Pathways and sources of the warm Atlantic Intermediate Water in the trough system leading to the 79-North Glacier in a high resolution model
More than 25% of mean global sea level rise is caused by mass loss of Greenland Ice Sheet (GrIS). A significant part of this melt is attributed to the interaction between marine terminating glaciers of the GrIS and the surrounding warm ocean waters. However, the sources and pathways of the warm wate...
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ftoceanrep:oai:oceanrep.geomar.de:45265 2023-05-15T16:03:39+02:00 Pathways and sources of the warm Atlantic Intermediate Water in the trough system leading to the 79-North Glacier in a high resolution model He, Yunchang Koszalka, Inga Monika Wekerle, Claudia Schaffer, Janin Kanzow, Torsten 2018 https://oceanrep.geomar.de/id/eprint/45265/ unknown He, Y., Koszalka, I. M. , Wekerle, C., Schaffer, J. and Kanzow, T. (2018) Pathways and sources of the warm Atlantic Intermediate Water in the trough system leading to the 79-North Glacier in a high resolution model. [Poster] In: EGU General Assembly 2018. , 08.-13.04.2018, Vienna, Austria . Geophysical Research Abstracts, 20 (EGU2018-8395-1). info:eu-repo/semantics/closedAccess Conference or Workshop Item NonPeerReviewed 2018 ftoceanrep 2023-04-07T15:43:05Z More than 25% of mean global sea level rise is caused by mass loss of Greenland Ice Sheet (GrIS). A significant part of this melt is attributed to the interaction between marine terminating glaciers of the GrIS and the surrounding warm ocean waters. However, the sources and pathways of the warm waters on the shelf, their variability and mechanisms of the heat transfer involved are variable regionally and yet largely unknown. In this work, we focus on the 79-North Glacier (79-NG), a major glacier in North-East Greenland that was subject to an increased melt in the last years. Recent observations show that Atlantic Intermediate Water (AIW) warmer than 1°C reaches the 79NG via the trough system on the East Greenland continental shelf. In particular, these observations indicate that AIW reaches the glacier rather through the southern Norske Trough than through the northern Westwind Trough. Here we employ Lagrangian modelling and analysis using a high resolution FESOM (Finite Element Sea Ice-Ocean Model) simulation. Particle trajectories representing warm AIW mass are calculated to determine the pathways of this water mass on the adjacent shelf in the Norske Trough, and we analyze the water property changes along the trajectories. Moreover, to identify the sources of the AIW in the vicinity of the 79-NG, we compute backward particle trajectories Conference Object East Greenland glacier Greenland Ice Sheet Sea ice OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Greenland |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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More than 25% of mean global sea level rise is caused by mass loss of Greenland Ice Sheet (GrIS). A significant part of this melt is attributed to the interaction between marine terminating glaciers of the GrIS and the surrounding warm ocean waters. However, the sources and pathways of the warm waters on the shelf, their variability and mechanisms of the heat transfer involved are variable regionally and yet largely unknown. In this work, we focus on the 79-North Glacier (79-NG), a major glacier in North-East Greenland that was subject to an increased melt in the last years. Recent observations show that Atlantic Intermediate Water (AIW) warmer than 1°C reaches the 79NG via the trough system on the East Greenland continental shelf. In particular, these observations indicate that AIW reaches the glacier rather through the southern Norske Trough than through the northern Westwind Trough. Here we employ Lagrangian modelling and analysis using a high resolution FESOM (Finite Element Sea Ice-Ocean Model) simulation. Particle trajectories representing warm AIW mass are calculated to determine the pathways of this water mass on the adjacent shelf in the Norske Trough, and we analyze the water property changes along the trajectories. Moreover, to identify the sources of the AIW in the vicinity of the 79-NG, we compute backward particle trajectories |
format |
Conference Object |
author |
He, Yunchang Koszalka, Inga Monika Wekerle, Claudia Schaffer, Janin Kanzow, Torsten |
spellingShingle |
He, Yunchang Koszalka, Inga Monika Wekerle, Claudia Schaffer, Janin Kanzow, Torsten Pathways and sources of the warm Atlantic Intermediate Water in the trough system leading to the 79-North Glacier in a high resolution model |
author_facet |
He, Yunchang Koszalka, Inga Monika Wekerle, Claudia Schaffer, Janin Kanzow, Torsten |
author_sort |
He, Yunchang |
title |
Pathways and sources of the warm Atlantic Intermediate Water in the trough system leading to the 79-North Glacier in a high resolution model |
title_short |
Pathways and sources of the warm Atlantic Intermediate Water in the trough system leading to the 79-North Glacier in a high resolution model |
title_full |
Pathways and sources of the warm Atlantic Intermediate Water in the trough system leading to the 79-North Glacier in a high resolution model |
title_fullStr |
Pathways and sources of the warm Atlantic Intermediate Water in the trough system leading to the 79-North Glacier in a high resolution model |
title_full_unstemmed |
Pathways and sources of the warm Atlantic Intermediate Water in the trough system leading to the 79-North Glacier in a high resolution model |
title_sort |
pathways and sources of the warm atlantic intermediate water in the trough system leading to the 79-north glacier in a high resolution model |
publishDate |
2018 |
url |
https://oceanrep.geomar.de/id/eprint/45265/ |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
East Greenland glacier Greenland Ice Sheet Sea ice |
genre_facet |
East Greenland glacier Greenland Ice Sheet Sea ice |
op_relation |
He, Y., Koszalka, I. M. , Wekerle, C., Schaffer, J. and Kanzow, T. (2018) Pathways and sources of the warm Atlantic Intermediate Water in the trough system leading to the 79-North Glacier in a high resolution model. [Poster] In: EGU General Assembly 2018. , 08.-13.04.2018, Vienna, Austria . Geophysical Research Abstracts, 20 (EGU2018-8395-1). |
op_rights |
info:eu-repo/semantics/closedAccess |
_version_ |
1766399346437259264 |