Monitoring global climate change using SLR data from LARES and other geodetic satellites
The Earth Orientation Parameters (EOP), i.e. the spin axis of the Earth, is influenced by the mass redistribution inside and on the surface of the Earth. On the Earth surface, global ice melting, sea level change and atmospheric circulation are the prime contributors. Recent studies have unraveled t...
Published in: | SPIE Proceedings, Sensors and Smart Structures Technologies for Civil, Mechanical, and Aerospace Systems 2016 |
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Main Authors: | , , , , |
Other Authors: | , , , , |
Format: | Conference Object |
Language: | English |
Published: |
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2016
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Online Access: | http://hdl.handle.net/11573/951821 https://doi.org/10.1117/12.2222149 http://spie.org/x1848.xml |
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author | PAOLOZZI, Antonio PARIS, Claudio Pavlis, Erricos C. SINDONI, GIAMPIERO CIUFOLINI, IGNAZIO |
author2 | Jerome P. Lynch Paolozzi, Antonio Paris, Claudio Pavlis, Erricos C. Sindoni, Giampiero Ciufolini, Ignazio |
author_facet | PAOLOZZI, Antonio PARIS, Claudio Pavlis, Erricos C. SINDONI, GIAMPIERO CIUFOLINI, IGNAZIO |
author_sort | PAOLOZZI, Antonio |
collection | Sapienza Università di Roma: CINECA IRIS |
container_start_page | 98034N |
container_title | SPIE Proceedings, Sensors and Smart Structures Technologies for Civil, Mechanical, and Aerospace Systems 2016 |
container_volume | 9803 |
description | The Earth Orientation Parameters (EOP), i.e. the spin axis of the Earth, is influenced by the mass redistribution inside and on the surface of the Earth. On the Earth surface, global ice melting, sea level change and atmospheric circulation are the prime contributors. Recent studies have unraveled the majority of the mysteries behind the Chandler wobble, the annual motion and the secular motion of the pole. The differences from the motion of a pole for a rigid Earth is indeed due to the mass redistribution and transfer of angular momentum among the atmosphere, the oceans and solid Earth. The technique of laser ranging and the use of laser ranged satellites such as LARES along with other techniques such Very Long Baseline Interferometry (VLBI) allow to measure the EOP with accuracies at the level of ~200 μas which correspond to few millimeters at the Earth's surface, while the use of Global Navigation Satellite System (GNSS) data can reach an accuracy even below 100 μas. At these unprecedented high levels of accuracy, even tiny anomalous behavior in EOP can be observed and thus correlated to global environmental changes such as ice melting on Greenland and the polar caps, and extreme events that involve strong ocean-atmosphere coupling interactions such as the El Niño. The contribution of Satellite Laser Ranging (SLR) data such as from the LARES mission and similar satellites to this area is outlined in this paper. |
format | Conference Object |
genre | Greenland |
genre_facet | Greenland |
geographic | Greenland Chandler |
geographic_facet | Greenland Chandler |
id | ftunivromairis:oai:iris.uniroma1.it:11573/951821 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-59.682,-59.682,-64.490,-64.490) |
op_collection_id | ftunivromairis |
op_doi | https://doi.org/10.1117/12.2222149 |
op_relation | info:eu-repo/semantics/altIdentifier/isbn/9781510600447 info:eu-repo/semantics/altIdentifier/wos/WOS:000382319400126 ispartofbook:Proceedings of SPIE - The International Society for Optical Engineering Sensors and Smart Structures Technologies for Civil, Mechanical, and Aerospace Systems 2016 volume:9803 firstpage:1 lastpage:9 numberofpages:9 http://hdl.handle.net/11573/951821 doi:10.1117/12.2222149 http://spie.org/x1848.xml |
op_rights | info:eu-repo/semantics/restrictedAccess |
publishDate | 2016 |
publisher | SPIE |
record_format | openpolar |
spelling | ftunivromairis:oai:iris.uniroma1.it:11573/951821 2025-05-04T14:26:32+00:00 Monitoring global climate change using SLR data from LARES and other geodetic satellites PAOLOZZI, Antonio PARIS, Claudio Pavlis, Erricos C. SINDONI, GIAMPIERO CIUFOLINI, IGNAZIO Jerome P. Lynch Paolozzi, Antonio Paris, Claudio Pavlis, Erricos C. Sindoni, Giampiero Ciufolini, Ignazio 2016 http://hdl.handle.net/11573/951821 https://doi.org/10.1117/12.2222149 http://spie.org/x1848.xml eng eng SPIE info:eu-repo/semantics/altIdentifier/isbn/9781510600447 info:eu-repo/semantics/altIdentifier/wos/WOS:000382319400126 ispartofbook:Proceedings of SPIE - The International Society for Optical Engineering Sensors and Smart Structures Technologies for Civil, Mechanical, and Aerospace Systems 2016 volume:9803 firstpage:1 lastpage:9 numberofpages:9 http://hdl.handle.net/11573/951821 doi:10.1117/12.2222149 http://spie.org/x1848.xml info:eu-repo/semantics/restrictedAccess Electronic Optical and Magnetic Material Condensed Matter Physic Computer Science Applications1707 Computer Vision and Pattern Recognition Applied Mathematic Electrical and Electronic Engineering info:eu-repo/semantics/conferenceObject 2016 ftunivromairis https://doi.org/10.1117/12.2222149 2025-04-10T14:52:02Z The Earth Orientation Parameters (EOP), i.e. the spin axis of the Earth, is influenced by the mass redistribution inside and on the surface of the Earth. On the Earth surface, global ice melting, sea level change and atmospheric circulation are the prime contributors. Recent studies have unraveled the majority of the mysteries behind the Chandler wobble, the annual motion and the secular motion of the pole. The differences from the motion of a pole for a rigid Earth is indeed due to the mass redistribution and transfer of angular momentum among the atmosphere, the oceans and solid Earth. The technique of laser ranging and the use of laser ranged satellites such as LARES along with other techniques such Very Long Baseline Interferometry (VLBI) allow to measure the EOP with accuracies at the level of ~200 μas which correspond to few millimeters at the Earth's surface, while the use of Global Navigation Satellite System (GNSS) data can reach an accuracy even below 100 μas. At these unprecedented high levels of accuracy, even tiny anomalous behavior in EOP can be observed and thus correlated to global environmental changes such as ice melting on Greenland and the polar caps, and extreme events that involve strong ocean-atmosphere coupling interactions such as the El Niño. The contribution of Satellite Laser Ranging (SLR) data such as from the LARES mission and similar satellites to this area is outlined in this paper. Conference Object Greenland Sapienza Università di Roma: CINECA IRIS Greenland Chandler ENVELOPE(-59.682,-59.682,-64.490,-64.490) SPIE Proceedings, Sensors and Smart Structures Technologies for Civil, Mechanical, and Aerospace Systems 2016 9803 98034N |
spellingShingle | Electronic Optical and Magnetic Material Condensed Matter Physic Computer Science Applications1707 Computer Vision and Pattern Recognition Applied Mathematic Electrical and Electronic Engineering PAOLOZZI, Antonio PARIS, Claudio Pavlis, Erricos C. SINDONI, GIAMPIERO CIUFOLINI, IGNAZIO Monitoring global climate change using SLR data from LARES and other geodetic satellites |
title | Monitoring global climate change using SLR data from LARES and other geodetic satellites |
title_full | Monitoring global climate change using SLR data from LARES and other geodetic satellites |
title_fullStr | Monitoring global climate change using SLR data from LARES and other geodetic satellites |
title_full_unstemmed | Monitoring global climate change using SLR data from LARES and other geodetic satellites |
title_short | Monitoring global climate change using SLR data from LARES and other geodetic satellites |
title_sort | monitoring global climate change using slr data from lares and other geodetic satellites |
topic | Electronic Optical and Magnetic Material Condensed Matter Physic Computer Science Applications1707 Computer Vision and Pattern Recognition Applied Mathematic Electrical and Electronic Engineering |
topic_facet | Electronic Optical and Magnetic Material Condensed Matter Physic Computer Science Applications1707 Computer Vision and Pattern Recognition Applied Mathematic Electrical and Electronic Engineering |
url | http://hdl.handle.net/11573/951821 https://doi.org/10.1117/12.2222149 http://spie.org/x1848.xml |