New Zealand Simulation

This page describes a numerical simulation over New Zealand as an extension of the study New Zealand.

Computational Domain

The computation grid shown below uses horizontal mesh spacings of 1km in a uniform region near the surface. The vertical grid uses uniform spacing of 500 m to an altitude of 140 km. Stretching of ~2% is used past the uniform regions to the edge of the domain in each direction. The horizontal mesh is coarsened by a factor of 2 at three interfaces of altitudes 140, 200, 260 km. The resulting mesh at the top of the domain has a horizontal region with spacings of 8km.

surface
The location of the x-z plane animation is noted above.

Wind Profiles

Thermodynamic profiles displayed for data point located at 45.5°S, 170°E. This maps to (-11.2,-210.8) km in grid space, slightly SSE of Lauder (-36.8,-160.9).

winds

direction

direction

temperature

N^2

R

gamma

Forcing

A hyperbolic tangent forcing function gradually introduces winds near the surface with the objective of achieving the wind profile within a two hour period.

The following animations start at the end of the ramping period.

Results in xz plane





Results in an xy plane centered at Lauder (-36.8,-160.9)

u' at 65km


winds winds winds

winds winds winds

w' at 65km


winds winds winds

winds winds winds

T'/T'_bar at 65km


winds winds winds

winds winds winds

u' at 90km


winds winds winds

winds winds winds

w' at 90km


winds winds winds

winds winds winds

T'/T'_bar at 90km


winds winds winds

winds winds winds







Results in a high altitude xy plane


winds winds winds

winds winds winds



The Following Results are Taken at the Last Time Frame t~=6.83 hr

winds winds

winds winds



Averaged x Spectra


winds

winds