They tried to sail north, away from the storm’s projected path. The storm kept changing direction. The tracking uncertainty that made evasion difficult was compounded by Raymond’s specific behavior: it was not following a simple westward track but was curving and adjusting in ways that made prediction difficult. Each advisory update revised the projected track slightly, and each revision required a recalculation of their evasion options.
For three days they maneuvered. They could not get clear. By October 12, they were within the storm’s circulation, in conditions that made further evasion impossible.
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## What 140-Knot Winds Feel Like
The wind speed figures associated with Hurricane Raymond — 140 knots as recorded by the Hazana’s onboard anemometer, 143 mph as the peak meteorological measurement — are numbers that most people have no physical reference for.
Standard hurricane categories define a Category 4 storm as having sustained winds between 130 and 156 mph. These are sustained winds, not gusts; the gusts within a Category 4 environment routinely exceed 170 mph. At these wind speeds, the air itself becomes a physical force: it removes roof structures, moves vehicles, and creates a continuous, overwhelming pressure on any surface it contacts.
At sea, the wind’s effects are compounded by its interaction with the water. Wind at hurricane speed does not simply move air; it tears the surface off the water, creating a horizontal spray that reduces visibility to near zero and fills the air with atomized saltwater. The waves that build under sustained hurricane-force winds are not the organized swells of an ordinary ocean passage; they are steep, breaking, chaotic masses of water that can come from multiple directions simultaneously as the storm’s circulation creates a pattern of swells that interact at cross-angles.