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  • 1. Browny, Nicola Jane
    et al.
    Nilsson, Johan
    Pemberton, Per
    SMHI, Forskningsavdelningen, Oceanografi.
    Arctic Ocean Freshwater Dynamics: Transient Response to Increasing River Runoff and Precipitation2019Ingår i: Journal of Geophysical Research - Oceans, ISSN 2169-9275, E-ISSN 2169-9291, Vol. 124, nr 7, s. 5205-5219Artikel i tidskrift (Refereegranskat)
  • 2. Fransner, Filippa
    et al.
    Gustafsson, Erik
    Tedesco, Letizia
    Vichi, Marcello
    Hordoir, Robinson
    SMHI, Forskningsavdelningen, Oceanografi.
    Roquet, Fabien
    Spilling, Kristian
    Kuznetsov, Ivan
    Eilola, Kari
    SMHI, Forskningsavdelningen, Oceanografi.
    Morth, Carl-Magnus
    Humborg, Christoph
    Nycander, Jonas
    Non-Redfieldian Dynamics Explain Seasonal pCO(2) Drawdown in the Gulf of Bothnia2018Ingår i: Journal of Geophysical Research - Oceans, ISSN 2169-9275, E-ISSN 2169-9291, Vol. 123, nr 1, s. 166-188Artikel i tidskrift (Refereegranskat)
  • 3. Fredriksson, S. T.
    et al.
    Arneborg, Lars
    SMHI, Forskningsavdelningen, Oceanografi.
    Nilsson, H.
    Handler, R. A.
    Surface shear stress dependence of gas transfer velocity parameterizations using DNS2016Ingår i: Journal of Geophysical Research - Oceans, ISSN 2169-9275, E-ISSN 2169-9291, Vol. 121, nr 10, s. 7369-7389Artikel i tidskrift (Refereegranskat)
  • 4. Grist, Jeremy P.
    et al.
    Josey, Simon A.
    New, Adrian L.
    Roberts, Malcolm
    Koenigk, Torben
    SMHI, Forskningsavdelningen, Klimatforskning - Rossby Centre.
    Iovino, Doroteaciro
    Increasing Atlantic Ocean Heat Transport in the Latest Generation Coupled Ocean-Atmosphere Models: The Role of Air-Sea Interaction2018Ingår i: Journal of Geophysical Research - Oceans, ISSN 2169-9275, E-ISSN 2169-9291, Vol. 123, nr 11, s. 8624-8637Artikel i tidskrift (Refereegranskat)
  • 5.
    Hordoir, Robinson
    et al.
    SMHI, Forskningsavdelningen, Oceanografi.
    Axell, Lars
    SMHI, Forskningsavdelningen, Oceanografi.
    Löptien, Ulrike
    SMHI, Forskningsavdelningen, Oceanografi.
    Dietze, Heiner
    Kuznetsov, Ivan
    SMHI, Forskningsavdelningen, Oceanografi.
    Influence of sea level rise on the dynamics of salt inflows in the Baltic Sea2015Ingår i: Journal of Geophysical Research - Oceans, ISSN 2169-9275, E-ISSN 2169-9291, Vol. 120, nr 10, s. 6653-6668Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    The Baltic Sea is a marginal sea, located in a highly industrialized region in Central Northern Europe. Saltwater inflows from the North Sea and associated ventilation of the deep exert crucial control on the entire Baltic Sea ecosystem. This study explores the impact of anticipated sea level changes on the dynamics of those inflows. We use a numerical oceanic general circulation model covering both the Baltic and the North Sea. The model successfully retraces the essential ventilation dynamics throughout the period 1961-2007. A suite of idealized experiments suggests that rising sea level is associated with intensified ventilation as saltwater inflows become stronger, longer, and more frequent. Expressed quantitatively as a salinity increase in the deep central Baltic Sea, we find that a sea level rise of 1 m triggers a saltening of more than 1 PSU. This substantial increase in ventilation is the consequence of the increasing cross section in the Danish Straits amplified by a reduction of vertical mixing.

  • 6. Kniebusch, Madline
    et al.
    Meier, Markus
    SMHI, Forskningsavdelningen, Oceanografi.
    Neumann, Thomas
    Borgel, Florian
    Temperature Variability of the Baltic Sea Since 1850 and Attribution to Atmospheric Forcing Variables2019Ingår i: Journal of Geophysical Research - Oceans, ISSN 2169-9275, E-ISSN 2169-9291, Vol. 124, nr 6, s. 4168-4187Artikel i tidskrift (Refereegranskat)
  • 7. Lambert, Erwin
    et al.
    Nummelin, Aleksi
    Pemberton, Per
    SMHI, Forskningsavdelningen, Oceanografi.
    Ilicak, Mehmet
    Tracing the Imprint of River Runoff Variability on Arctic Water Mass Transformation2019Ingår i: Journal of Geophysical Research - Oceans, ISSN 2169-9275, E-ISSN 2169-9291, Vol. 124, nr 1, s. 302-319Artikel i tidskrift (Refereegranskat)
  • 8.
    Meier, Markus
    et al.
    SMHI, Forskningsavdelningen, Oceanografi.
    Vaeli, Germo
    Naumann, Michael
    Eilola, Kari
    SMHI, Forskningsavdelningen, Oceanografi.
    Frauen, Claudia
    Recently Accelerated Oxygen Consumption Rates Amplify Deoxygenation in the Baltic Sea2018Ingår i: Journal of Geophysical Research - Oceans, ISSN 2169-9275, E-ISSN 2169-9291, Vol. 123, nr 5, s. 3227-3240Artikel i tidskrift (Refereegranskat)
  • 9.
    Pemberton, Per
    et al.
    SMHI, Forskningsavdelningen, Oceanografi.
    Nilsson, J.
    The response of the central Arctic Ocean stratification to freshwater perturbations2016Ingår i: Journal of Geophysical Research - Oceans, ISSN 2169-9275, E-ISSN 2169-9291, Vol. 121, nr 1, s. 792-817Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Using a state-of-the-art coupled ice-ocean-circulation model, we perform a number of sensitivity experiments to examine how the central Arctic Ocean stratification responds to changes in river runoff and precipitation. The simulations yield marked changes in the cold halocline and the Arctic Atlantic layer. Increased precipitation yields a warming of the Atlantic layer, which primarily is an advective signal, propagated through the St. Anna Trough, reflecting air-sea heat flux changes over the Barents Sea. As the freshwater supply is increased, the anticyclonic Beaufort Gyre is weakened and a greater proportion of the Arctic Ocean freshwater is exported via the Fram Strait, with nearly compensating export decreases through the Canadian Arctic Archipelago. The corresponding reorganization of the freshwater pool appears to be controlled by advective processes, rather than by the local changes in the surface freshwater flux. A simple conceptual model of the Arctic Ocean, based on a geostrophically controlled discharge of the low-salinity water, is introduced and compared with the simulations. Key predictions of the conceptual model are that the halocline depth should decrease with increasing freshwater input and that the Arctic Ocean freshwater storage should increase proportionally to the square root of the freshwater input, which are in broad qualitative agreement with the sensitivity experiments. However, the model-simulated rate of increase of the freshwater storage is weaker, indicating that effects related to wind forcing and rerouting of the freshwater-transport pathways play an important role for the dynamics of the Arctic Ocean freshwater storage.

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