English

edit

Noun

edit

atlantification (uncountable)

  1. Alternative form of Atlantification
    • 2003, Paul F. Wassmann, Eduard Bauerfeind, Martin Fortier, Mitsuo Fukuchi, Barry T. Hargrave, Brad Moran, Thomas T. Noji, Eva-Maria Nöthig, Kalle Olli, Rolf Peinert, Hiroshi Sasaki, Vladimir P. Shevchenko, “Particulate Organic Carbon Flux to the Arctic Ocean Sea Floor”, in Rüdiger Stein, Robie W. Macdonald, editors, The Organic Carbon Cycle in the Arctic Ocean: Present and Past, →ISBN, page 135:
      Global warming results in an “atlantification” of large regions of the contemporary MIZ band in the Atlantic sector of the Arctic and probably in increased export of ArW, fresh-water, ice and ice-bound detritus through the Fram Strait. In the Barents Sea, the term atlantification implies that the current MIZ will move northwards and that stratification will decrease strongly in the MIZ region.
    • 2017 April, Igor V. Polyakov, Andrey V. Pnyushkov, Matthew B. Alkire, Igor M. Ashik, Till M. Baumann, Eddy C. Carmack, Ilona Goszczko, John Guthrie, Vladimir V. Ivanov, Torsten Kanzow, Richard Krishfield, Ronald Kwok, Arild Sundfjord, James Morison, Robert Rember, Alexander Yulin, “Greater role for Atlantic inflows on sea-ice loss in the Eurasian Basin of the Arctic Ocean”, in Science, volume 356, number 6335, page 285:
      This encroaching “atlantification” of the Eurasian Basin represents an essential step toward a new Arctic climate state, with a substantially greater role for Atlantic inflows.
    • 2019 May 16, Atle Staalesen, “With radical Arctic change comes spawning cod in new northern waters”, in The Independent Barents Observer:
      We see a similar atlantification of the sea to the north and east of Svalbard; less sea ice in the Arctic Ocean leads to less melt-water and thus the warm Atlantic water remains atop the water column for most of the year, staying entirely on the surface.of the sea to the north and east of Svalbard; less sea ice in the Arctic Ocean leads to less melt-water and thus the warm Atlantic water remains atop the water column for most of the year, staying entirely on the surface.