The Bermuda high is a weather phenomenon that is commonly observed in the western Atlantic Ocean. It is a high-pressure system that forms over the western Atlantic Ocean, near the island of Bermuda. The Bermuda high is an important weather system that affects the weather patterns in the eastern United States, the Caribbean, and parts of South America.
Definitions
The Bermuda high is a high-pressure system that forms over the western Atlantic Ocean, near the island of Bermuda. It is a semi-permanent, subtropical high-pressure system that is characterized by warm, moist air and light winds.
Origin
The Bermuda high is thought to have originated during the last Ice Age, when the massive glaciers that covered much of North America caused the jet stream to shift southward. This shift in the jet stream created a high-pressure system over the western Atlantic Ocean, which eventually became the Bermuda high.
Meaning in different dictionaries
The Bermuda high is defined as a semi-permanent, subtropical high-pressure system that is characterized by warm, moist air and light winds. It is also known as the Azores high, the North Atlantic high, and the Atlantic high.
Associations
The Bermuda high is associated with warm, humid weather in the eastern United States, as well as with hurricanes and tropical storms that form in the western Atlantic Ocean. It is also associated with the trade winds that blow across the Caribbean and the Gulf of Mexico.
Synonyms
The Bermuda high is also known as the Azores high, the North Atlantic high, and the Atlantic high.
Antonyms
There are no antonyms for the Bermuda high, as it is a weather phenomenon that is characterized by high pressure and warm, humid weather.
The same root words
There are no other words that share the same root words as the Bermuda high.
Example Sentences
- The Bermuda high is associated with warm, humid weather in the eastern United States.
- The Bermuda high is also associated with hurricanes and tropical storms that form in the western Atlantic Ocean.
The Bermuda high is an important weather system that affects the weather patterns in the eastern United States, the Caribbean, and parts of South America. It is a semi-permanent, subtropical high-pressure system that is characterized by warm, moist air and light winds. The Bermuda high is associated with warm, humid weather in the eastern United States, as well as with hurricanes and tropical storms that form in the western Atlantic Ocean.