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    Stability of the Thermohaline Circulation to Noisy Surface Buoyancy Forcing for the Present and a Warm Climate in an Ocean General Circulation Model 

    Source: Journal of Physical Oceanography:;1998:;Volume( 028 ):;issue: 005:;page 842
    Author(s): Skagseth, Øystein; Mork, Kjell Arne
    Publisher: American Meteorological Society
    Abstract: The stabilities of two different circulation regimes in the North Atlantic, 1) the present thermohaline circulation and 2) a weaker thermohaline circulation, are compared using the Hamburg Large Scale Geostrophic (LSG) ...
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    Recent Warming and Freshening of the Norwegian Sea Observed by Argo Data 

    Source: Journal of Climate:;2019:;volume 032:;issue 012:;page 3695
    Author(s): Mork, Kjell Arne; Skagseth, Øystein; Søiland, Henrik
    Publisher: American Meteorological Society
    Abstract: AbstractClimate variability in the Norwegian Sea, comprising the Norwegian and Lofoten Basins, was investigated based upon monthly estimates of ocean heat and freshwater contents using data from Argo floats during 2002?18. ...
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    Wind-Driven Atlantic Water Flow as a Direct Mode for Reduced Barents Sea Ice Cover 

    Source: Journal of Climate:;2016:;volume( 030 ):;issue: 002:;page 803
    Author(s): Lien, Vidar S.; Schlichtholz, Pawel; Skagseth, Øystein; Vikebø, Frode B.
    Publisher: American Meteorological Society
    Abstract: ariability in the Barents Sea ice cover on interannual and longer time scales has previously been shown to be governed by oceanic heat transport. Based on analysis of observations and results from an ocean circulation model ...
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    Structure and Forcing of Observed Exchanges across the Greenland–Scotland Ridge 

    Source: Journal of Climate:;2018:;volume 031:;issue 024:;page 9881
    Author(s): Bringedal, Carina; Eldevik, Tor; Skagseth, Øystein; Spall, Michael A.; Østerhus, Svein
    Publisher: American Meteorological Society
    Abstract: AbstractThe 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 ...
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    Analysis of the Arctic System for Freshwater Cycle Intensification: Observations and Expectations 

    Source: Journal of Climate:;2010:;volume( 023 ):;issue: 021:;page 5715
    Author(s): Rawlins, Michael A.; Steele, Michael; Holland, Marika M.; Adam, Jennifer C.; Cherry, Jessica E.; Francis, Jennifer A.; Groisman, Pavel Ya; Hinzman, Larry D.; Huntington, Thomas G.; Kane, Douglas L.; Kimball, John S.; Kwok, Ron; Lammers, Richard B.; Lee, Craig M.; Lettenmaier, Dennis P.; McDonald, Kyle C.; Podest, Erika; Pundsack, Jonathan W.; Rudels, Bert; Serreze, Mark C.; Shiklomanov, Alexander; Skagseth, Øystein; Troy, Tara J.; Vörösmarty, Charles J.; Wensnahan, Mark; Wood, Eric F.; Woodgate, Rebecca; Yang, Daqing; Zhang, Ke; Zhang, Tingjun
    Publisher: American Meteorological Society
    Abstract: Hydrologic cycle intensification is an expected manifestation of a warming climate. Although positive trends in several global average quantities have been reported, no previous studies have documented broad intensification ...
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