Tropical Storm Chantal (2007)
Short-lived Atlantic tropical storm in late July–early August 2007 that formed between Bermuda and Cape Cod, reached about 50 mph winds, then became extratropical and moved near Newfoundland.
Overview
Tropical Storm Chantal was a brief tropical cyclone in the northern Atlantic that existed at the end of July and start of August 2007. It was the third named storm of the 2007 Atlantic hurricane season. Chantal is notable for forming from a non-tropical low in mid-latitudes, reaching modest tropical intensity, and then undergoing a rapid transition to an extratropical cyclone while remaining principally over open water.
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10 ImagesMeteorological origins
The system that became Chantal developed from a non-tropical low between Bermuda and Cape Cod in waters off Massachusetts. On July 31 environmental conditions—such as locally favorable sea-surface temperatures and a concentration of organized convection—allowed the low to acquire a warm-core structure and the National Hurricane Center to classify it as a tropical storm. The storm demonstrated how mid-latitude disturbances can acquire tropical characteristics when conditions briefly permit.
Structure and peak intensity
- Peak winds: about 50 mph (80 km/h) sustained, based on operational observations.
- Core type: developed a temporary warm core with organized convection.
- Convection: the presence and persistence of organized convection were central to its classification and subsequent decay.
Track and evolution
After becoming a tropical storm, Chantal moved quickly northeastward into progressively cooler sea-surface temperatures. As the storm advanced, convection waned and the system began to lose its tropical characteristics. The National Hurricane Center issued advisories during Chantal's tropical phase but discontinued tropical advisories on August 1 when it became clear the system was completing extratropical transition.
Timeline
- Late July: a non-tropical low organizes in the northern Atlantic.
- July 31: the system is classified as Tropical Storm Chantal after convection consolidates.
- August 1: Chantal moves into cooler waters, convection decreases, and extratropical transition begins; NHC stops tropical advisories.
- Post-transition: remnants move near southeast Newfoundland and later into higher-latitude waters toward the Arctic Ocean.
Impacts
Because Chantal remained mainly over open water and moved rapidly, it produced little reported damage to land areas and no notable coastal impacts were recorded. Marine interests were the most affected, with elevated seas and gusty winds possible in the storm's vicinity. The brief nature of the storm limited any sustained hazards to coastal communities.
Forecasting and scientific significance
Chantal highlights several forecasting challenges: identifying tropical genesis from a non-tropical precursor, assessing the longevity of convection in a marginal environment, and predicting the timing of extratropical transition. Operational forecasters relied on satellite observations and model analyses of atmospheric structure to determine when Chantal met the criteria for a tropical storm and later when it became post-tropical.
Context within the 2007 season
As the third named storm of the 2007 Atlantic hurricane season, Chantal was a relatively minor event in a season that produced multiple tropical cyclones of varying intensity. Its life cycle is illustrative of short-lived, mid-latitude tropical storms that form over marginally warm waters and are quickly absorbed into larger-scale mid-latitude systems.
Terminology and classification
The distinction between tropical, subtropical, and extratropical systems rests on structure and energy source. A true tropical cyclone derives energy from a warm core and organized deep convection; when convection diminishes and the storm begins deriving energy from horizontal temperature contrasts, it is said to be an extratropical cyclone. Observations of sustained organized convection and a coherent warm core were key to Chantal's brief classification as a tropical storm.
Legacy
Although not a destructive storm, Chantal contributes to the climatological record of Atlantic tropical cyclones and to the understanding of how non-tropical disturbances can transition to tropical systems. Its rapid evolution and transition offer a useful case for study in operational meteorology and in improving prediction of hybrid storm behavior in mid-latitudes.
For official advisories and post-storm analyses, consult archival products from agencies such as the National Hurricane Center and regional meteorological services that monitor the northern Atlantic basin. Historical summaries of the season provide broader context for Chantal's place in the 2007 season.
Questions and answers
Q: What is Tropical Storm Chantal?
A: Tropical Storm Chantal was a short-lived storm that occurred in the northern Atlantic Ocean, and it was the third named storm of the 2007 Atlantic hurricane season.
Q: Did Tropical Storm Chantal cause any damage to land?
A: No, Tropical Storm Chantal stayed away from land during its existence.
Q: How did Tropical Storm Chantal form?
A: Tropical Storm Chantal formed from a non-tropical system between Bermuda on Cape Cod, Massachusetts that developed on July 31 with good conditions for further development.
Q: What were the maximum sustained winds in Tropical Storm Chantal?
A: The maximum sustained winds in Tropical Storm Chantal were 50 mph (80 km/h).
Q: What happened when convection began to decrease in Tropical Storm Chantal?
A: When convection began to decrease, the National Hurricane Center stopped sending out advisories on August 1 when Chantal began to turn into an extratropical cyclone.
Q: Did the remnants of Tropical Storm Chantal move over any land areas?
A: Yes, the remnants of Tropical Storm Chantal moved over southeast Newfoundland before moving into the Arctic Ocean.
Q: When did Tropical Storm Chantal occur?
A: Tropical Storm Chantal occurred in 2007 during the Atlantic hurricane season.
Related articles
Author
AlegsaOnline.com Tropical Storm Chantal (2007) Leandro Alegsa
URL: https://en.alegsaonline.com/art/101690
Sources
- nhc.noaa.gov : "Tropical Depression Three Discussion One"
- nhc.noaa.gov : "Tropical Depression Three Discussion Two"
- nhc.noaa.gov : "Tropical Storm Chantal Tropical Cyclone Update"
- nhc.noaa.gov : "Tropical Storm Chantal Discussion Three"
- nhc.noaa.gov : "Tropical Storm Chantal Discussion Four"
- nhc.noaa.gov : "Tropical Storm Chantal Discussion Five"
- atl.ec.gc.ca : "Post-Tropical Storm Chantal Information Statement at 3:00 AM ADT Wednesday August 1, 2007"
- atl.ec.gc.ca : "Post-Tropical Storm Chantal Intermediate Information Statement at 12:30 PM ADT Wednesday August 1, 2007"
- atl.ec.gc.ca : "Post-Tropical Storm Chantal Intermediate Information Statement at 6:30 PM ADT Wednesday August 1, 2007"
- weather.bm : "Sunny beginning, wet ending…"
- atl.ec.gc.ca : "Tropical Storm Chantal Information Statement at 9:00 AM ADT Tuesday July 31, 2007"
- atl.ec.gc.ca : "Tropical Storm Chantal Information Statement at 3:30 PM ADT Tuesday July 31, 2007"
- canada.com : "Newfoundlanders mopping up after Chantal"