kennelly-heaviside layer (Meaning)
kennelly-heaviside layer (n)
a region of the ionosphere (from 50 to 90 miles up) that reflects radio waves of medium length
Synonyms & Antonyms of kennelly-heaviside layer
No Synonyms and anytonyms found
kennelly-heaviside layer Sentence Examples
- The Kennelly-Heaviside layer is a conducting layer in the Earth's ionosphere that reflects radio waves.
- The Kennelly-Heaviside layer is formed when ultraviolet radiation from the sun ionizes atoms and molecules in the upper atmosphere, creating free electrons.
- The Kennelly-Heaviside layer is found at an altitude of about 90 to 150 kilometers (56 to 93 miles) above the Earth's surface.
- The Kennelly-Heaviside layer is named after two scientists, Arthur Kennelly and Oliver Heaviside, who independently predicted its existence in the early 20th century.
- The Kennelly-Heaviside layer is also known as the E-layer or the ionosphere E-region.
- The Kennelly-Heaviside layer is important for long-distance radio communication because it reflects radio waves back to Earth, allowing signals to be transmitted over long distances.
- The Kennelly-Heaviside layer is also important for satellite communications, as it reflects signals from satellites back to Earth.
- The Kennelly-Heaviside layer is affected by solar activity, and its properties can change depending on the time of day, the season, and the sun's activity level.
- The Kennelly-Heaviside layer is a dynamic region of the atmosphere, and its properties are constantly changing.
- The Kennelly-Heaviside layer is an important part of the Earth's atmosphere and plays a vital role in radio communications.
FAQs About the word kennelly-heaviside layer
a region of the ionosphere (from 50 to 90 miles up) that reflects radio waves of medium length
No synonyms found.
No antonyms found.
The Kennelly-Heaviside layer is a conducting layer in the Earth's ionosphere that reflects radio waves.
The Kennelly-Heaviside layer is formed when ultraviolet radiation from the sun ionizes atoms and molecules in the upper atmosphere, creating free electrons.
The Kennelly-Heaviside layer is found at an altitude of about 90 to 150 kilometers (56 to 93 miles) above the Earth's surface.
The Kennelly-Heaviside layer is named after two scientists, Arthur Kennelly and Oliver Heaviside, who independently predicted its existence in the early 20th century.
