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Magnetometer (MAG)

The GOES-R Series Magnetometer provides measurements of the space environment magnetic field that controls charged particle dynamics in the outer region of the magnetosphere. These particles can be dangerous to spacecraft and human spaceflight. The geomagnetic field measurements are important for providing alerts and warnings to many customers, including satellite operators and power utilities.

Data plot showing magnetic field strength over time using blue, green, and red to show OB_x, OB_y, and OB_z

First data plot from the Magnetometer. Credit: ?

The GOES-R Series Magnetometer products are an integral part of NOAA's space weather operations, providing information on the general level of geomagnetic activity and permitting detection of sudden magnetic storms. In addition, measurements can be used to validate large-scale space environment models that are used in operations. GOES Magnetometer data are also important in research, being among the most widely used spacecraft data by the national and international research community.

The MAG requirements are similar to the tri-axial fluxgates that have previously flown. The GOES-R Series requires measurements of three components of the geomagnetic field with a resolution of 0.016 nT and response frequency of 2.5 Hz.

Earth's magnetic field shown as loops and solar wind shown as rays coming from the sun.

Diagram depicting solar wind and Earth's magnetic field. Credit: ?

The magnetosphere is the comet-shaped region around the Earth that is affected by the Earth's magnetic field. It extends some 37,282 miles (60,000 km) from the Earth on the side facing the sun, but on the opposite side, it extends much farther. The boundary of the magnetosphere is called the "magnetopause."

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This video demonstrates a successful boom deployment from the GOES-R Magnetometer Engineering Development Unit. The Magnetometer boom deploys after the spacecraft launches, separates from its launch vehicle, and undergoes a series of orbit raising maneuvers.