Trough Movement |
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| How will the trough develop? Use the matrix below to best describe the evolution of the upper flow pattern over the next 6 hours. |
No. The stronger flow is upwind of the trough and the flow is mainly zonal. This will not result in the trough becoming stationary.
As we have discovered the trough is diffluent. A confluent trough is required for relaxation.
No. The strong flow on the upwind side the trough will not allow the trough to become stationary.
No. For the trough to disrupt the southern portion of a trough would advance, perhaps developing a cut-off circulation, whilst the opposite (residual) portion of the trough becomes quasi-stationary.
No. For the trough to disrupt the southern portion of a trough would advance, perhaps developing a cut-off circulation, whilst the opposite (residual) portion of the trough becomes quasi-stationary.
No. For the trough to disrupt the southern portion of a trough would advance, perhaps developing a cut-off circulation, whilst the opposite (residual) portion of the trough becomes quasi-stationary.