On the origin of water masses in the Beaufort Gyre

Kelly, S. J.; Proshutinsky, A.; Popova, E. K. ORCID: https://orcid.org/0000-0002-2012-708X; Aksenov, Y. K. ORCID: https://orcid.org/0000-0001-6132-3434; Yool, A. ORCID: https://orcid.org/0000-0002-9879-2776. 2019 On the origin of water masses in the Beaufort Gyre. Journal of Geophysical Research: Oceans, 124 (7). 4696-4709. https://doi.org/10.1029/2019JC015022

Before downloading, please read NORA policies.

Preview

Text
Kelly_et_al-2019-Journal_of_Geophysical_Research__Oceans.pdf
Available under License Creative Commons Attribution 4.0.
Download (2MB) | Preview

Official URL: http://dx.doi.org/10.1029/2019JC015022

Abstract/Summary

The Beaufort Gyre is a key feature of the Arctic Ocean, acting as a reservoir for freshwater in the region. Depending on whether the prevailing atmospheric circulation in the Arctic is anticyclonic or cyclonic, either a net accumulation or release of freshwater occurs. The sources of freshwater to the Arctic Ocean are well established and include contributions from the North American and Eurasian Rivers, the Bering Strait Pacific water inflow, sea ice meltwater, and precipitation, but their contribution to the Beaufort Gyre freshwater accumulation varies with changes in the atmospheric circulation. Here we use a Lagrangian backward tracking technique in conjunction with the 1/12‐degree resolution Nucleus for European Modelling of the Ocean model to investigate how sources of freshwater to the Beaufort Gyre have changed in recent decades, focusing on increase in the Pacific water content in the gyre between the late 1980s and early 2000s. Using empirical orthogonal functions we analyze the change in the Arctic oceanic circulation that occurred between the 1980s and 2000s. We highlight a “waiting room” advective pathway that was present in the 1980s and provide evidence that this pathway was caused by a shift in the center of Ekman transport convergence in the Arctic. We discuss the role of these changes as a contributing factor to changes in the stratification, and hence potentially the biology, of the Beaufort Gyre region.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1029/2019JC015022
ISSN:	2169-9275
Date made live:	21 Aug 2019 12:24 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/524826

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1029/2019JC015022

ISSN:

2169-9275

Date made live:

21 Aug 2019 12:24 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/524826