由于地磁位型的不同,发生率的分布并不具有经度对称性,即使在磁赤道附近也如此。
Due to the magnetic effects, the occurrence rate of the instability is not symmetric in longitudes even at the magnetic equator.
由于地磁位型的不同,发生率的分布并不具有经度对称性,即使在磁赤道附近也如此。
Due to the magnetic effects, the occurrence rate of the instability is not symmetric in longitudes even at the magnetic equator.
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