Long‐Lived Concentric Eyewalls in Numerically Simulated Typhoon Lekima (2019)

Abstract Typhoon Lekima (2019) exhibited a long‐lived concentric eyewall (LLCE) structure, which was successfully simulated using the Weather Research and Forecasting model. The simulation captured the LLCE, including a nearly steady inner eyewall and an expanding outer eyewall indicated by the radius of the maximum tangential wind (RMW). The RMW budget diagnostics reveal that the radial advection of momentum is balanced by the vertical advection of momentum and diffusion at the inner RMW. This dynamic balance maintains a near‐zero radial gradient of tangential wind tendency, thereby supporting a steady inner eyewall with a sharpening tangential wind profile. The inward‐propagating rainbands enhance tangential winds outside the outer eyewall, maintaining a positive radial gradient of tangential wind tendency and facilitating the outer RMW expansion. These processes produce a wide moat, which prolongs the duration of the CE by weakening the suppression of the outer eyewall on the inner eyewall.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-06-24
DOI
https://doi.org/10.1029/2025gl116192
Citations
1
Primary Topic
Tropical and Extratropical Cyclones Research
Type
article
Field-Weighted Citation Impact
1.30

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article

Long‐Lived Concentric Eyewalls in Numerically Simulated Typhoon Lekima (2019)

Nannan Qin, Qingyuan Liu
1 citations
Geophysical Research Letters
Tropical and Extratropical Cyclones Research
1.30
article

Long‐Lived Concentric Eyewalls in Numerically Simulated Typhoon Lekima (2019)

Nannan Qin, Qingyuan Liu
article en
1 citations

Abstract

Abstract Typhoon Lekima (2019) exhibited a long‐lived concentric eyewall (LLCE) structure, which was successfully simulated using the Weather Research and Forecasting model. The simulation captured the LLCE, including a nearly steady inner eyewall and an expanding outer eyewall indicated by the radius of the maximum tangential wind (RMW). The RMW budget diagnostics reveal that the radial advection of momentum is balanced by the vertical advection of momentum and diffusion at the inner RMW. This dynamic balance maintains a near‐zero radial gradient of tangential wind tendency, thereby supporting a steady inner eyewall with a sharpening tangential wind profile. The inward‐propagating rainbands enhance tangential winds outside the outer eyewall, maintaining a positive radial gradient of tangential wind tendency and facilitating the outer RMW expansion. These processes produce a wide moat, which prolongs the duration of the CE by weakening the suppression of the outer eyewall on the inner eyewall.

Geophysical Research LettersVol. 52(12)
Nanjing University of Information Science and Technology (CN), Jiangsu Institute of Meteorological Sciences (CN), Chinese Academy of Meteorological Sciences (CN)
National Natural Science Foundation of China, Government of Jiangsu Province, Natural Science Foundation of Jiangsu Province, Nanjing University of Information Science and Technology, Key Laboratory of Meteorological Disaster
Openalex Percentile: Top 21%
Tropical and Extratropical Cyclones Research
1.30
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Long‐Lived Concentric Eyewalls in Numerically Simulated Typhoon Lekima (2019) — Nannan Qin, Qingyuan Liu · Geophysical Research Letters (2025) | TGRS Research Map | TGRS