Intensification of Hurricane Idalia by a river plume in the eastern Gulf of Mexico

Hurricane Idalia formed on 26 August 2023 and three days later rapidly intensified from a Category 1 to Category 4 strength storm in less than 24 h over the west Florida shelf. On August 30, it made landfall along Florida’s Big Bend area as a Category 3 hurricane. Strikingly, despite Idalia’s modera...

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Main Authors: Jing Shi, Chuanmin Hu, Jennifer Cannizzaro, Brian Barnes, Yingjun Zhang, Chad Lembke, Matthieu Le Henaff
Format: Article
Language:English
Published: IOP Publishing 2025-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/adad8a
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author Jing Shi
Chuanmin Hu
Jennifer Cannizzaro
Brian Barnes
Yingjun Zhang
Chad Lembke
Matthieu Le Henaff
author_facet Jing Shi
Chuanmin Hu
Jennifer Cannizzaro
Brian Barnes
Yingjun Zhang
Chad Lembke
Matthieu Le Henaff
author_sort Jing Shi
collection DOAJ
description Hurricane Idalia formed on 26 August 2023 and three days later rapidly intensified from a Category 1 to Category 4 strength storm in less than 24 h over the west Florida shelf. On August 30, it made landfall along Florida’s Big Bend area as a Category 3 hurricane. Strikingly, despite Idalia’s moderate intensity and favorable vortex structure, neither upper ocean thermal energy nor environmental vertical wind shear conditions were as favorable during its intensification from Category 2 to Category 4 as earlier in its path, raising the question of what external factors contributed to its extreme intensification during this phase. Using satellite data, underwater glider observations, and numerical model outputs, this study reveals that, in addition to the 2023 marine heatwave, an extensive riverine plume in the eastern Gulf of Mexico, extending from the Mississippi-Alabama-Florida shelf to the Straits of Florida, produced a ∼20 m thick low-salinity layer (∼34–34.5 psu) and a corresponding warm upper ocean (>29 °C, ∼25–30 m thick). This defined a 10–20 m thick strongly stratified barrier layer below the surface layer with buoyancy frequencies exceeding 10 ^−3 s ^−1 that suppresses vertical mixing and became a critical factor contributing to Idalia’s rapid intensification under the relatively less than favorable thermal and wind field environments. Therefore, incorporating the river plume in future forecast models appears to be essential to improve the accuracy of intensity predictions, especially in the areas affected by the plume, where stratification plays an important role in the intensification dynamics.
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spelling doaj-art-3536503daad745d288ddc97baab47e5a2025-02-04T08:30:19ZengIOP PublishingEnvironmental Research Letters1748-93262025-01-0120202405010.1088/1748-9326/adad8aIntensification of Hurricane Idalia by a river plume in the eastern Gulf of MexicoJing Shi0https://orcid.org/0000-0002-3214-7440Chuanmin Hu1https://orcid.org/0000-0003-3949-6560Jennifer Cannizzaro2https://orcid.org/0000-0002-9536-6333Brian Barnes3https://orcid.org/0000-0003-0056-3500Yingjun Zhang4https://orcid.org/0000-0003-2079-5157Chad Lembke5Matthieu Le Henaff6https://orcid.org/0000-0001-5548-2543College of Marine Science, University of South Florida , St. Petersburg, FL, United States of AmericaCollege of Marine Science, University of South Florida , St. Petersburg, FL, United States of AmericaCollege of Marine Science, University of South Florida , St. Petersburg, FL, United States of AmericaCollege of Marine Science, University of South Florida , St. Petersburg, FL, United States of AmericaCollege of Marine Science, University of South Florida , St. Petersburg, FL, United States of AmericaCollege of Marine Science, University of South Florida , St. Petersburg, FL, United States of AmericaCooperative Institute for Marine and Atmospheric Studies (CIMAS), University of Miami , Miami, FL, United States of AmericaHurricane Idalia formed on 26 August 2023 and three days later rapidly intensified from a Category 1 to Category 4 strength storm in less than 24 h over the west Florida shelf. On August 30, it made landfall along Florida’s Big Bend area as a Category 3 hurricane. Strikingly, despite Idalia’s moderate intensity and favorable vortex structure, neither upper ocean thermal energy nor environmental vertical wind shear conditions were as favorable during its intensification from Category 2 to Category 4 as earlier in its path, raising the question of what external factors contributed to its extreme intensification during this phase. Using satellite data, underwater glider observations, and numerical model outputs, this study reveals that, in addition to the 2023 marine heatwave, an extensive riverine plume in the eastern Gulf of Mexico, extending from the Mississippi-Alabama-Florida shelf to the Straits of Florida, produced a ∼20 m thick low-salinity layer (∼34–34.5 psu) and a corresponding warm upper ocean (>29 °C, ∼25–30 m thick). This defined a 10–20 m thick strongly stratified barrier layer below the surface layer with buoyancy frequencies exceeding 10 ^−3 s ^−1 that suppresses vertical mixing and became a critical factor contributing to Idalia’s rapid intensification under the relatively less than favorable thermal and wind field environments. Therefore, incorporating the river plume in future forecast models appears to be essential to improve the accuracy of intensity predictions, especially in the areas affected by the plume, where stratification plays an important role in the intensification dynamics.https://doi.org/10.1088/1748-9326/adad8aHurricane Idaliaintensificationriver plumesalinityocean colorGulf of Mexico
spellingShingle Jing Shi
Chuanmin Hu
Jennifer Cannizzaro
Brian Barnes
Yingjun Zhang
Chad Lembke
Matthieu Le Henaff
Intensification of Hurricane Idalia by a river plume in the eastern Gulf of Mexico
Environmental Research Letters
Hurricane Idalia
intensification
river plume
salinity
ocean color
Gulf of Mexico
title Intensification of Hurricane Idalia by a river plume in the eastern Gulf of Mexico
title_full Intensification of Hurricane Idalia by a river plume in the eastern Gulf of Mexico
title_fullStr Intensification of Hurricane Idalia by a river plume in the eastern Gulf of Mexico
title_full_unstemmed Intensification of Hurricane Idalia by a river plume in the eastern Gulf of Mexico
title_short Intensification of Hurricane Idalia by a river plume in the eastern Gulf of Mexico
title_sort intensification of hurricane idalia by a river plume in the eastern gulf of mexico
topic Hurricane Idalia
intensification
river plume
salinity
ocean color
Gulf of Mexico
url https://doi.org/10.1088/1748-9326/adad8a
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