Alternative Vertical Coordinates

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Presentation transcript:

Alternative Vertical Coordinates

Consider scalar A as a 4-d variable, using either z or s.

Consider

Note: now have “s” terms and “z” terms on opposite sides.

Then d/dt becomes

But

So then we can relate the vertical speeds

Horizontal momentum

But

So, horizontal momentum becomes

Pressure coordinate

Then with s=p,

Or

Continuity Equation

Change to p-coord. Key factor:

So

Mass continuity is then

Using pT = constant p top of atmosphere, and pH = surface pressure: Other coordinates Using pT = constant p top of atmosphere, and pH = surface pressure: