They Came From the Pacific: How Changing Arctic Currents Could Contribute to an Ecological Regime Shift in the Atlantic Ocean

Abstract The Arctic Ocean is rapidly changing. With warming waters, receding sea ice, and changing circulation patterns, it has been hypothesized that previously closed ecological pathways between the Pacific and Atlantic Oceans will be opened as we move toward a seasonally ice‐free Arctic. The disc...

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Main Authors: S. J. Kelly, E. Popova, Y. Aksenov, R. Marsh, A. Yool
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2020-04-01
Series:Earth's Future
Subjects:
Online Access:https://doi.org/10.1029/2019EF001394
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spelling doaj-1ddb5ce8ddef45f7b456a1bb365bfb5e2020-11-25T02:03:01ZengAmerican Geophysical Union (AGU)Earth's Future2328-42772020-04-0184n/an/a10.1029/2019EF001394They Came From the Pacific: How Changing Arctic Currents Could Contribute to an Ecological Regime Shift in the Atlantic OceanS. J. Kelly0E. Popova1Y. Aksenov2R. Marsh3A. Yool4National Oceanography Centre Southampton UKNational Oceanography Centre Southampton UKNational Oceanography Centre Southampton UKOcean and Earth Science University of Southampton Southampton UKNational Oceanography Centre Southampton UKAbstract The Arctic Ocean is rapidly changing. With warming waters, receding sea ice, and changing circulation patterns, it has been hypothesized that previously closed ecological pathways between the Pacific and Atlantic Oceans will be opened as we move toward a seasonally ice‐free Arctic. The discovery of the Pacific diatom Neodenticula seminae in the Atlantic suggests that a tipping point may have already been reached and this “opening up” of the Arctic could already be underway. Here, we investigate how circulation connectivity between the Pacific and Atlantic Oceans has changed in recent decades, using a state‐of‐the‐art high‐resolution ocean model and a Lagrangian particle‐tracking method. We identify four main trans‐Arctic pathways and a fifth route that is sporadically available with a shorter connectivity timescale. We discuss potential explanations for the existence of this “shortcut” advective pathway, linking it to a shift in atmospheric and oceanic circulation regimes. Advective timescales associated with each route are quantified, and seasonal and interannual trends in the main four pathways are discussed, including an increase in Fram Strait outflow relative to the Canadian Archipelago. In conclusion, we note that while tipping points for ecological connectivity are species dependent, even the most direct routes require multiannual connectivity timescales.https://doi.org/10.1029/2019EF001394Ecological connectivityNEMOLagrangian modelingarctic circulation
collection DOAJ
language English
format Article
sources DOAJ
author S. J. Kelly
E. Popova
Y. Aksenov
R. Marsh
A. Yool
spellingShingle S. J. Kelly
E. Popova
Y. Aksenov
R. Marsh
A. Yool
They Came From the Pacific: How Changing Arctic Currents Could Contribute to an Ecological Regime Shift in the Atlantic Ocean
Earth's Future
Ecological connectivity
NEMO
Lagrangian modeling
arctic circulation
author_facet S. J. Kelly
E. Popova
Y. Aksenov
R. Marsh
A. Yool
author_sort S. J. Kelly
title They Came From the Pacific: How Changing Arctic Currents Could Contribute to an Ecological Regime Shift in the Atlantic Ocean
title_short They Came From the Pacific: How Changing Arctic Currents Could Contribute to an Ecological Regime Shift in the Atlantic Ocean
title_full They Came From the Pacific: How Changing Arctic Currents Could Contribute to an Ecological Regime Shift in the Atlantic Ocean
title_fullStr They Came From the Pacific: How Changing Arctic Currents Could Contribute to an Ecological Regime Shift in the Atlantic Ocean
title_full_unstemmed They Came From the Pacific: How Changing Arctic Currents Could Contribute to an Ecological Regime Shift in the Atlantic Ocean
title_sort they came from the pacific: how changing arctic currents could contribute to an ecological regime shift in the atlantic ocean
publisher American Geophysical Union (AGU)
series Earth's Future
issn 2328-4277
publishDate 2020-04-01
description Abstract The Arctic Ocean is rapidly changing. With warming waters, receding sea ice, and changing circulation patterns, it has been hypothesized that previously closed ecological pathways between the Pacific and Atlantic Oceans will be opened as we move toward a seasonally ice‐free Arctic. The discovery of the Pacific diatom Neodenticula seminae in the Atlantic suggests that a tipping point may have already been reached and this “opening up” of the Arctic could already be underway. Here, we investigate how circulation connectivity between the Pacific and Atlantic Oceans has changed in recent decades, using a state‐of‐the‐art high‐resolution ocean model and a Lagrangian particle‐tracking method. We identify four main trans‐Arctic pathways and a fifth route that is sporadically available with a shorter connectivity timescale. We discuss potential explanations for the existence of this “shortcut” advective pathway, linking it to a shift in atmospheric and oceanic circulation regimes. Advective timescales associated with each route are quantified, and seasonal and interannual trends in the main four pathways are discussed, including an increase in Fram Strait outflow relative to the Canadian Archipelago. In conclusion, we note that while tipping points for ecological connectivity are species dependent, even the most direct routes require multiannual connectivity timescales.
topic Ecological connectivity
NEMO
Lagrangian modeling
arctic circulation
url https://doi.org/10.1029/2019EF001394
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