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The Remarkable 2024 North Atlantic Mid-Season Hurricane Lull
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Original Article
The 2024 North Atlantic (hereafter Atlantic) hurricane season started
quickly, with the earliest Category 5 on record (Beryl) and three
hurricanes forming through 14 August. Following Ernesto’s dissipation on
20 August, the Atlantic hurricane season became extremely quiet during
the climatological peak of hurricane season, with only one Category 2
hurricane (Francine) and one tropical storm through 23 September.
Several environmental factors likely contributed to this unexpected,
prolonged lull. During mid-to-late August, subseasonal conditions were
broadly favorable for Atlantic hurricanes, but a northward shift in
African easterly wave emergence latitude yielded fewer TC seed
disturbances that traversed unfavorably cool ocean water. During
early-to-mid September, subseasonal variability driven by the
Madden-Julian oscillation was less conducive to hurricane activity, with
several bouts of increased vertical wind shear across the central
Atlantic. Throughout most of the lull, the tropical Atlantic was
anomalously dry and subsident, suppressing hurricane formation chances.
Wiley
Philip J Klotzbach
Emily Bercos-Hickey
Kimberly M. Wood
Carl J. Schreck III
Michael Bell
Eric S. Blake
Steven G. Bowen
Louis-Philippe Caron
Daniel Chavas
Jennifer M Collins
Ethan J. Gibney
Kurt Alexander Hansen
Andrew Hazleton
Jhordanne Jones
Michael Lowry
Angelie Nieves-Jimenez
Christina M Patricola
Levi G. Silvers
Ryan Eugene Truchelut
John Uehling
Title: The Remarkable 2024 North Atlantic Mid-Season Hurricane Lull
Description:
\papertype
Original Article
The 2024 North Atlantic (hereafter Atlantic) hurricane season started
quickly, with the earliest Category 5 on record (Beryl) and three
hurricanes forming through 14 August.
Following Ernesto’s dissipation on
20 August, the Atlantic hurricane season became extremely quiet during
the climatological peak of hurricane season, with only one Category 2
hurricane (Francine) and one tropical storm through 23 September.
Several environmental factors likely contributed to this unexpected,
prolonged lull.
During mid-to-late August, subseasonal conditions were
broadly favorable for Atlantic hurricanes, but a northward shift in
African easterly wave emergence latitude yielded fewer TC seed
disturbances that traversed unfavorably cool ocean water.
During
early-to-mid September, subseasonal variability driven by the
Madden-Julian oscillation was less conducive to hurricane activity, with
several bouts of increased vertical wind shear across the central
Atlantic.
Throughout most of the lull, the tropical Atlantic was
anomalously dry and subsident, suppressing hurricane formation chances.
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