The Oceanic Eddy Heat Transport
By S. Jayne, Jochem Marotzke. 2002
264 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/2ea673727c5f8b94f62942a57f8a26a658f07d00
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Citations in the corpus
- Continuous, Array-Based Estimates of Atlantic Ocean Heat Transport at 26.5°N (2011, background): “Jayne and Marotzke (2002) found that the eddy heat flux due to temporal correlation of y9 and u9 anomalies is nearly zero at 268N, which is located between a region of positive values to the north (up to ;0.1 PW at 408N) and negative values to the south (20.2 PW at 158N).”
- The Role of Mesoscale Eddies in the Rectification of the Southern Ocean Response to Climate Change (2010, background): “(Jayne and Marotzke 2002), poleward eddy heat fluxes in the Southern Ocean are believed to be the strongest.”
- Eddy-Induced Heat Transport in the Subtropical North Pacific from Argo, TMI, and Altimetry Measurements (2005, result): “Using a high-resolution ocean general circulation model (OGCM), Jayne and Marotzke (2002) estimated recently the eddy heat transport directly from the model output and compared it with the estimate by Stammer (1998).”
- Southern Ocean eddy phenomenology (2015, background): “Qualitatively, the variation of the eddy heat transport with latitude due to stirring matches rather well estimates based on model simulations [Jayne and Marotzke, 2002; Volkov et al., 2008; Griffies et al., 2015], in contrast to the eddy heat transport based on the trapping effect as estimated by…”
- 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).”
- Global Patterns of Mesoscale Eddy Properties and Diffusivities (2014, background): “The issue is not simply of theoretical interest; the meridional ocean eddy heat transport is quite significant at low latitudes (Jayne and Marotzke 2002).”