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

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書目名稱Geomagnetic Diagnosis of the Magnetosphere影響因子(影響力)




書目名稱Geomagnetic Diagnosis of the Magnetosphere影響因子(影響力)學科排名




書目名稱Geomagnetic Diagnosis of the Magnetosphere網(wǎng)絡公開度




書目名稱Geomagnetic Diagnosis of the Magnetosphere網(wǎng)絡公開度學科排名




書目名稱Geomagnetic Diagnosis of the Magnetosphere被引頻次




書目名稱Geomagnetic Diagnosis of the Magnetosphere被引頻次學科排名




書目名稱Geomagnetic Diagnosis of the Magnetosphere年度引用




書目名稱Geomagnetic Diagnosis of the Magnetosphere年度引用學科排名




書目名稱Geomagnetic Diagnosis of the Magnetosphere讀者反饋




書目名稱Geomagnetic Diagnosis of the Magnetosphere讀者反饋學科排名

入伍儀式

Computer Vision for Capturing Floran the polar magnetic field. Other aspects of the magnetospheric substorm are similarly called ‘a(chǎn)uroral 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 ‘a(chǎn)uroral 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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赤字

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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