Cyclone Glenda formed in late March and quickly intensified into a powerful tropical cyclone. As it approached the coast of Western Australia, meteorologists monitored its trajectory closely, anticipating landfall near the town of Onslow. The Bureau of Meteorology issued warnings, advising residents of the impending storm and urging protective measures. Glenda reached its peak intensity just before landfall, with reported sustained winds reaching over 200 km/h (124 mph). The cyclone brought heavy rainfall, with accumulations exceeding 200 mm in some areas, exacerbating the risk of flooding and damaging coastal structures. As Glenda made landfall, it caused widespread destruction, including downed trees, damaged roofs, and disrupted power supply. Emergency services, including State Emergency Service volunteers, mobilized to assist affected residents in the aftermath of the storm.

In the wake of Cyclone Glenda, the recovery process began promptly. Local authorities assessed the damages and began clearing debris from streets and properties. Community resilience was tested as residents worked together to restore normalcy, with many relying on assistance from local government and NGOs. The event highlighted the importance of preparedness and response for severe weather events in the region, as well as the ongoing need for robust infrastructure in cyclone-prone areas of Western Australia. Furthermore, the event's meteorological data contributed to the broader understanding and forecasting of tropical cyclones in the Australian region.