Effects of space weather on GOCE electrostatic gravity gradiometer measurements

We examine the presence of residual nongravitational signatures in gravitational gradients measured by GOCE electrostatic gravity gradiometer. These signatures are observed over the magnetic poles during geomagnetically active days and can contaminate the trace of the gravitational gradient tensor b...

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Published in:Journal of Geodesy
Main Authors: Ince, E., Pagiatakis, S.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2016
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_2653924
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_2653924 2023-05-15T16:29:19+02:00 Effects of space weather on GOCE electrostatic gravity gradiometer measurements Ince, E. Pagiatakis, S. 2016 https://gfzpublic.gfz-potsdam.de/pubman/item/item_2653924 unknown info:eu-repo/semantics/altIdentifier/doi/10.1007/s00190-016-0931-8 https://gfzpublic.gfz-potsdam.de/pubman/item/item_2653924 Journal of Geodesy info:eu-repo/semantics/article 2016 ftgfzpotsdam https://doi.org/10.1007/s00190-016-0931-8 2022-09-14T05:53:42Z We examine the presence of residual nongravitational signatures in gravitational gradients measured by GOCE electrostatic gravity gradiometer. These signatures are observed over the magnetic poles during geomagnetically active days and can contaminate the trace of the gravitational gradient tensor by up to three to five times the expected noise level of the instrument ( ∼∼11 mE). We investigate these anomalies in the gradiometer measurements along many satellite tracks and examine possible causes using external datasets, such as interplanetary electric field measurements from the ACE (advanced composition explorer) and WIND spacecraft, and Poynting vector (flux) estimated from equivalent ionospheric currents derived from spherical elementary current systems over North America and Greenland. We show that the variations in the east-west and vertical electrical currents and Poynting vector components at the satellite position are highly correlated with the disturbances observed in the gradiometer measurements. The results presented in this paper reveal that the disturbances are due to intense ionospheric current variations that are enhanced by increased solar activity that causes a very dynamic drag environment. Moreover, successful modelling and removal of a high percentage of these disturbances are possible using external geomagnetic field observations. Article in Journal/Newspaper Greenland GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Greenland Journal of Geodesy 90 12 1389 1403
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language unknown
description We examine the presence of residual nongravitational signatures in gravitational gradients measured by GOCE electrostatic gravity gradiometer. These signatures are observed over the magnetic poles during geomagnetically active days and can contaminate the trace of the gravitational gradient tensor by up to three to five times the expected noise level of the instrument ( ∼∼11 mE). We investigate these anomalies in the gradiometer measurements along many satellite tracks and examine possible causes using external datasets, such as interplanetary electric field measurements from the ACE (advanced composition explorer) and WIND spacecraft, and Poynting vector (flux) estimated from equivalent ionospheric currents derived from spherical elementary current systems over North America and Greenland. We show that the variations in the east-west and vertical electrical currents and Poynting vector components at the satellite position are highly correlated with the disturbances observed in the gradiometer measurements. The results presented in this paper reveal that the disturbances are due to intense ionospheric current variations that are enhanced by increased solar activity that causes a very dynamic drag environment. Moreover, successful modelling and removal of a high percentage of these disturbances are possible using external geomagnetic field observations.
format Article in Journal/Newspaper
author Ince, E.
Pagiatakis, S.
spellingShingle Ince, E.
Pagiatakis, S.
Effects of space weather on GOCE electrostatic gravity gradiometer measurements
author_facet Ince, E.
Pagiatakis, S.
author_sort Ince, E.
title Effects of space weather on GOCE electrostatic gravity gradiometer measurements
title_short Effects of space weather on GOCE electrostatic gravity gradiometer measurements
title_full Effects of space weather on GOCE electrostatic gravity gradiometer measurements
title_fullStr Effects of space weather on GOCE electrostatic gravity gradiometer measurements
title_full_unstemmed Effects of space weather on GOCE electrostatic gravity gradiometer measurements
title_sort effects of space weather on goce electrostatic gravity gradiometer measurements
publishDate 2016
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_2653924
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_source Journal of Geodesy
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1007/s00190-016-0931-8
https://gfzpublic.gfz-potsdam.de/pubman/item/item_2653924
op_doi https://doi.org/10.1007/s00190-016-0931-8
container_title Journal of Geodesy
container_volume 90
container_issue 12
container_start_page 1389
op_container_end_page 1403
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