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Chief Meteorologist David Paul explains how wind shear is affecting Hurricane Beryl

Until now, Beryl was in an optimal environment for development. That's changing.

HOUSTON — Conditions have to be perfect for a hurricane to reach Cat. 5 intensity. That's what happened on Monday as Hurricane Beryl's winds strengthened to 165 mph. 

To get this strong, the storm must be in an un-sheared environment with light upper-level winds. This allows the storm to become perfectly symmetrical and vertically stacked through the vertical atmosphere, with cyclonic inflow at the surface and un-disturbed anti-cyclonic outflow at the top of the system.

Credit: KHOU 11

Here's what that looks like, as Beryl was intensifying in an un-sheared environment on Monday. The storm is 'standing' straight up and down with no upper level wind shear to disturb the circulation.

Credit: KHOU 11

When hurricanes enter an environment in which the upper-level winds begin to blow, the system tilts and the circulation is disrupted.

Credit: KHOU 11

This process began on Tuesday as the storm moved into an area where the upper-level winds began to blow in from the southwest. This southwesterly 'wind shear' is already disrupting the circulation and weakening the storms' intensity. Pretty amazing how different Beryl looks on satellite Tuesday compared to Monday.

Credit: KHOU 11

 

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