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首页> 外文期刊>GEM - International Journal on Geomathematics >Visualising geomagnetic data by means of corresponding observations
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Visualising geomagnetic data by means of corresponding observations

机译:通过相应的观测结果可视化地磁数据

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摘要

Geomagnetic observation data was already being depicted (visualised) in the form of isolines on maps and globes back in the eighteenth century. Corresponding, synchronous observations had already been made in certain astronomical and meteorological areas, but this method yielded singular results in the field of geomagnetism. The observation results were consequently made generally available. It was Alexander von Humboldt who took the first critical steps in establishing this method of corresponding observations in geomagnetic research; Russia was the first cooperative partner. However, the future of geomagnetic research belonged to Gauss, who improved observation methods and instruments as well as making this information available to a wider public in the journal “Resultate aus den Beobachtungen des magnetischen Vereins”. He published the results of corresponding observations in form of pictorial illustrations; this clearly showed who led the field in his day. It was left to Gauss’ pupil Adolph Theodor Kupffer, born in the Baltic area, to make Gauss’ results known in Russia and to promote them; this was particularly important in a time in which Göttingen had already relinquished its status as the centre of geomagnetic research. Russia became the site of the world’s first geomagnetic research institution, i.e. the main geophysical observatory founded in 1849, which still exists today.
机译:早在18世纪,地磁观测数据就已经以等值线的形式在地图和地球仪上进行了描绘(可视化)。相应地,已经在某些天文和气象领域进行了同步观测,但是这种方法在地磁领域产生了奇异的结果。因此,观察结果普遍可用。亚历山大·冯·洪堡(Alexander von Humboldt)采取了关键的第一步,建立了地磁研究中相应观测方法。俄罗斯是第一个合作伙伴。然而,地磁研究的未来属于高斯,他改进了观测方法和仪器,并在“ Result of aus den Beobachtungen des magnetischen Vereins”杂志上将这一信息提供给更广泛的公众。他以绘画插图的形式发表了相应观察的结果;这清楚地表明了谁领导了他的时代。高斯的学生阿道夫·西奥多·库弗(Adolph Theodor Kupffer)留在波罗的海地区,以便在俄罗斯宣传高斯的成绩并加以推广。在哥廷根已经放弃其作为地磁研究中心地位的时代,这一点尤其重要。俄罗斯成为世界上第一个地磁研究机构的所在地,即1849年成立的主要地球物理观测站,至今仍然存在。

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