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 23-Oct-2024

Volcanic Eruption & Ionospheric Disturbances

Geography

Why in the News?

A new study links the Tonga volcano eruption of 15th January 2022 to the formation of Equatorial Plasma Bubbles (EPBs) over the Indian subcontinent. Tonga volcano is a submarine volcano in the South Pacific Ocean. Researchers found that atmospheric gravity waves from the eruption triggered ionospheric disturbances affecting satellite communication.

Tonga Volcano

  • Location: Western South Pacific Ocean, west of the main inhabited islands in the Kingdom of Tonga.
  • It is one of 12 confirmed submarine volcanoes along the Tofua Arc, a segment of the larger Tonga-Kermadec volcanic arc.
  • The Tonga-Kermadec arc formed as a result of subduction of the Pacific Plate beneath the Indo-Australian Plate.
  • Submarine Volcano: It is an undersea Volcano consisting of two small uninhabited islands, Hunga-Ha’apai and Hunga-Tonga.
  • It is a part of the Ring of Fire.

Location of Tonga Volcano

Equatorial Plasma Bubbles (EPBs)

  • These are regions of depleted plasma density in the Earth’s ionosphere, typically occurring in the equatorial and low-latitude regions during the nighttime.
  • These bubbles form due to instabilities in the ionosphere, often after sunset and can disrupt radio signals, including those used for GPS and communication systems.
  • Their formation and behavior are influenced by factors like geomagnetic activity and solar conditions.
  • They are most frequent during the winter solstice (21st or 22nd December) and least frequent during the summer solstice (21st June).

Ionosphere

  • It is a layer of Earth’s upper atmosphere, extending from about 50 km to 1,000 km above the surface.
  • The electrically charged atoms and molecules that are formed in this way are called ions, giving the ionosphere its name.
  • It’s a very active part of the atmosphere and it grows and shrinks depending on the energy it absorbs from the sun.
  • It is ionized by solar radiation, meaning it contains a high concentration of ions and free electrons.
  • This layer plays a crucial role in atmospheric electricity and affects radio wave propagation, which is essential for communication and navigation systems.
  • It is an electrically conducting region capable of reflecting radio signals back to Earth.

Formation of EPBs