Titlebook: Geomagnetic Diagnosis of the Magnetosphere; A. Nishida Book 1978 Springer Science+Business Media New York 1978 Erdmagnetismus.Magnetosphär

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书目名称Geomagnetic Diagnosis of the Magnetosphere影响因子(影响力)




书目名称Geomagnetic Diagnosis of the Magnetosphere影响因子(影响力)学科排名




书目名称Geomagnetic Diagnosis of the Magnetosphere网络公开度




书目名称Geomagnetic Diagnosis of the Magnetosphere网络公开度学科排名




书目名称Geomagnetic Diagnosis of the Magnetosphere被引频次




书目名称Geomagnetic Diagnosis of the Magnetosphere被引频次学科排名




书目名称Geomagnetic Diagnosis of the Magnetosphere年度引用




书目名称Geomagnetic Diagnosis of the Magnetosphere年度引用学科排名




书目名称Geomagnetic Diagnosis of the Magnetosphere读者反馈




书目名称Geomagnetic Diagnosis of the Magnetosphere读者反馈学科排名

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Computer Vision for Capturing Floran the polar magnetic field. Other aspects of the magnetospheric substorm are similarly called ‘auroral substorm,’ ionospheric substorm,’ etc. (Akasofu, 1968). The magnetospheric substorm represents a process in which plasma is accelerated and electric current is generated at the expense of the magnetic field energy stored in the magnetotail.

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Implosion in the Magnetotail,n the polar magnetic field. Other aspects of the magnetospheric substorm are similarly called ‘auroral substorm,’ ionospheric substorm,’ etc. (Akasofu, 1968). The magnetospheric substorm represents a process in which plasma is accelerated and electric current is generated at the expense of the magnetic field energy stored in the magnetotail.

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0079-1938 osphere. Because the· magnetosphere and its environment are filled with plasma in which electric current can easily flow, dynamic processes that occur in the magnetosphere tend to produce perturba­ tions in the geomagnetic field. Geomagnetic data have therefore pro­ vided valuable means for sensing

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Paleontology

Paleontology

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Dynamic Structure of the Inner Magnetosphere,phere, the ring current is thought to develop within the magnetosphere, and the search for the carrier of such a current led to the prediction of the presence of particles trapped in the geomagnetic field (Singer, 1957).

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