- COOLING
- ambient warm

- net-

cool - WARMING

particles | free surface u | free surface v |

dyeblob | interior u,v | interior w |

crystals | vertical u | bottom u,v,w |

tracer | short time | long time |
---|

\[\begin{aligned} \frac{\partial u_g}{\partial z} = -\frac{g}{f \rho_0}\hat{z} \times \nabla{\rho} \\ \end{aligned} \] \[\begin{aligned} u_g = \frac{1}{\rho f} \times \nabla{p} \\ \end{aligned} \]

\[\begin{aligned} R_0 = \frac{u}{fL} \\ \end{aligned} \]

315K | potential temperature [θ] | /cyan\ isosurface | denser fluid | -5°C | |

+40 m/s | west-to-east [u] jet flow | (blue) isosurface | u flow cyclonic (CCW) | +2.5 cm/s | |

5 m/s interval | + into the page | |white| contours | u (cyclonic) positive | .5 cm/s interval | |

5 m/s interval | - out of the page | |red| contours | u (anticyclonic) negative | .5 cm/s interval | |

Climate IDV - Polar Fronts and Jets Perpetual Ocean (2005-2007) |
Fronts Experiment: Cylinder Collapse - Virtual Lab Curious Properties of Rotating Fluids |

Weather in a Tank