地球の磁場における落下は不規則である.
David Gubbins1, Adrian L Jones, Christopher C Finlay
1School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK. gubbins@earth.leeds.ac.uk
まとめ
地球の磁場強度は1590年から1840年まで,後の急速な衰退とは異なり,安定したままでした. この安定性は,二極場が19世紀まで一定であったことを示しており,その後の変化は南半球から生じた.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地球科学 地球科学 地球科学
- パレオマグネティズム (古磁気学) とは
背景:
- 地球の磁場は,1840年以来,1世紀あたり約5%の大幅な衰退率を示しています.
- 磁場の方向測定は,強度測定より250年以上前のものです.
研究 の 目的:
- 1590年から1840年までの地球の磁場強度の変化を推定する.
- 1840年以降観測された磁場崩壊の起源を調査する.
主な方法:
- 古磁気方向のグローバルモデルと古磁気強度のデータを組み合わせた.
- エクストラポレーションされた磁場強度は,コア表面に変化する.
主要な成果:
- 地球の磁場強度は,西暦1590年から1840年の間にほぼ一定であった.
- 後の衰退期 (1840年後の) は,南半球における逆磁気流のパッチから発生した.
- 方向データだけで,これらのパッチの存在が示されましたが,1840年以前のモデルは最小限の証拠を示しました.
結論:
- 地球の磁場は,1840年まで安定した二極状態を維持した.
- 観測された磁場強度の衰退は,19世紀に始まり,南半球の特定の流動パッチによって引き起こされた.
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