Monitoring geomagnetic information in the territory of Croatia

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geofizika Pub Date : 2019-01-01 DOI:10.15233/GFZ.2019.36.3
M. Brkić
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引用次数: 2

Abstract

In orientation and navigation using compass, reliable map’s marginal information of Earth’s magnetic field declination and its annual variation, namely geomagnetic information (GI), is crucial. Monitoring geomagnetic information means observing declination and its annual variation and checking the reliability of the actual GI model. A typical way of monitoring GI across a national territory involves conducting periodic geomagnetic network surveys to assess and update the model. The objective of the paper was to investigate improving the GI model reliability when an earlier model’s error was raised to standard accuracy, and repeat station network surveys were not yet completed. A series of processing steps in modelling were revised to preserve the original data reliability. The partial 2008.5, 2009.5 and 2010.5 declination solutions were directly reduced to epoch 2015.0, and then to 2016.0, using the IGRF-12 model. The next step was to use 2016 and 2017 quiet daily declination means to estimate corresponding annual variations at surrounding observatories and repeat stations. Normal declination annual variation models were then built for further reductions to epoch 2017.0, and 2018.0, and for forward extrapolations. The quiet days observatory data were analysed to estimate the effect of the input time series length and linear extrapolated time span on forward extrapolation error. Thus, the reliability decline of the initial GI model slowed down in the sequence of models presented. The final GI2018v2 model, valid for 2018.0–2019.0, proved reliable in comparison to the repeat station declination observations of 2018.
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监测克罗地亚境内的地磁资料
在指南针定位导航中,可靠的地球磁场赤纬及其年变化的地图边缘信息,即地磁信息(GI)至关重要。地磁信息监测就是观测赤纬及其年变化,并检验实际GI模式的可靠性。在全国范围内监测地理特征的一种典型方法是定期进行地磁网调查,以评估和更新模型。本文的目的是探讨在早期模型误差提高到标准精度,且重复站网调查尚未完成的情况下,如何提高GI模型的可靠性。修正了建模中的一系列处理步骤,以保持原始数据的可靠性。利用IGRF-12模式将2008.5、2009.5和2010.5的部分赤纬解直接还原为2015.0历元,然后再还原为2016.0历元。下一步是使用2016年和2017年安静日赤纬方法估计周围观测站和重复站相应的年变化。然后建立了正常赤纬年变化模型,以进一步减少至2017.0和2018.0历元,并进行前向外推。分析了静日观测资料,估计了输入时间序列长度和线性外推时间跨度对前向外推误差的影响。因此,初始GI模型的可靠性下降速度随着模型的增加而减慢。与2018年的重复站赤纬观测结果相比,最终的GI2018v2模型(2018 - 2019.0有效)被证明是可靠的。
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来源期刊
Geofizika
Geofizika 地学-地球化学与地球物理
CiteScore
1.60
自引率
0.00%
发文量
17
审稿时长
>12 weeks
期刊介绍: The Geofizika journal succeeds the Papers series (Radovi), which has been published since 1923 at the Geophysical Institute in Zagreb (current the Department of Geophysics, Faculty of Science, University of Zagreb). Geofizika publishes contributions dealing with physics of the atmosphere, the sea and the Earth''s interior.
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