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Atlantic Ocean observatory to solve mysterious irregularity of Earth's magnetic field.


Byline: ANI

Washington, Nov 30 (ANI): A newly developed observatory on a remote island in the middle of the Atlantic Ocean will provide researchers with new knowledge about the mysterious irregularity of the Earth's magnetic field Earth's magnetic field (and the surface magnetic field) is approximately a magnetic dipole, with one pole near the north pole (see Magnetic North Pole) and the other near the geographic south pole (see Magnetic South Pole).  known as the South Atlantic Anomaly The South Atlantic Anomaly (or SAA) is the region where Earth's inner van Allen radiation belt makes its closest approach to the planet's surface. The result is that, for a given altitude, the radiation intensity is higher over this region than elsewhere. .

The observatory is a partnership between the Danish Meteorological Institute The Danish Meteorological Institute (Danish: Danmarks Meteorologiske Institut) is the official Danish meteorological institute, administrated by the Ministry of Transport and Energy.  (DMI (Desktop Management Interface) The first desktop management standard from the DMTF. Enabling PCs to be monitored from a central console, it was superseded by the DMTF's Common Information Model (see CIM). ), and DTU DTU Technical University of Denmark
DTU Data Transfer Unit
DTU Data Transmission Unit
DTU Direct To User
DTU Data Terminal Unit
DTU Dry Tree Unit (offshore oil and gas production)
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 Space, the Danish National Space Institute.

The new geomagnetic observatory is located on the island of Tristan da Cunha Tristan da Cunha (trĭs`tăn də k`nə), group of volcanic islands in the S Atlantic, about midway between S Africa and S America.  and was inaugurated on November 14 by the island's roughly 300 inhabitants
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 and a few of the researchers on the project.

Tristan da Cunha is the remotest inhabited island in the world and is also located right in the middle of the South Atlantic Anomaly, which is the area where the Earth's magnetic field is weakest.

This makes it incredibly interesting for the Danish researchers, who are working to understand the Earth's magnetic field and the way in which it affects satellites, for example.

"Until now, Denmark has mostly been involved in projects that measure the magnetic field from space, with the Orsted satellite and the future Swarm satellite mission, as well as the measuring stations in Greenland," said Professor Nils Olsen of DTU Space.

"With the observatory on Tristan da Cunha, we will have a measuring station in the Tropics right in the middle of the South Atlantic Anomaly, where the strength of the magnetic field is only half as high as in Denmark," he added.

At present, the strength of the Earth's magnetic field is decreasing by 5 percent every hundred years and researchers do not know why or what the consequences will be.

In the South Atlantic Anomaly, the strength of the magnetic field is decreasing ten times as fast and the measuring station will therefore also give the researchers the opportunity to learn more about the consequences of the global weakening of the magnetic field.

The magnetic field protects the Earth from radiation from space and the area around the South Atlantic Anomaly is therefore very poorly protected.

In the Anomaly, the radiation belts that surround the Earth, the van Allen belts, are very close to the surface of the Earth. This is, among other things, significant to satellites, which suffer by far the majority of faults when they fly through this area.

"Opening the observatory is a milestone in our research," said senior researcher Jurgen Matzka from DMI, who is heading the project. (ANI)

Copyright 2008 Asian News International The Asian News International (ANI) agency provides multimedia news to China and 50 bureaus in India. It covers virtually all of South Asia since its foundation and presently claims, on its official website, to be the leading South Asia-wide news agency.  (ANI) - All Rights Reserved.

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Publication:Asian News International
Date:Dec 3, 2008
Words:420
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