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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Main Authors: Beeck S. S., Jensen A. B. O.
Format: Article
Language:English
Published: De Gruyter 2021-09-01
Series:Journal of Geodetic Science
Subjects:
Online Access:https://doi.org/10.1515/jogs-2020-0123
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author Beeck S. S.
Jensen A. B. O.
author_facet Beeck S. S.
Jensen A. B. O.
author_sort Beeck S. S.
collection DOAJ
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.
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spelling doaj.art-653c85d0da4e49c4a7e1076d0f73e5432022-12-22T02:16:43ZengDe GruyterJournal of Geodetic Science2081-99432021-09-01111839410.1515/jogs-2020-0123ROTI maps of Greenland using krigingBeeck S. S.0Jensen A. B. O.1National Space Institute, Technical University of Denmark (DTU Space), 2800 Kongens Lyngby, DenmarkDivision of Geodesy and Satellite Positioning, KTH Royal Institute of Technology, Stockholm, SwedenGNSS 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.https://doi.org/10.1515/jogs-2020-0123arcticglobal navigation satellite systemgreenlandinterpolationionospherekrigingnavigationrate of tec indexscintillationtotal electron content
spellingShingle Beeck S. S.
Jensen A. B. O.
ROTI maps of Greenland using kriging
Journal of Geodetic Science
arctic
global navigation satellite system
greenland
interpolation
ionosphere
kriging
navigation
rate of tec index
scintillation
total electron content
title 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_short ROTI maps of Greenland using kriging
title_sort roti maps of greenland using kriging
topic arctic
global navigation satellite system
greenland
interpolation
ionosphere
kriging
navigation
rate of tec index
scintillation
total electron content
url https://doi.org/10.1515/jogs-2020-0123
work_keys_str_mv AT beeckss rotimapsofgreenlandusingkriging
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