The dynamics of ocean heat transport variability

By S. Jayne, Jochem Marotzke. 2001

214 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/26b6c06d79ab8d2409d5a8926290449322db9862

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Citations in the corpus

Atmospheric bridge, oceanic tunnel, and global climatic teleconnections (2007, background): “…and above the thermocline, the wind-induced Ekman transport, at very short timescales of weekly to monthly, is returned as a compensating barotropic flow from the surface to the bottom ocean and contributes to a strong seasonal variability of the oceanic heat transport [Jayne and Marotzke, 2001].”
Continuous, Array-Based Estimates of Atlantic Ocean Heat Transport at 26.5°N (2011, methodology): “…these results is that much of the seasonal variation of the MHT at 26.58N is due to variations in the geostrophic circulation; that is, it is not dominated simply by Ekman heat transport variability as has frequently been implied by modeling studies (Böning et al. 2001; Jayne and Marotzke 2001).”
The Oceanic Eddy Heat Transport (2002, background): “Figure 4 shows the zonal basin integrals of the eddy heat transport for the 4 components of the overturning decomposition in Lee and Marotzke (1998) and Hall and Bryden (1982) (see also Jayne and Marotzke 2001).”
Simulated variability of the Atlantic meridional overturning circulation (2004, background): “It is clear from the complexity and the still incomplete theoretical understanding of the system (e.g. Jayne and Marotzke 2001; Johnson and Marshall 2002), that in-depth studies involving theoretical and observational analysis, together with (simplified and complex) model studies, are required to…”
Eddy-Induced Heat Transport in the Subtropical North Pacific from Argo, TMI, and Altimetry Measurements (2005, background): “A rich literature now exists that addresses the north–south ocean heat transport and comprehensive recent reviews can be found in Trenberth and Caron (2001), Bryden and Imawaki (2001), Jayne and Marotzke (2001), and Talley (2003).”
Eddy‐induced meridional heat transport in the ocean (2008, background): “It has been perceived that globally eddies play only a minor role in the time-dependent heat transport, but in a number of locations they contribute to the time-mean heat transport [Jayne and Marotzke, 2001, 2002] (hereinafter referred to as JM2001 and JM2002).”
Causes of Interannual–Decadal Variability in the Meridional Overturning Circulation of the Midlatitude North Atlantic Ocean (2008, background): “…wave propagation, that is, especially in the (intra-) seasonal range, was first noted by Bryan (1982), followed up by Böning and Herrmann (1994) and Jayne and Marotzke (2001): its main elements are changes in meridional Ekman transport at the surface, compensated by a weakly depthdependent return…”
Variability of the Meridional Overturning in the North Atlantic from the 50 years GECCO State Estimation (2006, background): “On monthly to interannual time scale, the local Ekman transport caused by zonal wind stress is the most prominent mechanism which is also described by Jayne and Marotzke (2001) and Böning and Herrmann (1994) to be the most important process responsible for the seasonal vari- ability.”
Large-Scale Ocean Heat and Freshwater Transports during the World Ocean Circulation Experiment (2003, background): “Correlated temporal variations in the temperature field (rectification) are not directly taken into account, and numerical simulations suggest this effect is small (Jayne and Marotzke 2001).”
The Annual Cycle of the Energy Budget. Part I: Global Mean and Land–Ocean Exchanges (2008, background): “In the ocean, FS in the tropics is balanced principally by the transport of ocean energy (mainly heat) (FO) and its divergence ( · FO), while in midlatitudes it is largely balanced locally by changes in ocean heat storage OE / t (Jayne and Marotzke 2001; Trenberth et al. 2001).”
Volume, heat, and freshwater transports of the global ocean circulation 1993-2000, estimated from a general circulation model constrained by World Ocean Circulation Experiment (WOCE) data (2003, background): “Further subdecomposition is possible [e.g., Jayne and Marotzke, 2001] and these decompositions are not unique.”
Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “Atlantic OHT variability is closely related to AMOC variability in the tropics/ subtropics [Jayne and Marotzke, 2001; Wunsch and Heimbach, 2006], while in the subpolar gyre OHT variations do not follow AMOC variations closely, as gyre circulation variations and temperature anomalies advected by the…”