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  Static Stability
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The following equation provides the static stability:<br>
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  sigma=-(R/P)*(1000/P)<font size=-1><sup>-R/c<font size=-5><sub>p</sub>
  </font></sup></font>*(partial theta/partial p)
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<br><br>
<a href="theta.html">Potential temperature</a> was computed using Poisson's equation,
except at 1000 mb, where a lapse rate of 6.5K/km was used to bring the 850 mb
temperatures to 1000 mb using the 850 mb heights.
<br><br>
Partial theta/partial p is calculated using numerical differences. A forward
difference gives the static stability at 1000 mb:<br>
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  partial theta/partial p |<sub>p=p<font size=-1><sub>0</sub></font></sub>=
  [theta(p<font size=-1><sub>0</sub></font>+dp)-theta(p<font size=-1><sub>0</sub>
  </font>)]/dp
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<br>
A centered unequal difference gives the static stability at 850 mb and 500 mb:<br>
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  partial theta/partial p |<sub>p=p<font size=-1><sub>0</sub></font></sub>=
  [(dp<font size=-1><sub>2</sub></font>)theta(p<font size=-1><sub>0</sub>
  </font>+dp<font size=-1><sub>1</sub></font>)+(dp<font size=-1><sub>1</sub>
  </font>-dp<font size=-1><sub>2</sub></font>)theta(p<font size=-1><sub>0</sub>
  </font>)
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-(dp<font size=-1><sub>1</sub></font>)theta(p<font size=-1><sub>0</sub>
  </font>-dp<font size=-1><sub>2</sub></font>)]/(2*dp<font size=-1><sub>1</sub>
  </font>*dp<font size=-1><sub>2</sub></font>)
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At 200 mb, a backward difference gives the static stability:<br>
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  partial theta/partial p |<sub>p=p<font size=-1><sub>0</sub></font></sub>=
  [theta(p<font size=-1><sub>0</sub></font>)-theta(p<font size=-1><sub>0</sub>
  </font>-dp)]/dp
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  </p>
Units: m<font size=-1><sup>2</sup></font> s<font size=-1><sup>-2</sup></font> kPa<font size=-1><sup>-2</sup></font>
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