Cyclonic Eddies in the West Greenland Boundary Current System
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phoc-JPO-D-20-0255.1.pdf
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Checksum (MD5)
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Author(s)
Pacini, Astrid
Pickart, Robert
Le Bras, Isabela
Straneo, Fiammetta
Holliday, N
Spall, Michael
Date Issued
June 8, 2021
Journal
Journal of Physical Oceanography
Publisher
American Meteorological Society
Citation
Pacini, A., R. S. Pickart, I. A. Le Bras, F. Straneo, N. P. Holliday, and M. A. Spall, 2021: Cyclonic Eddies in the West Greenland Boundary Current System. J. Phys. Oceanogr., 51, 2087–2102.
Version
Final published version
Abstract
The boundary current system in the Labrador Sea plays an integral role in modulating convection in the interior basin. Four years of mooring data from the eastern Labrador Sea reveal persistent mesoscale variability in the West Greenland boundary current. Between 2014 and 2018, 197 middepth intensified cyclones were identified that passed the array near the 2000-m isobath. In this study, we quantify these features and show that they are the downstream manifestation of Denmark Strait Overflow Water (DSOW) cyclones. A composite cyclone is constructed revealing an average radius of 9 km, maximum azimuthal speed of 24 cm s−1, and a core propagation velocity of 27 cm s−1. The core propagation velocity is significantly smaller than upstream near Denmark Strait, allowing them to trap more water. The cyclones transport a 200-m-thick lens of dense water at the bottom of the water column and increase the transport of DSOW in the West Greenland boundary current by 17% relative to the background flow. Only a portion of the features generated at Denmark Strait make it to the Labrador Sea, implying that the remainder are shed into the interior Irminger Sea, are retroflected at Cape Farewell, or dissipate. A synoptic shipboard survey east of Cape Farewell, conducted in summer 2020, captured two of these features that shed further light on their structure and timing. This is the first time DSOW cyclones have been observed in the Labrador Sea—a discovery that could have important implications for interior stratification.
Subjects
Boundary currents
Eddies
Transport
Terms of Use
Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.
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DOI of Published Version
https://doi.org/10.1175/JPO-D-20-0255.1
