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Table 1.
Interpolation and extrapolation used to construct the atmosphere from given nodes.
| Parameter | Interpolation | Top | Bottom |
|---|---|---|---|
| T | Bezier | Linear | Linear* |
| v | Bezier | Constant | Linear |
| B | Bezier | Constant | Linear |
| θB, ϕB | Bezier | Constant | Constant |
Notes. The temperature at the bottom of the atmosphere is extrapolated linearly so that its temperature gradient is parallel to the temperature gradient of the semi-empirical FALC model atmosphere (Fontenla et al. 1993).
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