Swarm satellite mission to try to sense ocean magnetism
Baku, December 18 (AZERTAC). European scientists are going to try to measure the movement of the oceans by tracing their magnetism alone.
The effort will be achieved using three super-sensitive spacecraft called Swarm, which should launch in 2012.
The magnetic signal of the tides sweeping around the globe has been seen before, but the new mission would aim to observe far more detail.
It should provide additional data on how the oceans transfer heat around the Earth, a key feature of the climate.
"When salty ocean water flows through the magnetic field of the Earth, an electric field is generated and this electric field again makes a magnetic field," explained Dr Hermann Lühr, from the German Research Centre for Geosciences (GFZ) and a leading investigator on Swarm.
"We hope to have the possibility to measure the ocean currents which are so important for climate dynamics, because oceans are transporting a lot of heat. The German Champ mission was the first to see at least the tidal signal, but with Swarm we want to be able to monitor the currents themselves."
The new mission is one of the several innovative European Space Agency (Esa) endeavors being discussed this week here at the American Geophysical Union (AGU) Fall Meeting, the largest annual gathering of Earth and planetary scientists.
The major part of Earth`s global magnetic field is generated by convection of molten iron within the planet`s outer liquid core, but there are other components that contribute to the overall signal, including the magnetism retained in rocks.
Swarm`s goal is to investigate all the components, but pulling out the small part produced by ocean movement will probably be its greatest challenge, concedes Dr Mark Drinkwater from Esa`s Earth observation division.
"We're talking about tens of thousands of nanoteslas for the total field measured at satellite level, of which one part in 50,000 approximately is contributed by ocean circulation," he told BBC News.
"So it`s a akin to finding a needle in a haystack, but the modeling which has shown the irretrievability of this element of the magnetic field has demonstrated that it might be possible with."
It means the spacecraft themselves have to be built with extreme care. The magnetism generated by the satellites' own workings has to be minimized as much as possible, and thoroughly modeled to understand what interference it might be introducing into the scientific data.
Scientists reported first in 2003 that this satellite could sense the subtle magnetic field generated as the waters of the Earth moved under the gravitational tug of the Moon. This signal was apparent because of its very regular pattern.
Sensing the more complex signal from general ocean currents will be much more difficult, however.
At present, researchers use a range of methods to track the currents, including altimetry - the measurement of ocean surface height.
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