Tropical Storm Cristobal (2002)

Meteorological history and characteristics

Cristobal developed from a tropical disturbance and reached tropical-storm strength before weakening and losing organized convection. Like other tropical storms, it had a warm-core structure with organized bands of showers and thunderstorms while it persisted. The system tracked across the central Atlantic and eventually decayed as it encountered cooler waters and less favorable atmospheric conditions.

Impacts

Although Cristobal did not cause large-scale structural damage, it produced measurable weather at sea and along some coastal zones. Rain and gusty winds were reported on Bermuda when the storm's outer bands passed nearby. More seriously, the storm generated strong swell and hazardous surf along portions of the U.S. East Coast; those conditions contributed to three drowning fatalities near Long Island. Aside from these incidents, there were no widespread reports of severe land damage or major flooding associated with the storm.

• Measured rain and gusts on Bermuda — see regional summaries: Bermuda observations.
• Hazardous surf and coastal drownings near Long Island — reported in local accounts: Long Island reports.
• No significant infrastructure damage recorded from the storm.

Aftermath and significance

The primary hazards from Cristobal were marine in nature: elevated waves, rip currents, and churning seas that posed risks to swimmers, beachgoers, and small craft. The event underscores that even relatively weak or short-lived tropical storms can create dangerous coastal conditions well away from the storm's center. Cristobal (2002) is distinct from later storms that used the same name in subsequent seasons, each of which had different tracks and impacts.