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Magnetic CloudA magnetic cloud is a transient event observed in the solar wind. It was defined in 1981 by Burlaga et al as a region of enhanced magnetic field strength, smooth rotation of the magnetic field vector and low proton density and temperature [1]. Magnetic clouds are a possible manifestation of a Coronal Mass Ejection (CME). The association between CMEs and magnetic clouds was made by Burlaga et al in 1982 when a magnetic cloud was observed by Helios-1 two days after being observed by SMM[2]. However, because observations near Earth are usually done by a single spacecraft, many CMEs are not seen as being associated with magnetic clouds. The typical structure observed for a fast CME by a satellite such as ACE is a fast-mode shock wave followed by a dense (and hot) sheath of plasma (the downstream region of the shock) and a magnetic cloud. Additional recommended knowledge
Other characteristics of magnetic cloudsOther signatures of magnetic clouds are now used in addition to the one described above: among other, bidirectional superthermal electrons, unusual charge state or abundance of iron, helium, carbon and/or oxygen. The typical time for a magnetic cloud to move past a satellite at the L1 point is 1 day corresponding to a radius of 0.15 AU with a typical speed of 450 km s-1 and magnetic field strength of 20 nT [3] Other types of ejecta observed at EarthMagnetic clouds represent about one third of ejecta observed by satellites at Earth. Other types of ejecta are multiple-magnetic cloud events (a single structure with multiple subclouds distinguishable) and complex ejecta, which can be the result of the interaction of multiple CMEs Notes
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This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Magnetic_Cloud". A list of authors is available in Wikipedia. |