Rocky Mountain Simulations

This page describes a numerical simulation of gravity waves over the Rocky Mountains in Colorado.

Computational Domain

The layout of the of the simulation is shown in the figure below. Note that the computational domain (thin white line) is rotated at 7o with respect to lines of constant latitude.

domain


Just the computational domain is shown in the figure below. In this plot, and those that follow the results are shown in the computational frame. The terrain is damped around the domain edges in order to achieve a fixed elevation around the perimeter.

surface

The mesh is clustered in both horizontal directions in order to achieve 1000 x 1000 meter spacing over the mountain range in the region shown by the black rectangle. Very weak stretching is used so that the resolution is still ~1000 x 1000 m over the high planes east of the range. The domain extends to an altitude of 48 km and uses uniform vertical spacing of 1000 m. A total of 280 x 260 x 48 mesh points are used. Sponge layers are used on all external boundaries in order to absorb outgoing waves.

Wind and Thermodynamic Profiles

The mean winds and temperature profile are taken from radiosonde data, on three dates in February 2020, from a launch site in Grand Junction, Colorado. These profiles extend to an altitude slightly more than 30 km. A third order interpolating polynomial is then used to smoothly extend the winds above this altitude using the condition that U=V=0 at the upper boundary. Plots of various profiles for the three separate balloon measurements are shown below. Note that each profile is resampled on the 1000m mesh spacing.

Feb 01         Feb 10         Feb 20

winds winds winds

direction direction direction

temperature temperature temperature

Wind Condition


The mean winds near the surface are increased in time. Forcing terms gradually introduce winds near the surface with the objective of achieving the wind profile within a two hour period. A hyperbolic tangent function is used in order to produce gentle acceleration of the wind near the beginning and end of the forcing period. The maximum forcing rate is equivalent to that of a linear ramp with a duration of thirty minutes.

Results

Each animation is run for three simulation hours. u' and w' are shown for each wind profile.

Animation of u' in the xz plane at the position y = 0 km for winds Feb 01




Animation of w' in the xz plane at the position y = 0 km for winds Feb 01






Animation of u' in the xz plane at the position y = 0 km for winds Feb 10




Animation of w' in the xz plane at the position y = 0 km for winds Feb 10






Animation of u' in the xz plane at the position y = 0 km for winds Feb 20




Animation of w' in the xz plane at the position y = 0 km for winds Feb 20