Examples of 'vertical wind shear' in a sentence

Meaning of "vertical wind shear"

Vertical wind shear: A meteorological term describing the change in wind direction or speed with altitude, which can affect the development and intensity of thunderstorms and tropical cyclones by tilting or tearing them apart

How to use "vertical wind shear" in a sentence

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vertical wind shear
Vertical wind shear began to weaken the storm thereafter.
This does not take into account vertical wind shear.
Vertical wind shear.
The system was located in a region of light vertical wind shear.
Limited vertical wind shear can be positive for tropical cyclone formation.
In combination with the low vertical wind shear in the forecast.
Vertical wind shear is a change in wind speed or direction with change in altitude.
That includes atmospheric instability and rotational vertical wind shear.
The atmosphere responds by generating vertical wind shear to maintain thermal wind balance.
The cyclone turned southwest and weakened into a tropical depression due to vertical wind shear.
A strong vertical wind shear should exist above the peak of the barrier.
Tropical Cyclone Veronica will continue to weaken quickly because of the strong vertical wind shear.
Large vertical wind shear disrupts a growing disturbance and can prevent a tropical cyclone from forming.
Soon, it began to dissipate due to increasing vertical wind shear.
Vertical wind shear persisted and Danielle soon began to weaken again.

See also

However, the surrounding moderate vertical wind shear prevented this.
The increasing vertical wind shear and cooler water caused Alma to weaken to a tropical storm.
That 's because the system is in an area of moderate vertical wind shear.
Dusty, that vertical wind shear is going to be wicked over those mountains.
At that time, the system was disorganized due to high vertical wind shear.
Downbursts create vertical wind shear or microbursts, which is dangerous to aviation.
That 's because the storm is dealing with moderate vertical wind shear.
The vertical wind shear in a tropical cyclone 's environment is very important.
Over the next couple of hours, vertical wind shear decreased gradually.
Upper level analysis indicates a favorable environment, with low vertical wind shear.
Since the storm was very small, vertical wind shear caused significant weakening thereafter.
The stronger the outflow boundary is, the stronger the resultant vertical wind shear becomes.
Thereafter, increasing vertical wind shear and passage over cooler water will weaken the system.
Fani moved northward, struggling to intensify as moderate vertical wind shear hampered its progress.
Vertical wind shear increased again, which combined with land interaction quickly weakened the tropical cyclone.
Almost as soon as it became a tropical storm, vertical wind shear began impacting the system.
The system tracked west-southwest, organizing slowly in the face of moderate vertical wind shear.
Dusty, that vertical wind shear The mighty Himalayas.
The stronger the outflow boundary is, the stronger the resultant vertical wind shear will become.
Vertical wind shear ( red ) sets air spinning green.
Thereafter, east-northeasterly winds aloft led to vertical wind shear which weakened Owen.
Moderate vertical wind shear from the northwest developed, disrupting Jerry 's upper-level outflow.
The next day, Bavi encountered unfavorable environments due to moderate to high vertical wind shear.
Vertical wind shear reached Lane on August 10, which led to weakening.
During the next day, Kilo started to encounter moderate vertical wind shear and started weakening.
The JTWC said vertical wind shear has increased to 25 to 30 knots.
Later that day, the system was caught in a moderate Vertical Wind Shear and started weakening.
On September 30, began to weaken due to cooler waters and increasing vertical wind shear.
BRN below 10, Strong vertical wind shear and weak CAPE.
Hours, a steady increase in south-southwesterly vertical wind shear.
Single-cell thunderstorms form in environments of low vertical wind shear and last only 20-30 minutes.
The area had favourable upper-level divergence, but high vertical wind shear.

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