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Relevant bibliographies by topics / OSNAP MOC

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Journal articles

Academic literature on the topic 'OSNAP MOC'

Author: Grafiati

Published: 5 June 2025

Last updated: 1 August 2025

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Journal articles on the topic "OSNAP MOC"

1

Lozier, M. S., F. Li, S. Bacon, et al. "A sea change in our view of overturning in the subpolar North Atlantic." Science 363, no. 6426 (2019): 516–21. http://dx.doi.org/10.1126/science.aau6592.

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To provide an observational basis for the Intergovernmental Panel on Climate Change projections of a slowing Atlantic meridional overturning circulation (MOC) in the 21st century, the Overturning in the Subpolar North Atlantic Program (OSNAP) observing system was launched in the summer of 2014. The first 21-month record reveals a highly variable overturning circulation responsible for the majority of the heat and freshwater transport across the OSNAP line. In a departure from the prevailing view that changes in deep water formation in the Labrador Sea dominate MOC variability, these results su

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2

Tooth, Oliver John, Helen Louise Johnson, Chris Wilson, and Dafydd Gwyn Evans. "Seasonal overturning variability in the eastern North Atlantic subpolar gyre: a Lagrangian perspective." Ocean Science 19, no. 3 (2023): 769–91. http://dx.doi.org/10.5194/os-19-769-2023.

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Abstract. Both observations and ocean reanalyses show a pronounced seasonality in the strength of the Atlantic meridional overturning circulation (MOC) within the eastern North Atlantic subpolar gyre (eSPG). However, attributing this overturning seasonality to seasonal dense water formation remains challenging owing to the wide distribution of recirculation timescales within the Iceland and Irminger basins. Here, we investigate the nature of seasonal overturning variability using Lagrangian water parcel trajectories initialised across the Overturning in the Subpolar North Atlantic Program (OSN

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3

Mackay, Neill, Chris Wilson, N. Penny Holliday, and Jan D. Zika. "The Observation-Based Application of a Regional Thermohaline Inverse Method to Diagnose the Formation and Transformation of Water Masses North of the OSNAP Array from 2013 to 2015." Journal of Physical Oceanography 50, no. 6 (2020): 1533–55. http://dx.doi.org/10.1175/jpo-d-19-0188.1.

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AbstractThe strength of the meridional overturning circulation (MOC) in the North Atlantic is dependent upon the formation of dense waters that occurs at high northern latitudes. Wintertime deep convection in the Labrador and Irminger Seas forms the intermediate water mass known as Labrador Sea Water (LSW). Changes in the rate of formation and subsequent export of LSW are thought to play a role in MOC variability, but formation rates are uncertain and the link between formation and export is complex. We present the first observation-based application of a recently developed regional thermohali

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4

Vendramin, Roberto, Hongchang Fu, Yue Zhao, et al. "Abstract 6737: Pharmacologic modulation of nonsense-mediated decay induces anti-tumor immunogenicity in ex vivo patient tumors." Cancer Research 84, no. 6_Supplement (2024): 6737. http://dx.doi.org/10.1158/1538-7445.am2024-6737.

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Abstract Introduction: Immunogenic neoantigens derived from somatic tumor mutations are essential to initiate and sustain robust anti-tumor immune responses. Frameshift insertion/deletions (fs-indels) are a key source of immunogenic neoantigens. However, fs-indels often result in the introduction of premature termination codons (PTCs), leading to mRNA degradation by the nonsense-mediated mRNA decay (NMD) pathway. In human malignancies, NMD activity is increased in response to the heightened burden of somatic fs-indel mutations and effectively prevents the generation of highly immunogenic tumor

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5

Roussenov, Vassil M., Richard G. Williams, M. Susan Lozier, N. Penny Holliday, and Doug Smith. "Historical reconstruction of subpolar North Atlantic overturning and its relationship to density." JGR-Oceans, May 6, 2022. https://doi.org/10.5281/zenodo.6524716.

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Supporting Data: OSNAP_model.tar.gz, NetCDF format, file information: Annual-mean temperature and salinity data from the Met Office statistical ocean reanalysis used in the model reconstruction: Tp_meto_60-20.nc      Annual mean ocean potential temperature 1960 to 2020 S_meto_60-20.nc        Annual mean ocean salinity 1960 to 2020 Time series of model overturning (MOC) along OSNAP line, OSNAP west and OSNAP east sections: MOC_OSNAP.nc, MOC_West.nc, MOC_East.nc                          &nbsp

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6

Lozier, S., F. Li, S. Bacon, et al. "A sea change in our view of overturning in the subpolar North Atlantic." February 1, 2019. https://doi.org/10.1126/science.aau6592.

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To provide an observational basis for IPCC projections of a slowing Atlantic Meridional Overturning Circulation (MOC) in the 21<sup>st</sup> century, the Overturning in the Subpolar North Atlantic Program (OSNAP) observing system was launched in the summer of 2014. The first 21-month record reveals a highly variable overturning circulation responsible for the majority of the heat and freshwater transport across the OSNAP line. In a departure from the prevailing view that changes in deep water formation in the Labrador Sea dominate MOC variability, these results suggest that the conversion of w

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7

Fu, Yao, M. Susan Lozier, Sudip Majumder, and Tillys Petit. "Water Mass Transformation and Its Relationship With the Overturning Circulation in the Eastern Subpolar North Atlantic." Journal of Geophysical Research: Oceans 129, no. 12 (2024). https://doi.org/10.1029/2024jc021222.

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AbstractA recent study using the first 21 months of the OSNAP time series revealed that the export of dense waters in the eastern subpolar North Atlantic―as part of the Atlantic Meridional Overturning Circulation (MOC)―can be almost wholly attributed to surface‐forced water mass transformation (SFWMT) in the Irminger and Iceland basins, thus suggesting a minor role for other means of transformation, such as diapycnal mixing. To understand whether this result is valid over a period that exceeds the current observational record, we use four different ocean reanalysis products to investigate the

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8

Devana, M., and W. Johns. "Structure and Variability of Iceland Scotland Overflow Water Transport in the Western Iceland Basin." Journal of Geophysical Research: Oceans 129, no. 8 (2024). http://dx.doi.org/10.1029/2023jc020107.

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AbstractThe Iceland Scotland Overflow Water (ISOW) plume supplies approximately a third of the production of North Atlantic Deep Water and is a key component of the meridional overturning circulation (MOC). The Overturning in the Subpolar North Atlantic Program (OSNAP) mooring array in the Iceland Basin has provided high‐resolution observations of ISOW from 2014 to 2020. The ISOW plume forms a deep western boundary current along the eastern flank of Reykjanes Ridge, and its total transport varies by greater than a factor of two on intra‐seasonal timescales. EOF analysis of moored current meter

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9

Tagklis, Filippos, A. Bracco, T. Ito, and R. M. Castelao. "Submesoscale modulation of deep water formation in the Labrador Sea." Scientific Reports 10, no. 1 (2020). http://dx.doi.org/10.1038/s41598-020-74345-w.

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Abstract Submesoscale structures fill the ocean surface, and recent numerical simulations and indirect observations suggest that they may extend to the ocean interior. It remains unclear, however, how far-reaching their impact may be—in both space and time, from weather to climate scales. Here transport pathways and the ultimate fate of the Irminger Current water from the continental slope to Labrador Sea interior are investigated through regional ocean simulations. Submesoscale processes modulate this transport and in turn the stratification of the Labrador Sea interior, by controlling the ch

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