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The vertical component of relative vorticity is given by :

  • A.\(Y = \frac{\delta u}{\delta x} + \frac{\delta v}{\delta y}\)
  • B.\(Y = \frac{\delta v}{\delta x} - \frac{\delta u}{\delta y}\)
  • C.\(Y = \frac{\delta u}{\delta x} - \frac{\delta v}{\delta y}\)
  • D.\(Y = \frac{\delta^{2} u}{\delta y^{2}} + \frac{\delta^{2} v}{\delta x^{2}}\)

Answer: B

The vertical component of relative vorticity is \(Y = \frac{\delta v}{\delta x} - \frac{\delta u}{\delta y}\) (the paper writes the vorticity as Y).

Relative vorticity is the curl of the wind, and its vertical component, usually written \(\zeta\), is

\[ \zeta = \partial v/\partial x - \partial u/\partial y \]

where \(u\) and \(v\) are the eastward and northward wind components. It is positive for anticlockwise rotation in the northern hemisphere.

The sum of \(\partial u/\partial x\) and \(\partial v/\partial y\) is the horizontal divergence, not vorticity. The difference \(\partial u/\partial x - \partial v/\partial y\) is a stretching deformation, and the sum of second derivatives is not a vorticity expression.

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