Cyclone Fengal: Tracking the Storm’s Path and Impact

When dealing with Cyclone Fengal, a powerful tropical cyclone that formed over the Indian Ocean in 2025 and produced heavy rain, strong winds, and widespread flooding along coastal districts, Fengal Cyclone, you instantly step into a web of related weather phenomena. Tropical cyclones, large low‑pressure systems that feed on warm sea surface temperatures to generate massive convection and rotation are the broader family that Fengal belongs to. Understanding this family helps explain why weather forecasting, the science of predicting atmospheric conditions using satellites, radar, and computer models becomes critical the moment a system like Fengal shows up in satellite imagery. Another key piece is storm surge, the abnormal rise in sea level caused by the cyclone’s wind pushing water onto the shore, which often accounts for the most damaging floods. Finally, climate change, the long‑term shift in global temperatures and weather patterns driven by greenhouse‑gas emissions sets the stage for more frequent and intense storms, making each new cyclone a case study in a changing world. Together these entities form a network: Cyclone Fengal encompasses tropical cyclone dynamics, requires accurate weather forecasting, intensifies storm surge risk, and is influenced by climate change.

From the moment Fengal organized as a tropical depression, meteorologists tracked its wind speeds, pressure drops, and sea‑surface temperature thresholds. The forecast models flagged a rapid intensification phase—a classic sign that a cyclone is entering the explosive growth window dictated by the energy budget of warm ocean water. As Fengal neared landfall, warning centers issued alerts that highlighted expected storm surge heights up to three meters, a figure derived from combining wind‑generated water displacement with the local bathymetry. Communities along the coast were advised to brace for coastal erosion, saltwater intrusion, and the cascading failures of power and communication grids. Parallel to the real‑time response, researchers examined Fengal’s structure to see how the ongoing trend of rising sea temperatures—one of the hallmarks of climate change—might have lowered the threshold for such rapid intensification. Their early findings suggest that a 0.5 °C increase in sea surface temperature can shave off several hours from the storm’s development timeline, giving residents even less preparation time. This feedback loop, where stronger storms fuel further climate stress, is a central concern for policymakers drafting resilient infrastructure plans.

Below you’ll find a curated set of articles that dive deeper into each of these angles: detailed breakdowns of Fengal’s meteorological data, practical guides on interpreting storm surge warnings, analyses of how climate change is reshaping cyclone behavior, and real‑world case studies of community response. Whether you’re a student studying weather systems, a local official preparing evacuation routes, or just a curious reader, the posts ahead provide actionable insights and up‑to‑date information on Cyclone Fengal and its broader context. Browse the collection to see how each piece fits into the larger puzzle of tropical cyclone science and disaster preparedness.