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The National Hurricane Center (NHC) noted an environment supportive of tropical development, and by September 27 a broad surface low developed amid the convection.
As the cold low drifted southward, a surface low developed on October 12.
A surface low developed on September 19, and it gradually organized as it moved westward.
An upper-level low developed over Texas, providing unfavorable amounts of vertical wind shear.
By 25 February, the low developed a banding feature in which the highest winds were located.
A tropical low developed southwest of Christmas Island on 28 February.
Similar(19)
Samples produced at low speeds developed low shrinkage stress, which decayed with time.
Some East coast lows develop rapidly, becoming meteorological bombs.
On June 7, small area of low pressure developed off the west coast of India.
These are low for developed countries.
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