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Mid to late-Holocene sea-surface temperature variability off north-eastern Newfoundland and its linkage to the North Atlantic Oscillation

Bibliographic Data

ID12265145
AuthorsLisa Orme (0000-0003-0210-9264, National University of Ireland, Maynooth, corresponding author), Arto Miettinen (0000-0003-4537-2556, Norwegian Polar Institute, Fram Centre, Tromsø, Norway), Marit-Solveig Seidenkrantz (0000-0002-1973-5969, Palaeoceanography and Paleoclimate Group, Arctic Research Centre, and iClimate, Department of Geoscience, Aarhus University, Aarhus, Denmark), Kirsi Tuominen (University of Helsinki), Christof Pearce (0000-0002-4866-3204, Palaeoceanography and Paleoclimate Group, Arctic Research Centre, and iClimate, Department of Geoscience, Aarhus University, Aarhus, Denmark), Dmitry Divine (0000-0003-0548-6698, Norwegian Polar Institute), Dmitry V Divine (Norwegian Polar Institute, Fram Centre, Tromsø, Norway), Mimmi Oksman (0000-0002-8386-516X, Geological Survey of Denmark and Greenland, Copenhagen, Denmark), Antoon Kuijpers (0000-0002-3733-5440, Geological Survey of Denmark and Greenland, Copenhagen, Denmark)
Year2020
Volume31
Issue1
Pages3-15
Publication date2020-10-04
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683620961488
OpenAlexW3092090437
LanguageEN
Citations received3
References cited98

In recent decades the surface water temperature and salinity in the Labrador Sea have been influenced by atmospheric circulation patterns, such as the North Atlantic Oscillation (NAO), as well as a trend to increasingly warm atmospheric temperatures in recent years. These changes are concerning, given the important role that temperature and salinity have on deep convection in the Labrador Sea. Yet, due to the shortness of available records, the long-term patterns of climate variability in the region are not clear. Here, a diatom-based reconstruction of summer sea-surface temperature (SST) developed from Trinity Bay, Newfoundland, provides insight into variations of SST since 7.2 cal ka BP in the southwestern Labrador Sea. The results show that the Holocene Thermal Maximum (HTM) lasted until c. 5.2 cal ka BP, which was followed by a gradual cooling trend overprinted by centennial temperature fluctuations of 1–2°C. Long-term cooling was likely the result of declining Northern Hemisphere orbital summer insolation, potentially amplified by long-term changes in surface and bottom water salinity, which led to a gradual reduction in the stratification of the water column. Centennial fluctuations in temperature vary in-phase with reconstructed variations in the NAO, supporting a consistent relationship between atmospheric circulation and SST over centennial-millennial timescales. Other factors influencing the SST variability may have been solar forcing during the mid-Holocene and variations in the strength of the subpolar gyre during the late-Holocene. The most prolonged cool period at 5.2–4.1 cal ka BP coincides with sharply reduced salinity in the Labrador Sea and a weakening of deep ventilation in the northeast Atlantic, highlighting a period with altered ocean surface conditions and circulation across the northern North Atlantic

Atlantic multidecadal oscillation · Atmospheric Circulation · Bay · Climatology · Holocene · North Atlantic oscillation · Northern Hemisphere · Ocean gyre · Sea surface temperature · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Oceanographic and Atmospheric Processes · Geology · Oceanography

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Unique citing works3
Citations per year0,6
Citation span2021 - 2025 (5)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 3

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