Measuring Earth: Current status of the GRACE Follow-On Laser Ranging Interferometer
The GRACE mission that was launched in 2002 has impressively proven the feasibility of low-orbit satellite-to-satellite tracking for Earth gravity observations. Especially mass transport related to Earth's hydrological system could be well resolved both spatially and temporally. This allows to...
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ftdatacite:10.15488/708 2023-05-15T16:40:59+02:00 Measuring Earth: Current status of the GRACE Follow-On Laser Ranging Interferometer Schütze, Daniel 2016 https://dx.doi.org/10.15488/708 http://www.repo.uni-hannover.de/handle/123456789/732 en eng Bristol : Institute of Physics Publishing Creative Commons Attribution 3.0 Unported CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Geodetic satellites Gravitational effects Gravity waves Groundwater Interferometers NASA Orbits Flight hardware Gravitational wave detectors Ground water depletions Hydrological system Intersatellite distance Low-orbit satellites Gravitationswelle Dewey Decimal Classification500 | Naturwissenschaften Dewey Decimal Classification500 | Naturwissenschaften530 | Physik article Other CreativeWork 2016 ftdatacite https://doi.org/10.15488/708 2022-02-09T12:33:12Z The GRACE mission that was launched in 2002 has impressively proven the feasibility of low-orbit satellite-to-satellite tracking for Earth gravity observations. Especially mass transport related to Earth's hydrological system could be well resolved both spatially and temporally. This allows to study processes such as polar ice sheet decline and ground water depletion in great detail. Owing to GRACE's success, NASA and GFZ will launch the successor mission GRACE Follow-On in 2017. In addition to the microwave ranging system, GRACE Follow-On will be the first mission to use a Laser Ranging Interferometer as technology demonstrator to track intersatellite distance changes with unprecedented precision. This new ranging device inherits some of the technologies which have been developed for the future spaceborne gravitational wave detector LISA. I will present the architecture of the Laser Ranging Interferometer, point out similarities and differences to LISA, and conclude with the current status of the flight hardware production. Article in Journal/Newspaper Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Dewey ENVELOPE(-64.320,-64.320,-65.907,-65.907) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Geodetic satellites Gravitational effects Gravity waves Groundwater Interferometers NASA Orbits Flight hardware Gravitational wave detectors Ground water depletions Hydrological system Intersatellite distance Low-orbit satellites Gravitationswelle Dewey Decimal Classification500 | Naturwissenschaften Dewey Decimal Classification500 | Naturwissenschaften530 | Physik |
spellingShingle |
Geodetic satellites Gravitational effects Gravity waves Groundwater Interferometers NASA Orbits Flight hardware Gravitational wave detectors Ground water depletions Hydrological system Intersatellite distance Low-orbit satellites Gravitationswelle Dewey Decimal Classification500 | Naturwissenschaften Dewey Decimal Classification500 | Naturwissenschaften530 | Physik Schütze, Daniel Measuring Earth: Current status of the GRACE Follow-On Laser Ranging Interferometer |
topic_facet |
Geodetic satellites Gravitational effects Gravity waves Groundwater Interferometers NASA Orbits Flight hardware Gravitational wave detectors Ground water depletions Hydrological system Intersatellite distance Low-orbit satellites Gravitationswelle Dewey Decimal Classification500 | Naturwissenschaften Dewey Decimal Classification500 | Naturwissenschaften530 | Physik |
description |
The GRACE mission that was launched in 2002 has impressively proven the feasibility of low-orbit satellite-to-satellite tracking for Earth gravity observations. Especially mass transport related to Earth's hydrological system could be well resolved both spatially and temporally. This allows to study processes such as polar ice sheet decline and ground water depletion in great detail. Owing to GRACE's success, NASA and GFZ will launch the successor mission GRACE Follow-On in 2017. In addition to the microwave ranging system, GRACE Follow-On will be the first mission to use a Laser Ranging Interferometer as technology demonstrator to track intersatellite distance changes with unprecedented precision. This new ranging device inherits some of the technologies which have been developed for the future spaceborne gravitational wave detector LISA. I will present the architecture of the Laser Ranging Interferometer, point out similarities and differences to LISA, and conclude with the current status of the flight hardware production. |
format |
Article in Journal/Newspaper |
author |
Schütze, Daniel |
author_facet |
Schütze, Daniel |
author_sort |
Schütze, Daniel |
title |
Measuring Earth: Current status of the GRACE Follow-On Laser Ranging Interferometer |
title_short |
Measuring Earth: Current status of the GRACE Follow-On Laser Ranging Interferometer |
title_full |
Measuring Earth: Current status of the GRACE Follow-On Laser Ranging Interferometer |
title_fullStr |
Measuring Earth: Current status of the GRACE Follow-On Laser Ranging Interferometer |
title_full_unstemmed |
Measuring Earth: Current status of the GRACE Follow-On Laser Ranging Interferometer |
title_sort |
measuring earth: current status of the grace follow-on laser ranging interferometer |
publisher |
Bristol : Institute of Physics Publishing |
publishDate |
2016 |
url |
https://dx.doi.org/10.15488/708 http://www.repo.uni-hannover.de/handle/123456789/732 |
long_lat |
ENVELOPE(-64.320,-64.320,-65.907,-65.907) |
geographic |
Dewey |
geographic_facet |
Dewey |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_rights |
Creative Commons Attribution 3.0 Unported CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.15488/708 |
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1766031414810116096 |