Tropical Storm Chris
Tropical Storm Chris was a significant tropical cyclone that formed over the Atlantic Ocean in 2018. The storm developed from a tropical wave that emerged off the coast of Africa on June 28, 2018. As the wave moved westward, it gradually organized and became a tropical depression on July 6, 2018, at 21:00 UTC. The depression was located about 1,000 miles (1,609 km) east-southeast of the Lesser Antilles. Over the next 24 hours, the system continued to strengthen, and it became Tropical Storm Chris on July 7, 2018, at 21:00 UTC.
Formation and Intensification
Tropical Storm Chris formed in a region of favorable atmospheric conditions, including low wind shear and warm sea surface temperatures. These conditions allowed the storm to intensify rapidly, and it became a strong tropical storm with maximum sustained winds of 60 mph (95 km/h) on July 8, 2018. The storm’s central pressure decreased to 1002 mbar, indicating a significant increase in its intensity. As Chris moved northward, it encountered a mid-level trough, which caused the storm to turn northeastward. This change in direction helped to steer the storm away from the eastern United States and the Caribbean islands.
Track and Impact
Tropical Storm Chris tracked northeastward over the open waters of the Atlantic Ocean, posing no significant threat to land. However, the storm did produce rough seas and strong winds, which affected several ships and offshore platforms. On July 10, 2018, Chris reached its peak intensity, with maximum sustained winds of 70 mph (110 km/h) and a central pressure of 995 mbar. The storm maintained this intensity for about 24 hours before beginning to weaken due to increasing wind shear and cooler sea surface temperatures.
Storm Category | Maximum Sustained Winds | Central Pressure |
---|---|---|
Tropical Depression | 35 mph (55 km/h) | 1008 mbar |
Tropical Storm | 60 mph (95 km/h) | 1002 mbar |
Peak Intensity | 70 mph (110 km/h) | 995 mbar |
Weather Conditions and Storm Surge
Tropical Storm Chris produced strong winds and rough seas, with wave heights reaching up to 20 feet (6 meters) in some areas. The storm also generated a storm surge, which is a rise in sea level due to the storm’s winds and low atmospheric pressure. However, the storm surge was not significant, and it did not pose a major threat to coastal areas. The storm’s rainfall was also relatively limited, with most areas experiencing less than 2 inches (50 mm) of precipitation.
Storm Dissipation
Tropical Storm Chris began to dissipate on July 12, 2018, as it encountered increasing wind shear and cooler sea surface temperatures. The storm’s circulation became disorganized, and its winds decreased significantly. By July 13, 2018, Chris had degenerated into a post-tropical cyclone, and it was no longer a significant threat. The storm’s remnants continued to move northeastward, eventually merging with a frontal system over the North Atlantic Ocean.
- The storm's formation and intensification were influenced by favorable atmospheric conditions, including low wind shear and warm sea surface temperatures.
- Tropical Storm Chris posed no significant threat to land, but it did produce rough seas and strong winds that affected several ships and offshore platforms.
- The storm's track and intensity were closely monitored by meteorologists, who used advanced computer models and satellite imagery to predict its movement and strength.
What was the peak intensity of Tropical Storm Chris?
+Tropical Storm Chris reached its peak intensity on July 10, 2018, with maximum sustained winds of 70 mph (110 km/h) and a central pressure of 995 mbar.
Did Tropical Storm Chris pose a significant threat to land?
+No, Tropical Storm Chris did not pose a significant threat to land. The storm tracked northeastward over the open waters of the Atlantic Ocean, affecting only several ships and offshore platforms.
What factors influenced the formation and intensification of Tropical Storm Chris?
+The storm’s formation and intensification were influenced by favorable atmospheric conditions, including low wind shear and warm sea surface temperatures.