In October 2021, cyclone Shaheen traversed northern Oman, bringing heavy rains along the coast and highlighting the vulnerability of arid regions to tropical storms. A team of researchers from Sultan Qaboos University used this event as a test case to explore how warming waters and local topography influence cyclone simulations, particularly in terms of intensity, trajectory, and rainfall distribution.
What the study reveals: Precise results and key figures
Simulations show that as sea surface temperature (SST) increases, the model predicts intensified convection at the cyclone's core, resulting in heavier rainfall over coastal areas. Furthermore, Oman's mountainous topography, characterized by abrupt ranges rising rapidly from the coastline, alters air flow and leads to notable differences in the simulated cyclone trajectory. Thus, variations of a few degrees in SST and adjustments in topography can shift the cyclone's path by tens of kilometers, radically altering the areas most affected by downpours.
These differences are particularly pronounced when comparing standard ECMWF simulations with those enriched by Copernicus satellite data and advanced neural network models like GraphCast and Pangu-Weather. Machine learning models better capture fine-grained interactions between atmospheric humidity and oceanic heat, reducing prediction uncertainty related to cloud formation processes and surface dynamics.
