Ice Elevation Change Based on GNSS Measurements along the Korth-Traverse in Southern Greenland
In 1912, a Swiss expedition led by meteorologist Alfred de Quervain crossed the Greenland ice sheet on a route from Disko Bay to Tasiilaq. Based on that, in 2002, a series of geodetic expeditions carried out by W. Korth and later by T. Hitziger began along the same traverse as in 1912, with the last...
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ftdoajarticles:oai:doaj.org/article:c4347fed29364f38a44cb05e2c960587 2023-05-15T16:01:04+02:00 Ice Elevation Change Based on GNSS Measurements along the Korth-Traverse in Southern Greenland Thomas Hitziger Luisa Näke Karel Pavelka 2022-11-01T00:00:00Z https://doi.org/10.3390/app122312066 https://doaj.org/article/c4347fed29364f38a44cb05e2c960587 EN eng MDPI AG https://www.mdpi.com/2076-3417/12/23/12066 https://doaj.org/toc/2076-3417 doi:10.3390/app122312066 2076-3417 https://doaj.org/article/c4347fed29364f38a44cb05e2c960587 Applied Sciences, Vol 12, Iss 12066, p 12066 (2022) Greenland ice sheet monitoring GNSS expedition Jakobshavn Isbræ Helheim Glacier Technology T Engineering (General). Civil engineering (General) TA1-2040 Biology (General) QH301-705.5 Physics QC1-999 Chemistry QD1-999 article 2022 ftdoajarticles https://doi.org/10.3390/app122312066 2022-12-30T20:05:40Z In 1912, a Swiss expedition led by meteorologist Alfred de Quervain crossed the Greenland ice sheet on a route from Disko Bay to Tasiilaq. Based on that, in 2002, a series of geodetic expeditions carried out by W. Korth and later by T. Hitziger began along the same traverse as in 1912, with the last measurements taken in May 2021. The statically collected GPS/GNSS data provide very accurate elevation changes at 36 points along the almost 700 km long crossing over a period of 19 years. According to this, there is a maximum increase of 2.1 m in the central area and a decrease of up to 38.7 m towards the coasts (influence Ilulissat Isbræ). By using kinematic GNSS measurements, there is a very dense profile with a spacing of a few meters. The comparison of those measurements is performed using crossing points or minimum distances and gives equivalent results for both methods. It is shown that local ice topography is preserved, and thus gaps in data sets can be caught. Areas of accumulation and ablation on the ice sheet can be identified, showing the widespread influence of outlet glaciers up to 200 km. The data can be used for direct verification of altimetry data, such as IceSat. Both IceSat elevations and their changes can be compared. Article in Journal/Newspaper Disko Bay glacier Greenland Ice Sheet Ilulissat Jakobshavn Jakobshavn isbræ Tasiilaq Directory of Open Access Journals: DOAJ Articles Greenland Ilulissat ENVELOPE(-51.099,-51.099,69.220,69.220) Jakobshavn Isbræ ENVELOPE(-49.917,-49.917,69.167,69.167) Tasiilaq ENVELOPE(-37.637,-37.637,65.615,65.615) Applied Sciences 12 23 12066 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Greenland ice sheet monitoring GNSS expedition Jakobshavn Isbræ Helheim Glacier Technology T Engineering (General). Civil engineering (General) TA1-2040 Biology (General) QH301-705.5 Physics QC1-999 Chemistry QD1-999 |
spellingShingle |
Greenland ice sheet monitoring GNSS expedition Jakobshavn Isbræ Helheim Glacier Technology T Engineering (General). Civil engineering (General) TA1-2040 Biology (General) QH301-705.5 Physics QC1-999 Chemistry QD1-999 Thomas Hitziger Luisa Näke Karel Pavelka Ice Elevation Change Based on GNSS Measurements along the Korth-Traverse in Southern Greenland |
topic_facet |
Greenland ice sheet monitoring GNSS expedition Jakobshavn Isbræ Helheim Glacier Technology T Engineering (General). Civil engineering (General) TA1-2040 Biology (General) QH301-705.5 Physics QC1-999 Chemistry QD1-999 |
description |
In 1912, a Swiss expedition led by meteorologist Alfred de Quervain crossed the Greenland ice sheet on a route from Disko Bay to Tasiilaq. Based on that, in 2002, a series of geodetic expeditions carried out by W. Korth and later by T. Hitziger began along the same traverse as in 1912, with the last measurements taken in May 2021. The statically collected GPS/GNSS data provide very accurate elevation changes at 36 points along the almost 700 km long crossing over a period of 19 years. According to this, there is a maximum increase of 2.1 m in the central area and a decrease of up to 38.7 m towards the coasts (influence Ilulissat Isbræ). By using kinematic GNSS measurements, there is a very dense profile with a spacing of a few meters. The comparison of those measurements is performed using crossing points or minimum distances and gives equivalent results for both methods. It is shown that local ice topography is preserved, and thus gaps in data sets can be caught. Areas of accumulation and ablation on the ice sheet can be identified, showing the widespread influence of outlet glaciers up to 200 km. The data can be used for direct verification of altimetry data, such as IceSat. Both IceSat elevations and their changes can be compared. |
format |
Article in Journal/Newspaper |
author |
Thomas Hitziger Luisa Näke Karel Pavelka |
author_facet |
Thomas Hitziger Luisa Näke Karel Pavelka |
author_sort |
Thomas Hitziger |
title |
Ice Elevation Change Based on GNSS Measurements along the Korth-Traverse in Southern Greenland |
title_short |
Ice Elevation Change Based on GNSS Measurements along the Korth-Traverse in Southern Greenland |
title_full |
Ice Elevation Change Based on GNSS Measurements along the Korth-Traverse in Southern Greenland |
title_fullStr |
Ice Elevation Change Based on GNSS Measurements along the Korth-Traverse in Southern Greenland |
title_full_unstemmed |
Ice Elevation Change Based on GNSS Measurements along the Korth-Traverse in Southern Greenland |
title_sort |
ice elevation change based on gnss measurements along the korth-traverse in southern greenland |
publisher |
MDPI AG |
publishDate |
2022 |
url |
https://doi.org/10.3390/app122312066 https://doaj.org/article/c4347fed29364f38a44cb05e2c960587 |
long_lat |
ENVELOPE(-51.099,-51.099,69.220,69.220) ENVELOPE(-49.917,-49.917,69.167,69.167) ENVELOPE(-37.637,-37.637,65.615,65.615) |
geographic |
Greenland Ilulissat Jakobshavn Isbræ Tasiilaq |
geographic_facet |
Greenland Ilulissat Jakobshavn Isbræ Tasiilaq |
genre |
Disko Bay glacier Greenland Ice Sheet Ilulissat Jakobshavn Jakobshavn isbræ Tasiilaq |
genre_facet |
Disko Bay glacier Greenland Ice Sheet Ilulissat Jakobshavn Jakobshavn isbræ Tasiilaq |
op_source |
Applied Sciences, Vol 12, Iss 12066, p 12066 (2022) |
op_relation |
https://www.mdpi.com/2076-3417/12/23/12066 https://doaj.org/toc/2076-3417 doi:10.3390/app122312066 2076-3417 https://doaj.org/article/c4347fed29364f38a44cb05e2c960587 |
op_doi |
https://doi.org/10.3390/app122312066 |
container_title |
Applied Sciences |
container_volume |
12 |
container_issue |
23 |
container_start_page |
12066 |
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1766397065078767616 |