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Earth's magnetic field 'simpler than we thought'

机译:地球的磁场比我们想象的更简单

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Scientists have identified patterns in Earth's magnetic field that evolve on the order of 1000 years, providing new insight into how the field works and adding a measure of predictability to changes in the field not previously known. The discovery will also allow researchers to study the planet's past with finer resolution by using this geomagnetic 'fingerprint' to compare sediment cores taken from the Atlantic and Pacific oceans. Results of the research were recently published in Earth and Planetary Science Letters (https://doi.org/10.1016/j.epsl.2017.05.022).
机译:科学家们已经确定了地球磁场中的模式,即在1000年的阶数演变,提供了对现场如何运作和增加了以前已知的领域的变化的可预测性度量的新洞察。 发现还将允许研究人员通过使用这种地磁“指纹”来比较从大西洋和太平洋所采取的沉积核心来研究地球的过去。 最近在地球和行星科学字母中公布的研究结果(https://doi.org/10.1016/j.epsl.2017.05.022)。

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