An Overlooked Problem in Model Simulations of the Thermohaline Circulation and Heat Transport in the Atlantic Ocean

Many models of the large-scale thermohaline circulation in the ocean exhibit strong zonally integrated upwelling in the midlatitude North Atlantic that significantly decreases the amount of deep water that is carried from the formation regions in the subpolar North Atlantic toward low latitudes and...

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Veröffentlicht in:	Journal of climate 1995-03, Vol.8 (3), p.515-523
Hauptverfasser:	Böning, Claus W., Holland, William R., Bryan, Frank O., Danabasoglu, Gokhan, McWilliams, James C.
Format:	Artikel
Sprache:	eng
Schlagworte:	Atmospheric circulation Climate models Deep water Diffusion coefficient Marine Oceans Parameterization Parametric models Sea transportation Temperate regions Upwelling water
Online-Zugang:	Volltext
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