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NavierStokesGleichung

Navier-Stokes-Gleichung, often called the Navier-Stokes equations, describe the motion of viscous, Newtonian fluids. They arise from conservation of mass and momentum and combine fluid inertia with viscous stresses.

In the incompressible case with constant density, the equations are ρ(∂u/∂t + (u·∇)u) = -∇p + μΔu + f, together

The system is solved with appropriate boundary conditions, commonly no-slip u=0 on solid boundaries, and an

Mathematically, the three-dimensional, time-dependent incompressible problem remains a central open question regarding global existence and smoothness;

In practice, numerical methods such as finite elements, finite volumes, and spectral methods are used, and turbulence

Applications span aerodynamics, weather and climate modeling, oceanography, engineering, and biomechanics. The name honors Claude-Louis Navier

with
∇·u
=
0.
Here
u
is
the
velocity
field,
p
is
pressure,
μ
is
dynamic
viscosity,
ρ
is
density,
and
f
represents
external
body
forces
such
as
gravity.
For
compressible
fluids
the
momentum
equation
includes
the
viscous
stress
tensor
τ
and
is
completed
by
an
equation
of
state.
initial
velocity
field
u(x,0).
It
is
a
nonlinear,
coupled
set
of
partial
differential
equations
in
space
and
time.
Leray’s
weak
solutions
exist,
but
regularity
in
general
is
unresolved.
In
three
dimensions,
this
issue
is
one
of
the
seven
Millennium
Prize
Problems
posed
by
the
Clay
Mathematics
Institute.
is
modeled
via
approaches
like
Reynolds-averaged
Navier-Stokes
(RANS)
or
Large
Eddy
Simulation
(LES).
and
George
Gabriel
Stokes;
the
German
term
Navier-Stokes-Gleichung
is
commonly
used
in
German-language
texts.