about
Antiquity of the South Atlantic Anomaly and evidence for top-down control on the geodynamo.Gyre-driven decay of the Earth's magnetic dipoleRapid regional perturbations to the recent global geomagnetic decay revealed by a new Hawaiian record.Predicting space climate changeThe South Atlantic Anomaly: The Key for a Possible Geomagnetic ReversalCan core flows inferred from geomagnetic field models explain the Earth's dynamo?An impending geomagnetic transition? Hints from the pastThe influence of high-latitude flux lobes on the Holocene paleomagnetic record of IODP Site U1305 and the northern North AtlanticUsing archaeomagnetic field models to constrain the physics of the core: robustness and preferred locations of reversed flux patchesThe time dependence of reversed archeomagnetic flux patches
P2860
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P2860
description
2006 nî lūn-bûn
@nan
2006年の論文
@ja
2006年学术文章
@wuu
2006年学术文章
@zh
2006年学术文章
@zh-cn
2006年学术文章
@zh-hans
2006年学术文章
@zh-my
2006年学术文章
@zh-sg
2006年學術文章
@yue
2006年學術文章
@zh-hant
name
Fall in Earth's magnetic field is erratic.
@en
Fall in Earth's magnetic field is erratic.
@en-gb
Fall in Earth's magnetic field is erratic.
@nl
type
label
Fall in Earth's magnetic field is erratic.
@en
Fall in Earth's magnetic field is erratic.
@en-gb
Fall in Earth's magnetic field is erratic.
@nl
prefLabel
Fall in Earth's magnetic field is erratic.
@en
Fall in Earth's magnetic field is erratic.
@en-gb
Fall in Earth's magnetic field is erratic.
@nl
P356
P1433
P1476
Fall in Earth's magnetic field is erratic.
@en
P2093
Adrian L Jones
P304
P356
10.1126/SCIENCE.1124855
P407
P577
2006-05-01T00:00:00Z