On November 1, the system had estimated winds of 100 km/h (60 mph) and its most developed convection. After that, it slowly weakened, moved counter-clockwise, and headed east towards the west coast of North America. On November 2, wind shear started affecting the storm, and all convection was gone by the next day, when it was located roughly 520 mi (840 km) off the coast of Oregon.
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