The season's final storm, Hurricane Karl, dissipated on November 27.

Hurricane Karl was one of four hurricanes in the Atlantic Ocean on September 26.

Hurricane Karl made its way to southern Britain in 1998.

The origins of Hurricane Karl were from the interaction between a surface trough and westward-tracking tropical wave.

Hurricane Karl was a strong category 4 that only affected the Faroe Islands.

In October 2004, the vessel lost power during Hurricane Karl while doing a transatlantic crossing.

Tabasco was affected by Hurricane Karl and produced the overflow of the principal rivers.

Hurricane Karl was the fifth and final major hurricane of 2010's Atlantic hurricane season.

Hurricane Karl originated in a low pressure area that formed along a frontal boundary near the southeastern United States.

Hurricane Karl was unusual in several aspects.