The operator difference in absolute geomagnetic measurements

<p>Absolute geomagnetic measurement is very important at geomagnetic observatories. It plays a decisive role in data quality control and instrument calibration. As absolute geomagnetic measurements from modern fluxgate theodolite instruments have high precision, usually within 1&thinsp;arc...

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Main Authors: Y. He, X. Zhao, J. Wang, F. Yang, X. Li, C. Xin, W. Yan, W. Tian
Format: Article
Language:English
Published: Copernicus Publications 2019-01-01
Series:Geoscientific Instrumentation, Methods and Data Systems
Online Access:https://www.geosci-instrum-method-data-syst.net/8/21/2019/gi-8-21-2019.pdf
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spelling doaj-4a05ff7e4b3b4a0496e1547e423ebd972020-11-24T22:03:04ZengCopernicus PublicationsGeoscientific Instrumentation, Methods and Data Systems2193-08562193-08642019-01-018212710.5194/gi-8-21-2019The operator difference in absolute geomagnetic measurementsY. He0X. Zhao1J. Wang2F. Yang3X. Li4C. Xin5W. Yan6W. Tian7Institute of Geophysics, China Earthquake Administration, Beijing, 100081, ChinaInstitute of Geophysics, China Earthquake Administration, Beijing, 100081, ChinaLanzhou Institute of Seismology, China Earthquake Administration, Lanzhou, 730000, ChinaEarthquake Bureau of Xinjiang Province, Urumqi, 830011, ChinaQianling Observatory, Xi'an, 713300, ChinaLanzhou Observatory, Lanzhou, 730046, ChinaLanzhou Observatory, Lanzhou, 730046, ChinaLanzhou Observatory, Lanzhou, 730046, China<p>Absolute geomagnetic measurement is very important at geomagnetic observatories. It plays a decisive role in data quality control and instrument calibration. As absolute geomagnetic measurements from modern fluxgate theodolite instruments have high precision, usually within 1&thinsp;arcsec, the measurement results are susceptible to external factors. The operator difference is one of these factors and has become an important consideration that can not be ignored with respect to measurement results. Therefore, an experiment was designed in order to estimate the operator difference. Six fluxgate theodolites were used and six observers who were proficient in absolute measurements were invited to participate. The observers took turns making absolute geomagnetic measurements, and the operator difference between the observers for each instrument was computed by comparing baseline values using statistical methods.</p>https://www.geosci-instrum-method-data-syst.net/8/21/2019/gi-8-21-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Y. He
X. Zhao
J. Wang
F. Yang
X. Li
C. Xin
W. Yan
W. Tian
spellingShingle Y. He
X. Zhao
J. Wang
F. Yang
X. Li
C. Xin
W. Yan
W. Tian
The operator difference in absolute geomagnetic measurements
Geoscientific Instrumentation, Methods and Data Systems
author_facet Y. He
X. Zhao
J. Wang
F. Yang
X. Li
C. Xin
W. Yan
W. Tian
author_sort Y. He
title The operator difference in absolute geomagnetic measurements
title_short The operator difference in absolute geomagnetic measurements
title_full The operator difference in absolute geomagnetic measurements
title_fullStr The operator difference in absolute geomagnetic measurements
title_full_unstemmed The operator difference in absolute geomagnetic measurements
title_sort operator difference in absolute geomagnetic measurements
publisher Copernicus Publications
series Geoscientific Instrumentation, Methods and Data Systems
issn 2193-0856
2193-0864
publishDate 2019-01-01
description <p>Absolute geomagnetic measurement is very important at geomagnetic observatories. It plays a decisive role in data quality control and instrument calibration. As absolute geomagnetic measurements from modern fluxgate theodolite instruments have high precision, usually within 1&thinsp;arcsec, the measurement results are susceptible to external factors. The operator difference is one of these factors and has become an important consideration that can not be ignored with respect to measurement results. Therefore, an experiment was designed in order to estimate the operator difference. Six fluxgate theodolites were used and six observers who were proficient in absolute measurements were invited to participate. The observers took turns making absolute geomagnetic measurements, and the operator difference between the observers for each instrument was computed by comparing baseline values using statistical methods.</p>
url https://www.geosci-instrum-method-data-syst.net/8/21/2019/gi-8-21-2019.pdf
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