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During the latest Jurassic earliest Cretaceous (possibly the Tithonian early Berriasian), a series of north-trending structural highs and lows developed and extensive areas in the northern Porcupine Basin experienced folding, uplift and erosion.
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Some East coast lows develop rapidly, becoming meteorological bombs.
The National Hurricane Center (NHC) noted an environment supportive of tropical development, and by September 27 a broad surface low developed amid the convection.
On February 5, a tropical low developed in the Mozambique Channel.
A tropical low developed southwest of Christmas Island on 28 February.
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.
On 4 January, a tropical low developed within a monsoon trough over the Timor Sea.
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.
With favorable conditions, the low developed into a disturbance and soon into a depression on December 28.
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