Typhoon Nina Devastates the Philippines (1987)

November 25, 1987

On November 25, 1987, Typhoon Nina roared ashore in Southern Luzon, Philippines, packing catastrophic category 5 winds of 265 km/h (165 mph). Known locally as Typhoon Sisang, the storm's ferocious winds and towering storm surge obliterated entire coastal villages, leaving at least 1,036 people dead. It remains one of the deadliest typhoons to strike the Philippine archipelago in the twentieth century.

From Tropical Disturbance to Monster Typhoon

Typhoon Nina began as an unremarkable area of convection near the Marshall Islands in mid-November 1987. Meteorologists first classified it as a tropical cyclone on November 19, and by that evening it had strengthened into a tropical storm as it tracked west-northwest across the western Pacific. Late on November 20, Nina passed directly through Chuuk Lagoon in the Federated States of Micronesia, drenching the atoll before continuing its march toward Southeast Asia. After a brief lull in intensification, the storm crossed the threshold into typhoon strength on November 22. What followed was a period of explosive development: over the next two days, Nina's central pressure plummeted and its winds accelerated dramatically. By November 24, the storm had reached its peak ten-minute sustained intensity of 165 km/h, with even higher gusts, placing it among the most powerful storms of the 1987 Pacific typhoon season. This rapid intensification gave coastal communities in the Philippines little time to fully grasp the scale of the threat bearing down on them from the open ocean.

Landfall and Catastrophic Impact

During the afternoon of November 25, 1987, Typhoon Nina made landfall in Southern Luzon at its peak intensity, driving winds of 265 km/h (165 mph) into densely populated coastal provinces. The typhoon's ferocious winds tore roofs from homes, uprooted trees, and flattened light structures across the region, while a massive storm surge swept inland, inundating low-lying barangays. Entire villages along the coast were effectively wiped off the map as the surge combined with torrential rainfall to trigger flash floods and mudslides in mountainous terrain. Fishing communities were especially hard-hit, as boats were destroyed and shorelines reshaped by the pounding waves. Roads, bridges, and communication lines were severed, hampering the ability of provincial officials to assess damage or dispatch aid in the storm's immediate aftermath. Agricultural land, particularly rice paddies and coconut plantations that formed the backbone of the local economy, suffered extensive destruction just before the harvest season, compounding the human tragedy with severe economic losses. The confirmed death toll reached at least 1,036, though given the chaos in remote and coastal areas, the true human cost may never be fully known.

Aftermath and Legacy

In the days following the disaster, the Philippine government and international relief organizations mobilized emergency supplies, medical teams, and temporary shelter for the tens of thousands left homeless across Luzon. The scale of destruction underscored the Philippines' persistent vulnerability to powerful typhoons, particularly in coastal and low-lying regions where storm surge poses as much danger as wind. After weakening over land, Nina emerged into the South China Sea, curved northward, and gradually lost strength before dissipating entirely by November 30, 1987. The storm's Philippine name, Sisang, entered the country's grim catalog of deadly historical typhoons, later retired from PAGASA's naming lists in recognition of the devastation it caused. Typhoon Nina prompted renewed discussions among Philippine disaster planners about early-warning systems, evacuation protocols, and coastal infrastructure resilience, lessons that would inform responses to subsequent super typhoons in the decades that followed. The storm remains a somber benchmark in Philippine meteorological history, cited alongside other historic disasters as evidence of the archipelago's exposure to the full destructive power of the western Pacific's typhoon season.