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Bookmark or Share- Geomagnetic field - Magnetopause, Currents, Shielding | BritannicaThis system is called the magnetopause current, or Chapman-Ferraro current system for the English physicist Sydney Chapman and his student V.C.A. Ferraro, who first suggested its existence. It flows in a single sheet and forms a boundary between the magnetic fields of Earth and solar wind.
- #19H. The Magnetopause -- History - NASAThe magnetopause itself was first observed in 1961 by NASA's Explorer 12. Many satellites have since then studied and probed it--notably, Europe's HEOS 1 and 2 (1975-6) above the poles, as well as NASA's ISEE-3 (1983) and Japan's Geotail (1992-4), extended missions which, during the marked years, probed the distant tail region, up to distances
- Earth's magnetosphere - NOAA / NWS Space Weather Prediction CenterThe boundary between the solar wind and Earth’s magnetic field is called the magnetopause. The boundary is constantly in motion as Earth is buffeted by the ever-changing solar wind. While the magnetopause shields us to some extent from the solar wind, it is far from impenetrable, and energy, mass, and momentum are transferred from the solar ...
- CCMC Real-Time Tools - NASAPlease go to this iSWA layout to viwew the magnetopause standoff related images and to view movies of the recent development. Magnetic field at GOES-P and GOES-S Earth-Sun magnetic connectivity | Structure of heliosphere | Magnetopause position
- 磁层顶 - 百度百科磁层顶（英文：Magnetopause）是太阳风和磁层的交界区，它区分出太阳风和磁层的磁场和等离子体。 磁层顶位形变化反映太阳风变化，影响磁层内部磁场，也影响磁层内部各电流体系和各区域空间分布状况。
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