File:Ventilation in an idealized high-latitude ocean basin.jpg
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DescriptionVentilation in an idealized high-latitude ocean basin.jpg |
English: Schematic of ventilation in an idealized high-latitude ocean basin. The basin extends from a high-latitude landmass (or, equivalently, the North Pole) to an arbitrary mid-latitude zonal boundary of length L. The basin contains n sloping isopycnal layers of (spatially and temporally variable) thickness h and meridional velocity v that outcrop into the upper-ocean mixed layer (of depth H) within the region. Like the real-world high-latitude oceans, the basin hosts a double-celled overturning circulation, with inflow in intermediate layers and outflow in surface and deep layers. Ventilation is quantified with a surface-sourced tracer C, which crosses the mixed layer base with vertical velocity w and at an integrated rate FC. The tracer has interior sources and sinks SC within the basin, and is exported through the mid-latitude boundary at a rate TC. |
Date | |
Source | [1] |
Author | Alberto C. Naveira Garabato, Graeme A. MacGilchrist, Peter J. Brown, D. Gwyn Evans, Andrew J. S. Meijers and Jan D. Zika |
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current | 00:29, 9 April 2020 | 1,280 × 893 (71 KB) | Epipelagic (talk | contribs) | Uploaded a work by Alberto C. Naveira Garabato, Graeme A. MacGilchrist, Peter J. Brown, D. Gwyn Evans, Andrew J. S. Meijers and Jan D. Zika from [https://royalsocietypublishing.org/doi/full/10.1098/rsta.2016.0324] with UploadWizard |
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