The Near‐Surface Boundary Layer of Hurricane Laura (2020) at Landfall

Abstract While challenging, quantification of the near‐surface landfalling hurricane wind field is necessary for understanding hurricane intensity changes and damage potential. Using single‐ and dual‐Doppler Doppler on Wheels and in situ anemometer data, the wind structure of the very near‐surface b...

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Main Authors: Karen Ann Kosiba, Joshua Wurman, Paul Robinson
Format: Article
Language:English
Published: Wiley 2025-05-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2025GL114746
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author Karen Ann Kosiba
Joshua Wurman
Paul Robinson
author_facet Karen Ann Kosiba
Joshua Wurman
Paul Robinson
author_sort Karen Ann Kosiba
collection DOAJ
description Abstract While challenging, quantification of the near‐surface landfalling hurricane wind field is necessary for understanding hurricane intensity changes and damage potential. Using single‐ and dual‐Doppler Doppler on Wheels and in situ anemometer data, the wind structure of the very near‐surface boundary layer of Hurricane Laura (2020) is characterized. Small‐scale hurricane boundary layer (HBL) rolls (HBLRs) with a median size of approximately 400 m are present throughout much of the landfall, but are most vigorous in the eyewall. The maximum turbulent kinetic energy (TKE) and momentum flux associated with HBLRs occur in the eyewall and are much larger than previously documented at landfall. DOW‐derived and anemometer‐derived TKE values are comparable. Observed maximum surface gusts were consistent with the maximum radar wind speeds aloft, suggesting the importance of vertical transport within the HBL by sub‐kilometer scale structures for the enhancement of surface wind speeds.
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spelling doaj-art-49380e7c16a04cbab811cda7875005bc2025-08-20T02:17:01ZengWileyGeophysical Research Letters0094-82761944-80072025-05-01529n/an/a10.1029/2025GL114746The Near‐Surface Boundary Layer of Hurricane Laura (2020) at LandfallKaren Ann Kosiba0Joshua Wurman1Paul Robinson2University of Alabama in Huntsville Huntsville AL USAUniversity of Alabama in Huntsville Huntsville AL USAUniversity of Alabama in Huntsville Huntsville AL USAAbstract While challenging, quantification of the near‐surface landfalling hurricane wind field is necessary for understanding hurricane intensity changes and damage potential. Using single‐ and dual‐Doppler Doppler on Wheels and in situ anemometer data, the wind structure of the very near‐surface boundary layer of Hurricane Laura (2020) is characterized. Small‐scale hurricane boundary layer (HBL) rolls (HBLRs) with a median size of approximately 400 m are present throughout much of the landfall, but are most vigorous in the eyewall. The maximum turbulent kinetic energy (TKE) and momentum flux associated with HBLRs occur in the eyewall and are much larger than previously documented at landfall. DOW‐derived and anemometer‐derived TKE values are comparable. Observed maximum surface gusts were consistent with the maximum radar wind speeds aloft, suggesting the importance of vertical transport within the HBL by sub‐kilometer scale structures for the enhancement of surface wind speeds.https://doi.org/10.1029/2025GL114746hurricane windstropical cyclone winds
spellingShingle Karen Ann Kosiba
Joshua Wurman
Paul Robinson
The Near‐Surface Boundary Layer of Hurricane Laura (2020) at Landfall
Geophysical Research Letters
hurricane winds
tropical cyclone winds
title The Near‐Surface Boundary Layer of Hurricane Laura (2020) at Landfall
title_full The Near‐Surface Boundary Layer of Hurricane Laura (2020) at Landfall
title_fullStr The Near‐Surface Boundary Layer of Hurricane Laura (2020) at Landfall
title_full_unstemmed The Near‐Surface Boundary Layer of Hurricane Laura (2020) at Landfall
title_short The Near‐Surface Boundary Layer of Hurricane Laura (2020) at Landfall
title_sort near surface boundary layer of hurricane laura 2020 at landfall
topic hurricane winds
tropical cyclone winds
url https://doi.org/10.1029/2025GL114746
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