upd intro parabola, cleanup
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@@ -1,10 +1,12 @@
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Model Equations
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============================
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overview of PDE models to be used later on ...
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TODO
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give an overview of PDE models to be used later on ...
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continuous pde $\mathcal P^*$
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$\vx \in \Omega \subseteq \mathbb{R}^d$
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$\mathbf{x} \in \Omega \subseteq \mathbb{R}^d$
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for the domain $\Omega$ in $d$ dimensions,
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time $t \in \mathbb{R}^{+}$.
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@@ -47,11 +49,8 @@ and the abbreviations used inn: {doc}`notation`, at the bottom of the left panel
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% \newcommand{\corr}{\mathcal{C}} % just C for now...
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% \newcommand{\nnfunc}{F} % {\text{NN}}
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Some notation from SoL, move with parts from overview into "appendix"?
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We typically solve a discretized PDE $\mathcal{P}$ by performing discrete time steps of size $\Delta t$.
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Each subsequent step can depend on any number of previous steps,
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$\mathbf{u}(\mathbf{x},t+\Delta t) = \mathcal{P}(\mathbf{u}(\mathbf{x},t), \mathbf{u}(\mathbf{x},t-\Delta t),...)$,
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@@ -83,12 +82,13 @@ $\mathbf{u} = (u_x,u_y,u_z)^T$ for $d=3$.
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Burgers' equation in 2D. It represents a well-studied advection-diffusion PDE:
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$\frac{\partial u_x}{\partial{t}} + \mathbf{u} \cdot \nabla u_x =
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$\begin{aligned}
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\frac{\partial u_x}{\partial{t}} + \mathbf{u} \cdot \nabla u_x &=
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\nu \nabla\cdot \nabla u_x + g_x(t),
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\\
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\frac{\partial u_y}{\partial{t}} + \mathbf{u} \cdot \nabla u_y =
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\frac{\partial u_y}{\partial{t}} + \mathbf{u} \cdot \nabla u_y &=
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\nu \nabla\cdot \nabla u_y + g_y(t)
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$,
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\end{aligned}$,
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where $\nu$ and $\mathbf{g}$ denote diffusion constant and external forces, respectively.
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@@ -104,15 +104,15 @@ Later on, additional equations...
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Navier-Stokes, in 2D:
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$
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\frac{\partial u_x}{\partial{t}} + \mathbf{u} \cdot \nabla u_x =
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$\begin{aligned}
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\frac{\partial u_x}{\partial{t}} + \mathbf{u} \cdot \nabla u_x &=
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- \frac{1}{\rho}\nabla{p} + \nu \nabla\cdot \nabla u_x
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\\
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\frac{\partial u_y}{\partial{t}} + \mathbf{u} \cdot \nabla u_y =
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\frac{\partial u_y}{\partial{t}} + \mathbf{u} \cdot \nabla u_y &=
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- \frac{1}{\rho}\nabla{p} + \nu \nabla\cdot \nabla u_y
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\\
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\text{subject to} \quad \nabla \cdot \mathbf{u} = 0
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$
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\text{subject to} \quad \nabla \cdot \mathbf{u} &= 0
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\end{aligned}$
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@@ -121,28 +121,29 @@ Navier-Stokes, in 2D with Boussinesq:
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%$\frac{\partial u_x}{\partial{t}} + \mathbf{u} \cdot \nabla u_x$
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%$ -\frac{1}{\rho} \nabla p $
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$
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\frac{\partial u_x}{\partial{t}} + \mathbf{u} \cdot \nabla u_x = - \frac{1}{\rho} \nabla p
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$\begin{aligned}
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\frac{\partial u_x}{\partial{t}} + \mathbf{u} \cdot \nabla u_x &= - \frac{1}{\rho} \nabla p
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\\
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\frac{\partial u_y}{\partial{t}} + \mathbf{u} \cdot \nabla u_y = - \frac{1}{\rho} \nabla p + \eta d
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\frac{\partial u_y}{\partial{t}} + \mathbf{u} \cdot \nabla u_y &= - \frac{1}{\rho} \nabla p + \eta d
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\\
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\text{subject to} \quad \nabla \cdot \mathbf{u} = 0,
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\text{subject to} \quad \nabla \cdot \mathbf{u} &= 0,
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\\
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\frac{\partial d}{\partial{t}} + \mathbf{u} \cdot \nabla d = 0
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$
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\frac{\partial d}{\partial{t}} + \mathbf{u} \cdot \nabla d &= 0
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\end{aligned}$
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Navier-Stokes, in 3D:
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$
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\frac{\partial u_x}{\partial{t}} + \mathbf{u} \cdot \nabla u_x = - \frac{1}{\rho} \nabla p + \nu \nabla\cdot \nabla u_x
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\begin{aligned}
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\frac{\partial u_x}{\partial{t}} + \mathbf{u} \cdot \nabla u_x &= - \frac{1}{\rho} \nabla p + \nu \nabla\cdot \nabla u_x
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\\
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\frac{\partial u_y}{\partial{t}} + \mathbf{u} \cdot \nabla u_y = - \frac{1}{\rho} \nabla p + \nu \nabla\cdot \nabla u_y
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\frac{\partial u_y}{\partial{t}} + \mathbf{u} \cdot \nabla u_y &= - \frac{1}{\rho} \nabla p + \nu \nabla\cdot \nabla u_y
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\\
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\frac{\partial u_z}{\partial{t}} + \mathbf{u} \cdot \nabla u_z = - \frac{1}{\rho} \nabla p + \nu \nabla\cdot \nabla u_z
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\frac{\partial u_z}{\partial{t}} + \mathbf{u} \cdot \nabla u_z &= - \frac{1}{\rho} \nabla p + \nu \nabla\cdot \nabla u_z
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\\
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\text{subject to} \quad \nabla \cdot \mathbf{u} = 0.
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\text{subject to} \quad \nabla \cdot \mathbf{u} &= 0.
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\end{aligned}
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$
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