ROTI maps of Greenland using kriging

GNSS satellite signals are affected by the media when traversing Earth’s atmosphere, and the performance of GNSS based positioning and navigation is correlated with these effects. In the ionosphere, the signals are affected by the number of electrons along the signal path which can be quantified by...

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Published in:Journal of Geodetic Science
Main Authors: Beeck, S. S., Jensen, A. B. O.
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/20dd0314-ae59-4769-a42a-5f1dbe094d57
https://doi.org/10.1515/jogs-2020-0123
https://backend.orbit.dtu.dk/ws/files/257667148/10.1515_jogs_2020_0123.pdf
id ftdtupubl:oai:pure.atira.dk:publications/20dd0314-ae59-4769-a42a-5f1dbe094d57
record_format openpolar
spelling ftdtupubl:oai:pure.atira.dk:publications/20dd0314-ae59-4769-a42a-5f1dbe094d57 2024-09-15T18:08:52+00:00 ROTI maps of Greenland using kriging Beeck, S. S. Jensen, A. B. O. 2021 application/pdf https://orbit.dtu.dk/en/publications/20dd0314-ae59-4769-a42a-5f1dbe094d57 https://doi.org/10.1515/jogs-2020-0123 https://backend.orbit.dtu.dk/ws/files/257667148/10.1515_jogs_2020_0123.pdf eng eng https://orbit.dtu.dk/en/publications/20dd0314-ae59-4769-a42a-5f1dbe094d57 info:eu-repo/semantics/openAccess Beeck , S S & Jensen , A B O 2021 , ' ROTI maps of Greenland using kriging ' , Journal of Geodetic Science , vol. 11 , no. 1 , pp. 83-94 . https://doi.org/10.1515/jogs-2020-0123 Arctic Global Navigation Satellite System Greenland Interpolation Ionosphere Kriging Navigation Rate of TEC index Scintillation Total Electron Content article 2021 ftdtupubl https://doi.org/10.1515/jogs-2020-0123 2024-08-13T00:03:06Z GNSS satellite signals are affected by the media when traversing Earth’s atmosphere, and the performance of GNSS based positioning and navigation is correlated with these effects. In the ionosphere, the signals are affected by the number of electrons along the signal path which can be quantified by the total electron content. The focus of this article is scintillation effects caused by electrons in the Arctic ionosphere, and the rate of the total electron content index, the ROTI, is used as a measure of the scintillation. Data from permanent GNSS reference stations in Greenland is used to generate maps of the ROTI in Greenland, and the novelty of the work in this paper is the application of the ordinary kriging method as the basis for ROTI maps in the Arctic. Further, the choice of satellite constellations as well as the elevation mask used in the data analyses are analyzed and discussed. Also, the performance of using ordinary kriging for ROTI maps during times with both a low and a very high geomagnetic activity are discussed. The results show that ordinary kriging performs well during high geomagnetic activity, while during low activity the natural neighbor interpolation method is a better choice for the Arctic. Article in Journal/Newspaper Greenland Technical University of Denmark: DTU Orbit Journal of Geodetic Science 11 1 83 94
institution Open Polar
collection Technical University of Denmark: DTU Orbit
op_collection_id ftdtupubl
language English
topic Arctic
Global Navigation Satellite System
Greenland
Interpolation
Ionosphere
Kriging
Navigation
Rate of TEC index
Scintillation
Total Electron Content
spellingShingle Arctic
Global Navigation Satellite System
Greenland
Interpolation
Ionosphere
Kriging
Navigation
Rate of TEC index
Scintillation
Total Electron Content
Beeck, S. S.
Jensen, A. B. O.
ROTI maps of Greenland using kriging
topic_facet Arctic
Global Navigation Satellite System
Greenland
Interpolation
Ionosphere
Kriging
Navigation
Rate of TEC index
Scintillation
Total Electron Content
description GNSS satellite signals are affected by the media when traversing Earth’s atmosphere, and the performance of GNSS based positioning and navigation is correlated with these effects. In the ionosphere, the signals are affected by the number of electrons along the signal path which can be quantified by the total electron content. The focus of this article is scintillation effects caused by electrons in the Arctic ionosphere, and the rate of the total electron content index, the ROTI, is used as a measure of the scintillation. Data from permanent GNSS reference stations in Greenland is used to generate maps of the ROTI in Greenland, and the novelty of the work in this paper is the application of the ordinary kriging method as the basis for ROTI maps in the Arctic. Further, the choice of satellite constellations as well as the elevation mask used in the data analyses are analyzed and discussed. Also, the performance of using ordinary kriging for ROTI maps during times with both a low and a very high geomagnetic activity are discussed. The results show that ordinary kriging performs well during high geomagnetic activity, while during low activity the natural neighbor interpolation method is a better choice for the Arctic.
format Article in Journal/Newspaper
author Beeck, S. S.
Jensen, A. B. O.
author_facet Beeck, S. S.
Jensen, A. B. O.
author_sort Beeck, S. S.
title ROTI maps of Greenland using kriging
title_short ROTI maps of Greenland using kriging
title_full ROTI maps of Greenland using kriging
title_fullStr ROTI maps of Greenland using kriging
title_full_unstemmed ROTI maps of Greenland using kriging
title_sort roti maps of greenland using kriging
publishDate 2021
url https://orbit.dtu.dk/en/publications/20dd0314-ae59-4769-a42a-5f1dbe094d57
https://doi.org/10.1515/jogs-2020-0123
https://backend.orbit.dtu.dk/ws/files/257667148/10.1515_jogs_2020_0123.pdf
genre Greenland
genre_facet Greenland
op_source Beeck , S S & Jensen , A B O 2021 , ' ROTI maps of Greenland using kriging ' , Journal of Geodetic Science , vol. 11 , no. 1 , pp. 83-94 . https://doi.org/10.1515/jogs-2020-0123
op_relation https://orbit.dtu.dk/en/publications/20dd0314-ae59-4769-a42a-5f1dbe094d57
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1515/jogs-2020-0123
container_title Journal of Geodetic Science
container_volume 11
container_issue 1
container_start_page 83
op_container_end_page 94
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