This page describes a numerical simulation over New Zealand further extending the top of the domain from the study
New Zealand Zones.
Computational Domain
The computation grid shown below uses horizonal mesh spacings of 500 m 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 four interfaces of altitudes
140, 200, 260, 320 km.
Coarse Grid Comparison
A coarser grid with x-y spacing of 4km and 1km vertical in the unitform regions is used
for comparison. Only a single interface is used such that the grid spacing at the top of
the domain is the same as the full simulation.
The location of the x-z plane animation is noted above.
Wind Profiles
Winds profiles and time varyiation 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).
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.