EGU26-5009, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-5009
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Wednesday, 06 May, 16:15–18:00 (CEST), Display time Wednesday, 06 May, 14:00–18:00
 
Hall A, A.51
A Vorticity-Based Indicator for Typhoon Intensity Forecasting
Pan Xia
Pan Xia
  • Sun Yat-sen University, School of Atmospheric Sciences, China (xiap3@mail2.sysu.edu.cn)

Accurate tropical cyclone (TC) intensity forecasting remains challenged due to the lack of high-spatiotemporal-resolution observations of inner-core dynamics. This study introduces a novel structural indicator, Area-Mean Vorticity (VORm), derived from minute-scale FY-4B atmospheric motion vectors using the SPA-FABI framework. We identify a distinct "U-shaped" lifecycle in vorticity variability, identifying anomalous high-frequency fluctuations as robust precursors for TC rapid intensity change. Integrating VORm into linear (MLR, R2=0.97, RMSE=5.239 kt) and non-linear (XGBoost, RMSE=5.778 kt) models significantly enhances 6-hour forecast skill, with VORm ranking as a top-tier indicator alongside other well-known dynamical and thermodynamic environmental drivers. In physical terms, a critical synergy is established: environmental factors such as sea surface temperature (SST) define the theoretical ceiling of potential intensity, while VORm quantifies the efficiency of the TC inner-core engine in realizing this potential. Furthermore, SHAP (Shapley Additive Explanation) analysis also reveals that VORm serves as a low-variance "anchor" signal, stabilizing predictions against environmental uncertainty. Operationally, VORm fills the critical gap for real-time, high-fidelity structural predictors, offering a novel and effective pathway to reduce short-term TC intensity forecast errors.

 

How to cite: Xia, P.: A Vorticity-Based Indicator for Typhoon Intensity Forecasting, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-5009, https://doi.org/10.5194/egusphere-egu26-5009, 2026.