Rapid Intensification of Hurricane Ian in Relation to Anomalously Warm Subsurface Water on the Wide Continental Shelf

Abstract Hurricane Ian rapidly intensified from Category 3 to 5 as it transited the wide West Florida Shelf (WFS). This is ascribed to heating by the anomalously warm shelf waters, despite the water depth being shallow when compared to the thicker, mixed layer areas of the deeper ocean. By examining...

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Main Authors: Yonggang Liu, Robert H. Weisberg, Luis Sorinas, Jason A. Law, Alexander K. Nickerson
Format: Article
Language:English
Published: Wiley 2025-01-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2024GL113192
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author Yonggang Liu
Robert H. Weisberg
Luis Sorinas
Jason A. Law
Alexander K. Nickerson
author_facet Yonggang Liu
Robert H. Weisberg
Luis Sorinas
Jason A. Law
Alexander K. Nickerson
author_sort Yonggang Liu
collection DOAJ
description Abstract Hurricane Ian rapidly intensified from Category 3 to 5 as it transited the wide West Florida Shelf (WFS). This is ascribed to heating by the anomalously warm shelf waters, despite the water depth being shallow when compared to the thicker, mixed layer areas of the deeper ocean. By examining temperature from long‐term moorings, we found that the sea surface and subsurface temperatures exceeded the climatologies by 1–2°C and 2–3°C, respectively. Additionally, these anomalously high temperatures in summer/fall of 2022 were related to the absence of Gulf of Mexico Loop Current interactions with the WFS slope at its “pressure point”. Without such offshore forcing to induce an upwelling circulation, the warmer waters on the shelf were not flushed and replaced by colder waters of deeper ocean origin. This work highlights the importance of subsurface temperature and ocean circulation monitoring on shallow continental shelves, which are largely overlooked in hurricane‐related ocean heat content observational programs.
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publishDate 2025-01-01
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spelling doaj-art-b94076d9945841d0a4a5764174d7eaa02025-01-20T13:05:57ZengWileyGeophysical Research Letters0094-82761944-80072025-01-01521n/an/a10.1029/2024GL113192Rapid Intensification of Hurricane Ian in Relation to Anomalously Warm Subsurface Water on the Wide Continental ShelfYonggang Liu0Robert H. Weisberg1Luis Sorinas2Jason A. Law3Alexander K. Nickerson4College of Marine Science University of South Florida St. Petersburg FL USACollege of Marine Science University of South Florida St. Petersburg FL USACollege of Marine Science University of South Florida St. Petersburg FL USACollege of Marine Science University of South Florida St. Petersburg FL USACollege of Marine Science University of South Florida St. Petersburg FL USAAbstract Hurricane Ian rapidly intensified from Category 3 to 5 as it transited the wide West Florida Shelf (WFS). This is ascribed to heating by the anomalously warm shelf waters, despite the water depth being shallow when compared to the thicker, mixed layer areas of the deeper ocean. By examining temperature from long‐term moorings, we found that the sea surface and subsurface temperatures exceeded the climatologies by 1–2°C and 2–3°C, respectively. Additionally, these anomalously high temperatures in summer/fall of 2022 were related to the absence of Gulf of Mexico Loop Current interactions with the WFS slope at its “pressure point”. Without such offshore forcing to induce an upwelling circulation, the warmer waters on the shelf were not flushed and replaced by colder waters of deeper ocean origin. This work highlights the importance of subsurface temperature and ocean circulation monitoring on shallow continental shelves, which are largely overlooked in hurricane‐related ocean heat content observational programs.https://doi.org/10.1029/2024GL113192Hurricane Ianrapid intensificationsubsurface water temperatureGulf of Mexico Loop currentWest Florida Shelfcoastal ocean observing ststem
spellingShingle Yonggang Liu
Robert H. Weisberg
Luis Sorinas
Jason A. Law
Alexander K. Nickerson
Rapid Intensification of Hurricane Ian in Relation to Anomalously Warm Subsurface Water on the Wide Continental Shelf
Geophysical Research Letters
Hurricane Ian
rapid intensification
subsurface water temperature
Gulf of Mexico Loop current
West Florida Shelf
coastal ocean observing ststem
title Rapid Intensification of Hurricane Ian in Relation to Anomalously Warm Subsurface Water on the Wide Continental Shelf
title_full Rapid Intensification of Hurricane Ian in Relation to Anomalously Warm Subsurface Water on the Wide Continental Shelf
title_fullStr Rapid Intensification of Hurricane Ian in Relation to Anomalously Warm Subsurface Water on the Wide Continental Shelf
title_full_unstemmed Rapid Intensification of Hurricane Ian in Relation to Anomalously Warm Subsurface Water on the Wide Continental Shelf
title_short Rapid Intensification of Hurricane Ian in Relation to Anomalously Warm Subsurface Water on the Wide Continental Shelf
title_sort rapid intensification of hurricane ian in relation to anomalously warm subsurface water on the wide continental shelf
topic Hurricane Ian
rapid intensification
subsurface water temperature
Gulf of Mexico Loop current
West Florida Shelf
coastal ocean observing ststem
url https://doi.org/10.1029/2024GL113192
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