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Discovery of the pearl waves by Eyvind Sucksdorff

机译:艾文·萨克斯多夫(Eyvind Sucksdorff)发现珍珠浪

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Eyvind Sucksdorff (1899-1955) was an enthusiastic scientist who was the director of Sodankyla Geophysical Observatory (SGO) from 1927 to 1945. He continued magnetic measurements, which were started in 1913 when SGO was established. Sucksdorff observed events with periodically modulated amplitude in the registration of the new La Cour quick-run magnetometers in 1932-35. He interpreted these events to be due to short-period oscillations and called them "rapid micropulsations" or "pearl necklace" due to the shape of the signal in the registration. From the "pearl necklaces" he estimated the upper bound of the oscillation to be 2-3 s. Sucksdorff did not know the accurate values of the eigenperiods of the systems (H, D and Z components of the magnetometer). Later measurements have shown that they were 2-3s. Nowadays, the pearl pulsations discovered by Sucksdorff 70 years ago are known as a subgroup of Pc1 magnetic pulsations. Sucksdorff published his observations in 1936. He studied both the annual and diurnal distributions of the new pulsations. Comparisons of the records made in Stockholm, Copenhagen and Sodankyla revealed for the first time the global features of Pc1 pulsations. Sucksdorff did not present any explanation for the pearl pulsations he had observed. Leiv Harang from the Auroral Observatory at Tromso, Norway, published his analysis of rapid registrations made in Tromso in 1932-36 in the same issue of the Terrestrial Magnetism and Atmospheric Electricity. He used the name "vibrations" for his short-period oscillations. (C) 2007 Elsevier Ltd. All rights reserved.
机译:Eyvind Sucksdorff(1899-1955)是一位热情的科学家,曾于1927年至1945年担任Sodankyla地球物理观测站(SGO)的负责人。他继续进行磁测量,该测量始于1913年SGO成立。 Sucksdorff在1932-35年间观测到的事件中,其周期性地调制了新的La Cour快速运行磁力计。他将这些事件解释为是由于短周期的振荡所致,并由于配准中信号的形状而将其称为“快速微脉冲”或“珍珠项链”。根据“珍珠项链”,他估计振荡的上限为2-3 s。 Sucksdorff不知道系统本征周期(磁力计的H,D和Z分量)的准确值。后来的测量表明它们是2-3s。如今,由Sucksdorff于70年前发现的珍珠脉动被称为Pc1磁脉动的一个子群。 Sucksdorff于1936年发表了他的观察结果。他研究了新脉动的年度和昼夜分布。在斯德哥尔摩,哥本哈根和Sodankyla进行的记录比较表明,Pc1搏动的全球特征首次显现出来。 Sucksdorff没有对他观察到的珍珠脉动做出任何解释。来自挪威特罗姆瑟极光观测台的莱夫·哈朗(Leiv Harang)发表了他对1932-36年在特罗姆瑟进行的快速注册的分析,涉及同一时期的《地磁和大气电》。他使用“振动”这个名称来表示他的短期振荡。 (C)2007 Elsevier Ltd.保留所有权利。

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