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MODELLING AND ANALYSIS OF SOUTHERN AFRICAN GEOMAGNETIC FIELD OBSERVATIONS: 1840 UNTIL 1903

机译:南部非洲地磁观测的建模与分析:1840年至1903年

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摘要

The requirements of navigation, rather than any scientific interest in geomagnetism, prompted the recording of data of magnetic field components at the Cape of Good Hope (CGH), even before 1600. The importance of knowing the deviation of a compass needle from true north was sufficient to warrant the establishment of a recording station at the Cape in 1841. The first magnetic survey of the Union of South Africa, comparable with that of developed countries in the Northern Hemisphere, was carried out by Beattie (1909), assisted by J.T. Morrison of the University of Stellenbosch, who subsequently reduced the data to 1st July 1903. In this paper we compare the measurements in Cape Town between 1840 until 1903, as well as the field survey of 1903.5, to COV-OBS and gufm1, historical global geomagnetic field models covering the observatory and satellite period of 1840 until 2010 and 1590 until 1990, respectively, while declination observations show clear evidence of a geomagnetic jerk around 1880 to 1883, which correlates with similar observations in Europe a few years earlier (1870). The field survey data of 1903.5 are used to derive a Spherical Cap Harmonic Model for southern Africa using observations of declination (D), inclination (I) and horizontal intensity (H). We also used secular variation measurements for D, I and H obtained during 1900 to 1905 at a few select stations to derive a secular variation model for Southern Africa based on a polynomial approach.
机译:导航的需求,而不是对地磁的任何科学兴趣,促使人们甚至在1600年之前就在好望角(CGH)记录了磁场分量的数据。了解罗盘针偏离真北角的重要性在于足以保证在1841年在开普省建立一个录音站。Beattie(1909)在JT的协助下对南非联盟进行了首次磁探测,与北半球发达国家的磁探测相当。斯泰伦博斯大学的莫里森(Morrison)随后将数据缩减至1903年7月1日。在本文中,我们将1840年至1903年之间在开普敦的测量值以及1903.5的实地测量结果与COV-OBS和gufm1(历史全球地磁场模型分别覆盖了1840年至2010年的天文台和卫星时期以及1590年至1990年的天文数字,而磁偏角观测则清楚地表明了1880年至1883年左右地磁急动的证据,这与几年前欧洲的类似观测(1870年)相关。 1903.5的现场调查数据用于通过偏角(D),倾角(I)和水平强度(H)的观测结果得出南部非洲的球冠谐波模型。我们还使用了1900年至1905年在几个选定站点获得的D,I和H的长期变化量度,以基于多项式方法得出了南部非洲的长期变化量模型。

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