Evaluating altimetry-derived surface currents on the south Greenland shelf with surface drifters

The pathways and fate of freshwater in the East Greenland Coastal Current (EGCC) are crucial to the climate system. The EGCC transports large amounts of freshwater in close proximity to sites of deep open-ocean convection in the Labrador and Irminger seas. Many studies have attempted to analyze this...

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Published in:Ocean Science
Main Authors: A. Coquereau, N. P. Foukal
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
G
Online Access:https://doi.org/10.5194/os-19-1393-2023
https://doaj.org/article/04ec259e18f14fa18b384162d2fb333d
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spelling ftdoajarticles:oai:doaj.org/article:04ec259e18f14fa18b384162d2fb333d 2023-10-09T21:51:07+02:00 Evaluating altimetry-derived surface currents on the south Greenland shelf with surface drifters A. Coquereau N. P. Foukal 2023-09-01T00:00:00Z https://doi.org/10.5194/os-19-1393-2023 https://doaj.org/article/04ec259e18f14fa18b384162d2fb333d EN eng Copernicus Publications https://os.copernicus.org/articles/19/1393/2023/os-19-1393-2023.pdf https://doaj.org/toc/1812-0784 https://doaj.org/toc/1812-0792 doi:10.5194/os-19-1393-2023 1812-0784 1812-0792 https://doaj.org/article/04ec259e18f14fa18b384162d2fb333d Ocean Science, Vol 19, Pp 1393-1411 (2023) Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2023 ftdoajarticles https://doi.org/10.5194/os-19-1393-2023 2023-09-24T00:37:17Z The pathways and fate of freshwater in the East Greenland Coastal Current (EGCC) are crucial to the climate system. The EGCC transports large amounts of freshwater in close proximity to sites of deep open-ocean convection in the Labrador and Irminger seas. Many studies have attempted to analyze this system from models and various observational platforms, but the modeling results largely disagree with one another, and observations are limited due to the harsh conditions typical of the region. Altimetry-derived surface currents, constructed from remote-sensing observations and applying geostrophic equations, provide a continuous observational data set beginning in 1993. However, these products have historically encountered difficulties in coastal regions, and thus their validity must be checked. In this work, we use a comprehensive methodology to compare these Eulerian data to a Lagrangian data set of 34 surface drifter trajectories and demonstrate that the altimetry-derived surface currents are surprisingly capable of recovering the spatial structure of the flow field on the south Greenland shelf and can mimic the Lagrangian nature of the flow as observed from surface drifters. Article in Journal/Newspaper East Greenland Greenland Directory of Open Access Journals: DOAJ Articles Greenland Ocean Science 19 5 1393 1411
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
spellingShingle Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
A. Coquereau
N. P. Foukal
Evaluating altimetry-derived surface currents on the south Greenland shelf with surface drifters
topic_facet Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
description The pathways and fate of freshwater in the East Greenland Coastal Current (EGCC) are crucial to the climate system. The EGCC transports large amounts of freshwater in close proximity to sites of deep open-ocean convection in the Labrador and Irminger seas. Many studies have attempted to analyze this system from models and various observational platforms, but the modeling results largely disagree with one another, and observations are limited due to the harsh conditions typical of the region. Altimetry-derived surface currents, constructed from remote-sensing observations and applying geostrophic equations, provide a continuous observational data set beginning in 1993. However, these products have historically encountered difficulties in coastal regions, and thus their validity must be checked. In this work, we use a comprehensive methodology to compare these Eulerian data to a Lagrangian data set of 34 surface drifter trajectories and demonstrate that the altimetry-derived surface currents are surprisingly capable of recovering the spatial structure of the flow field on the south Greenland shelf and can mimic the Lagrangian nature of the flow as observed from surface drifters.
format Article in Journal/Newspaper
author A. Coquereau
N. P. Foukal
author_facet A. Coquereau
N. P. Foukal
author_sort A. Coquereau
title Evaluating altimetry-derived surface currents on the south Greenland shelf with surface drifters
title_short Evaluating altimetry-derived surface currents on the south Greenland shelf with surface drifters
title_full Evaluating altimetry-derived surface currents on the south Greenland shelf with surface drifters
title_fullStr Evaluating altimetry-derived surface currents on the south Greenland shelf with surface drifters
title_full_unstemmed Evaluating altimetry-derived surface currents on the south Greenland shelf with surface drifters
title_sort evaluating altimetry-derived surface currents on the south greenland shelf with surface drifters
publisher Copernicus Publications
publishDate 2023
url https://doi.org/10.5194/os-19-1393-2023
https://doaj.org/article/04ec259e18f14fa18b384162d2fb333d
geographic Greenland
geographic_facet Greenland
genre East Greenland
Greenland
genre_facet East Greenland
Greenland
op_source Ocean Science, Vol 19, Pp 1393-1411 (2023)
op_relation https://os.copernicus.org/articles/19/1393/2023/os-19-1393-2023.pdf
https://doaj.org/toc/1812-0784
https://doaj.org/toc/1812-0792
doi:10.5194/os-19-1393-2023
1812-0784
1812-0792
https://doaj.org/article/04ec259e18f14fa18b384162d2fb333d
op_doi https://doi.org/10.5194/os-19-1393-2023
container_title Ocean Science
container_volume 19
container_issue 5
container_start_page 1393
op_container_end_page 1411
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