain Correlation in Rotating Boundary Layer Flows
Geophysical Research Letters, Volume 53, Issue 2, 28 January 2026.Abstract Rotation is a fundamental feature of many weather systems. The pressure‐strain correlation plays an important role in the Reynolds stress budget. However, the behavior of the pressure‐strain correlation under rotation remains insufficiently explored. This study develops a closure model for the rotation‐induced pressure‐strain correlation.
Xin Shao, Ning Zhang
wiley +1 more source
A stochastic Galerkin method with adaptive time-stepping for the Navier–Stokes equations
, 2022 Bedřich Sousedík, Randy Price
openalex +1 more source
Accurate projection methods for the incompressible Navier—Stokes equations
, 2001 David L. Brown, R. Cortez, M. Minion
semanticscholar +1 more source
Flow‐Dependent Inertial Permeability Defines Crossover Between Darcy and Forchheimer Flow Regimes
Geophysical Research Letters, Volume 53, Issue 2, 28 January 2026.Abstract We present mechanistic evidence that the Forchheimer inertial permeability coefficient (β $\beta $) is flow‐dependent in the weak‐to‐intermediate inertia crossover regime, governed by pore‐scale eddy growth‐to‐confinement dynamics. In contrast to classical theory, β $\beta $ attains steady‐state (βs ${\beta }_{s}$) asymptotically in the ...
Kuldeep Singh, Negin Sharifabad
wiley +1 more source
A semi-implicit augmented IIM for Navier-Stokes equations with open, traction, or free boundary conditions. [PDF]
J Comput Phys, 2015 Li Z, Xiao L, Cai Q, Zhao H, Luo R.
europepmc +1 more source
Growth Rate and Energy Dissipation in Wind‐Forced Breaking Waves
Geophysical Research Letters, Volume 53, Issue 1, 16 January 2026.Abstract We investigate the energy growth and dissipation of wind‐forced breaking waves at high wind speed using direct numerical simulations of the coupled air–water Navier–Stokes equations. A turbulent wind boundary layer drives the growth of a pre‐existing narrowband wave field until it breaks, transferring energy into the water column.
Nicolò Scapin +5 more
wiley +1 more source
The meshless local Petrov-Galerkin method based on moving Kriging interpolation for solving the time fractional Navier-Stokes equations. [PDF]
Springerplus, 2016 Thamareerat N +2 more
europepmc +1 more source