Trough Movement

300hPa contour chart for 20/0001 UTC

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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.

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Yes indeed the trough is sharpening. So what will this mean in terms of development?

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No. The stronger flow is upwind of the trough and the flow is mainly zonal. This will not result in the trough becoming stationary.

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No. The flow is mainly zonal it is therefore impossible for the trough to retrogress.

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As we have discovered the trough is diffluent. A confluent trough is required for relaxation.

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No. The strong flow on the upwind side the trough will not allow the trough to become stationary.

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No. The strong flow on the upwind side the trough will not allow the trough to retrogress.

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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.

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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.

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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.

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Yes, the trough will extend and progress.

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No. The strong flow on the upwind side of the trough means it is unlikely to become stationary.

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No. the flow is mainly zonal it is therefore imposible for the trough to retrogress.