Adaptivity with moving grids
Adaptivity with moving grids
Adaptivity with moving grids
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120 C. J. Budd, W. Huang and R. D. Russell<br />
V<br />
θ<br />
9000<br />
9000<br />
8000<br />
8000<br />
7000<br />
7000<br />
z<br />
6000<br />
5000<br />
z<br />
6000<br />
5000<br />
4000<br />
4000<br />
3000<br />
3000<br />
2000<br />
2000<br />
1000<br />
1000<br />
−1 −0.5 0 0.5 1<br />
x<br />
x 10 6<br />
−5 0 5<br />
x<br />
x 10 5<br />
Figure 5.11. The (x, z) contours of the longitudinal velocity<br />
and potential temperature of the Eady problem close to the<br />
formation of a tropical storm.<br />
10000<br />
Arclength V monitor function<br />
10000<br />
Max eigenvalue monitor function<br />
9000<br />
9000<br />
8000<br />
8000<br />
7000<br />
7000<br />
z<br />
6000<br />
5000<br />
4000<br />
3000<br />
2000<br />
1000<br />
0<br />
−1 −0.5 0<br />
x<br />
0.5 1<br />
x 10 6<br />
z<br />
6000<br />
5000<br />
4000<br />
3000<br />
2000<br />
1000<br />
0<br />
−1 −0.5 0 0.5 1<br />
x<br />
x 10 6<br />
Figure 5.12. Two meshes adapted to the solution of the Eady<br />
problem presented above. In the first figure we use the arclength<br />
monitor function M 1 and in the second the potential vorticity<br />
monitor function M 2 .
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