Relevant bibliographies by topics / Greenland-Scotland Ridge

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters

Academic literature on the topic 'Greenland-Scotland Ridge'

Author: Grafiati
Published: 4 June 2021
Last updated: 12 February 2022

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Journal articles on the topic "Greenland-Scotland Ridge"

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Bringedal, Carina, Tor Eldevik, Øystein Skagseth, Michael A. Spall, and Svein Østerhus. "Structure and Forcing of Observed Exchanges across the Greenland–Scotland Ridge." Journal of Climate 31, no. 24 (2018): 9881–901. http://dx.doi.org/10.1175/jcli-d-17-0889.1.

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The Atlantic meridional overturning circulation and associated poleward heat transport are balanced by northern heat loss to the atmosphere and corresponding water-mass transformation. The circulation of northward-flowing Atlantic Water at the surface and returning overflow water at depth is particularly manifested—and observed—at the Greenland–Scotland Ridge where the water masses are guided through narrow straits. There is, however, a rich variability in the exchange of water masses across the ridge on all time scales. Focusing on seasonal and interannual time scales, and particularly the ga
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Beaird, Nicholas, Ilker Fer, Peter Rhines, and Charles Eriksen. "Dissipation of Turbulent Kinetic Energy Inferred from Seagliders: An Application to the Eastern Nordic Seas Overflows." Journal of Physical Oceanography 42, no. 12 (2012): 2268–82. http://dx.doi.org/10.1175/jpo-d-12-094.1.

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Abstract Turbulent mixing is an important process controlling the descent rate, water mass modification, and volume transport augmentation due to entrainment in the dense overflows across the Greenland–Scotland Ridge. These overflows, along with entrained Atlantic waters, form a major portion of the North Atlantic Deep Water, which pervades the abyssal ocean. Three years of Seaglider observations of the overflows across the eastern Greenland–Scotland Ridge are leveraged to map the distribution of dissipation of turbulent kinetic energy on the Iceland–Faroe Ridge. A method has been applied usin
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Uenzelmann-Neben, Gabriele, and Jens Gruetzner. "Chronology of Greenland Scotland Ridge overflow: What do we really know?" Marine Geology 406 (December 2018): 109–18. http://dx.doi.org/10.1016/j.margeo.2018.09.008.

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Biastoch, Arne, Rolf H. Käse, and Detlef B. Stammer. "The Sensitivity of the Greenland–Scotland Ridge Overflow to Forcing Changes." Journal of Physical Oceanography 33, no. 11 (2003): 2307–19. http://dx.doi.org/10.1175/1520-0485(2003)033<2307:tsotgr>2.0.co;2.

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Olsen, Steffen M., Bogi Hansen, Detlef Quadfasel, and Svein Østerhus. "Observed and modelled stability of overflow across the Greenland–Scotland ridge." Nature 455, no. 7212 (2008): 519–22. http://dx.doi.org/10.1038/nature07302.

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Rheinlænder, Jonathan W., David Ferreira, and Kerim H. Nisancioglu. "Topological Constraints by the Greenland–Scotland Ridge on AMOC and Climate." Journal of Climate 33, no. 13 (2020): 5393–411. http://dx.doi.org/10.1175/jcli-d-19-0726.1.

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AbstractChanges in the geometry of ocean basins have been influential in driving climate change throughout Earth’s history. Here, we focus on the emergence of the Greenland–Scotland Ridge (GSR) and its influence on the ocean state, including large-scale circulation, heat transport, water mass properties, and global climate. Using a coupled atmosphere–ocean–sea ice model, we consider the impact of introducing the GSR in an idealized Earth-like geometry, comprising a narrow Atlantic-like basin and a wide Pacific-like basin. Without the GSR, deep-water formation occurs near the North Pole in the
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7

Olsen, Steffen Malskcer, B. Hansen, D. Quadfasel, and S. Østerhus. "Stability of the overflow across the Greenland-Scotland Ridge since 1948." IOP Conference Series: Earth and Environmental Science 6, no. 3 (2009): 032017. http://dx.doi.org/10.1088/1755-1307/6/3/032017.

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8

Poore, H. R., R. Samworth, N. J. White, S. M. Jones, and I. N. McCave. "Neogene overflow of Northern Component Water at the Greenland-Scotland Ridge." Geochemistry, Geophysics, Geosystems 7, no. 6 (2006): n/a. http://dx.doi.org/10.1029/2005gc001085.

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9

Jensen, Mari F., Kerim H. Nisancioglu, and Michael A. Spall. "Large Changes in Sea Ice Triggered by Small Changes in Atlantic Water Temperature." Journal of Climate 31, no. 12 (2018): 4847–63. http://dx.doi.org/10.1175/jcli-d-17-0802.1.

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The sensitivity of sea ice to the temperature of inflowing Atlantic water across the Greenland–Scotland Ridge is investigated using an eddy-resolving configuration of the Massachusetts Institute of Technology General Circulation Model with idealized topography. During the last glacial period, when climate on Greenland is known to have been extremely unstable, sea ice is thought to have covered the Nordic seas. The dramatic excursions in climate during this period, seen as large abrupt warming events on Greenland and known as Dansgaard–Oeschger (DO) events, are proposed to have been caused by a
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10

Wright, James D., and Kenneth G. Miller. "Control of North Atlantic Deep Water Circulation by the Greenland-Scotland Ridge." Paleoceanography 11, no. 2 (1996): 157–70. http://dx.doi.org/10.1029/95pa03696.

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Dissertations / Theses on the topic "Greenland-Scotland Ridge"

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More, Colin. "The role of North Atlantic Current water in exchanges across the Greenland-Scotland Ridge from the Nordic Seas." Master's thesis, 2011. http://hdl.handle.net/10048/1681.

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The circulation and gradual transformation in properties of oceanic water masses is a matter of great interest for short-term weather and biological forecasting, as well as long-term climate change. It is usually agreed that the Nordic Seas between Greenland and Norway are key to these transformations since they are an important producer of dense water, a process central to the theory of the global thermohaline circulation. In this study, one component of this deep water is examined – that formed in the Nordic Seas themselves from the inflowing North Atlantic Current. Using Lagrangian particle
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Books on the topic "Greenland-Scotland Ridge"

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Structure and Development of the Greenland-Scotland Ridge: New Methods and Concepts. Springer, 2013.

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Book chapters on the topic "Greenland-Scotland Ridge"

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Jungclaus, Johann H., Andreas Macrander, and Rolf H. Käse. "Modelling the Overflows Across the Greenland–Scotland Ridge." In Arctic–Subarctic Ocean Fluxes. Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-6774-7_23.

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2

Hansen, Bogi, Svein Østerhus, William R. Turrell, et al. "The Inflow of Atlantic Water, Heat, and Salt to the Nordic Seas Across the Greenland–Scotland Ridge." In Arctic–Subarctic Ocean Fluxes. Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-6774-7_2.

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