Global contributions of mesoscale dynamics to meridional heat transport
نویسندگان
چکیده
Abstract. Mesoscale ocean processes are prevalent in many parts of the global oceans and may contribute substantially to meridional movement heat. Yet earlier surveys temperature fluxes heat transport (HT) have not formally distinguished between mesoscale large-scale contributions, or they defined eddy contributions based on temporal rather than spatial characteristics. This work uses filtering methods separate (gyre planetary wave) from (eddy, recirculation, tropical instability HT. Overall, flux (MTF) produces a net poleward HT at midlatitudes equatorward tropics, thereby resulting divergence subtropics. In addition MTF generated by propagating eddies waves, is also produced stationary recirculations near energetic western boundary currents, where difference current its recirculation MTF. The contribution yields different results temporally “eddy” HT, with latter including gyre wave motions low latitudes. most interannual decadal variability Southern Ocean, Indo-Pacific, North Atlantic. Surface kinetic energy (EKE) good proxy for regions highest time-mean EKE, though it does explain much modest EKE. approach quantifying can be used improve parameterizations effects coarse-resolution models assess regional impacts tracer fluxes.
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ژورنال
عنوان ژورنال: Ocean Science
سال: 2021
ISSN: ['1812-0784', '1812-0792']
DOI: https://doi.org/10.5194/os-17-1031-2021