Hurricane Trudy held maximum sustained winds of 150 km/h (90 mph) as it tracked toward Mexico's western coast on Saturday, positioned roughly 305 km south-southeast of Manzanillo. The US National Hurricane Center issued a hurricane warning from Manzanillo in Colima state to Cabo Corrientes in Jalisco, with the storm forecast to approach the coast Saturday night before passing near it into Sunday. Forecasters warned it could strengthen further before beginning to weaken. The rainfall projections tell the real story. Trudy is expected to dump 10 to 20 cm of rain across Michoacan, Colima, and Jalisco, with isolated totals reaching 38 cm — roughly 15 inches — through the weekend. Outer rain bands could deliver an additional 5 to 10 cm in Guerrero and Nayarit. The NHC explicitly flagged life-threatening flooding and landslides, particularly in steep terrain. What converts a dangerous storm into a potential catastrophe is ground saturation. Colima state acknowledged that while current risk levels were assessed as low, successive storms hitting Mexico's Pacific coast this year have left the soil unable to absorb further rainfall. Every additional centimeter of rain now runs off rather than soaking in, dramatically amplifying flood and landslide risk beyond what Trudy's raw rainfall numbers suggest. The Mexican navy urged extreme caution for the maritime community and coastal residents, citing high waves, heavy rains, and the risk of rising river levels. Coastal flooding from storm surge was flagged for areas exposed to onshore winds, accompanied by large and destructive waves. Swells from Trudy were already affecting southwestern coastal areas and were expected to spread northward through the weekend. This is the structural problem. Mexico's Pacific coast is absorbing compounding storm damage with no recovery window between events. Each successive storm degrades infrastructure, saturates terrain, and reduces the system's capacity to handle the next one. Trudy is not an isolated event — it is the latest iteration in a pattern where cumulative exposure matters more than any single storm's category rating. The human cost concentrates predictably. Steep-terrain communities with limited drainage infrastructure, coastal populations dependent on fishing and tourism, and agricultural regions already battered by prior storms bear the overwhelming burden. The benefits of cheap coastal development accrue broadly; the costs of climate-amplified storm seasons fall on the people least equipped to absorb them. Trudy will weaken after Sunday. The pattern that produced it — warm Pacific waters, saturated soils, successive storms with diminishing recovery intervals — will not.
