Preprints
https://doi.org/10.5194/egusphere-2025-2563
https://doi.org/10.5194/egusphere-2025-2563
26 Jun 2025
 | 26 Jun 2025
Status: this preprint is open for discussion and under review for Geoscientific Instrumentation, Methods and Data Systems (GI).

The azimuth observation by GNSS: A case study at Kakioka

Hiroki Matsushita, Daisuke Matsuura, Funa Iizuka, Junpei Oogi, and Seiki Asari

Abstract. For the azimuth observation to be made at its magnetic observatories routinely, Japan Meteorological Agency (JMA) has adopted a traditional method based on Polaris sighting. Due to its difficulty to implement under overcast weather conditions and to its demand on observers, for overtime work into the evening, we are motivated to seek for an alternative method based on the GNSS observation that might potentially relieve those two disadvantages. An experiment is made at Kakioka to assess the eligibility and effectiveness of the GNSS method for JMA's unmanned observatories, Memambetsu and Kanoya. The GNSS observations themselves achieve as high a precision as approximately 1 arcsecond, as far as they are analyzed with Static mode. Derived from the results of GNSS observation and some supplementary horizontal angle measurements, the azimuth of the azimuth mark for the absolute measurement is determined with a precision of a few arcsecond, which is comparable to the azimuth precision achieved by the Polaris sighting. However, we end up with their significant difference by about 10 arcseconds. We discuss this discrepancy to be possibly due to a local geoid gradient. The Polaris observation is made with a theodolite tilted in the gravitational direction, also known as the vertical line deviation, whereas the GNSS observations are based on the azimuth of the compliant ellipsoid plane.

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Hiroki Matsushita, Daisuke Matsuura, Funa Iizuka, Junpei Oogi, and Seiki Asari

Status: open (until 19 Aug 2025)

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Hiroki Matsushita, Daisuke Matsuura, Funa Iizuka, Junpei Oogi, and Seiki Asari
Hiroki Matsushita, Daisuke Matsuura, Funa Iizuka, Junpei Oogi, and Seiki Asari

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Short summary
We have adopted Polaris sighting as our azimuth observation at our observatories for a long time. This method, however, has some difficulties such as weather-dependent observation conditions. Therefore, we examined the GNSS method and found that its precision was comparable to the Polaris sighting. We also found that a significant difference of about 10 arcseconds between them. This is due likely to a deflection of vertical (DoV), which is well known in the field of geodetic surveying.
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