Frontogenesis and variability in Denmark Strait and its influence on overflow water

Spall, Michael A.; Pickart, Robert S.; Lin, Peigen; Appen, Wilken-Jon von; Mastropole, Dana; Valdimarsson, H.; Haine, Thomas W. N.; Almansi, Mattia ORCID: https://orcid.org/0000-0001-6849-3647. 2019 Frontogenesis and variability in Denmark Strait and its influence on overflow water. Journal of Physical Oceanography, 49 (7). 1889-1904. 10.1175/jpo-d-19-0053.1

Before downloading, please read NORA policies.

Preview

Text [15200485 - Journal of Physical Oceanography] Frontogenesis and Variability in Denmark Strait and Its Influence on Overflow Water.pdf - Published Version Available under License Creative Commons Attribution Non-commercial No Derivatives 4.0. Download (3MB) | Preview

Abstract/Summary

A high-resolution numerical model, together with in situ and satellite observations, is used to explore the nature and dynamics of the dominant high-frequency (from one day to one week) variability in Denmark Strait. Mooring measurements in the center of the strait reveal that warm water “flooding events” occur, whereby the North Icelandic Irminger Current (NIIC) propagates offshore and advects subtropical-origin water northward through the deepest part of the sill. Two other types of mesoscale processes in Denmark Strait have been described previously in the literature, known as “boluses” and “pulses,” associated with a raising and lowering of the overflow water interface. Our measurements reveal that flooding events occur in conjunction with especially pronounced pulses. The model indicates that the NIIC hydrographic front is maintained by a balance between frontogenesis by the large-scale flow and frontolysis by baroclinic instability. Specifically, the temperature and salinity tendency equations demonstrate that the eddies act to relax the front, while the mean flow acts to sharpen it. Furthermore, the model reveals that the two dense water processes—boluses and pulses (and hence flooding events)—are dynamically related to each other and tied to the meandering of the hydrographic front in the strait. Our study thus provides a general framework for interpreting the short-time-scale variability of Denmark Strait Overflow Water entering the Irminger Sea.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1175/jpo-d-19-0053.1
ISSN:	0022-3670
Date made live:	21 Apr 2021 14:03 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/530124

Actions (login required)

View Item

Document Downloads

More statistics for this item...