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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oai:doaj.org-article:653c85d0da4e49c4a7e1076d0f73e5432021-12-05T14:10:52ZROTI maps of Greenland using kriging2081-994310.1515/jogs-2020-0123https://doaj.org/article/653c85d0da4e49c4a7e1076d0f73e5432021-09-01T00:00:00Zhttps://doi.org/10.1515/jogs-2020-0123https://doaj.org/toc/2081-9943GNSS 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.Beeck S. S.Jensen A. B. O.Sciendoarticlearcticglobal navigation satellite systemgreenlandinterpolationionospherekrigingnavigationrate of tec indexscintillationtotal electron contentGeodesyQB275-343ENJournal of Geodetic Science, Vol 11, Iss 1, Pp 83-94 (2021) |
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arctic global navigation satellite system greenland interpolation ionosphere kriging navigation rate of tec index scintillation total electron content Geodesy QB275-343 |
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arctic global navigation satellite system greenland interpolation ionosphere kriging navigation rate of tec index scintillation total electron content Geodesy QB275-343 Beeck S. S. Jensen A. B. O. ROTI maps of Greenland using kriging |
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. |
format |
article |
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 |
publisher |
Sciendo |
publishDate |
2021 |
url |
https://doaj.org/article/653c85d0da4e49c4a7e1076d0f73e543 |
work_keys_str_mv |
AT beeckss rotimapsofgreenlandusingkriging AT jensenabo rotimapsofgreenlandusingkriging |
_version_ |
1718371645605806080 |