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a b Encoding: UTF8 471 471 pages = {81--101} 472 472 } 473 473 474 @article{bouffard_Boegman_DAO2013, 475 author = {D. Bouffard and L. Boegman}, 476 title = {A diapycnal diffusivity model for stratified environmental flows}, 477 volume = {61-62}, 478 issn = {03770265}, 479 url = {http://dx.doi.org/10.1016/j.dynatmoce.2013.02.002}, 480 doi = {10.1016/j.dynatmoce.2013.02.002}, 481 journal = DAO, 482 year = {2013}, 483 pages = {14--34}, 484 } 485 474 486 @ARTICLE{Bougeault1989, 475 487 author = {P. Bougeault and P. Lacarrere}, 476 488 title = {Parameterization of Orography-Induced Turbulence in a Mesobeta--Scale … … note = {MERSEA-WP09-MERCA-TASK-9.1.1} 788 800 pages = {8--13} 789 801 } 790 802 803 @article{de_lavergne_JPO2016_efficiency, 804 title = {The impact of a variable mixing efficiency on the abyssal overturning}, 805 issn = {0022-3670}, 806 url = {http://dx.doi.org//10.1175/JPO-D-14-0259.1}, 807 doi = {10.1175/JPO-D-14-0259.1}, 808 abstract = {In studies of ocean mixing, it is generally assumed that small-scale turbulent overturns lose 15-20 \% of their energy in eroding the background stratification. Accumulating evidence that this energy fraction, or mixing efficiency Rf, significantly varies depending on flow properties challenges this assumption, however. Here, we examine the implications of a varying mixing efficiency for ocean energetics and deep water mass transformation. Combining current parameterizations of internal wave-driven mixing with a recent model expressing Rf as a function of a turbulence intensity parameter Reb = εν/νN2, we show that accounting for reduced mixing efficiencies in regions of weak stratification or energetic turbulence (high Reb) strongly limits the ability of breaking internal waves to supply oceanic potential energy and drive abyssal upwelling. Moving from a fixed Rf = 1/6 to a variable efficiency Rf(Reb) causes Antarctic Bottom Water upwelling induced by locally-dissipating internal tides and lee waves to fall from 9 to 4 Sv, and the corresponding potential energy source to plunge from 97 to 44 GW. When adding the contribution of remotely-dissipating internal tides under idealized distributions of energy dissipation, the total rate of Antarctic Bottom Water upwelling is reduced by about a factor of 2, reaching 5-15 Sv compared to 10-33 Sv for a fixed efficiency. Our results suggest that distributed mixing, overflow-related boundary processes and geothermal heating are more effective in consuming abyssal waters than topographically-enhanced mixing by breaking internal waves. Our calculations also point to the importance of accurately constraining Rf(Reb) and including the effect in ocean models.}, 809 journal = {Journal of Physical Oceanography}, 810 author = {C. de Lavergne and G. Madec and J. Le Sommer and A. J. G. Nurser and A. C. Naveira Garabato }, 811 year = {2016}, 812 volume = {46}, pages = {663-–681} 813 } 814 791 815 @ARTICLE{Delecluse_Madec_Bk00, 792 816 author = {P. Delecluse and G. Madec}, 793 817 title = {Ocean modelling and the role of the ocean in the climate system}, … … note = {MERSEA-WP09-MERCA-TASK-9.1.1} 1159 1183 author = {A. E. Gill} 1160 1184 } 1161 1185 1186 @article{goff_JGR2010, 1187 author = {J. A. Goff}, 1188 title = {Global prediction of abyssal hill root-mean-square heights from small-scale altimetric gravity variability}, 1189 issn = {2156-2202}, 1190 url = {http://dx.doi.org/10.1029/2010JB007867}, 1191 doi = {10.1029/2010JB007867}, 1192 abstract = {Abyssal hills, which are pervasive landforms on the seafloor of the Earth's oceans, represent a potential tectonic record of the history of mid-ocean ridge spreading. However, the most detailed global maps of the seafloor, derived from the satellite altimetry-based gravity field, cannot be used to deterministically characterize such small-scale ({\textless}10 km) morphology. Nevertheless, the small-scale variability of the gravity field can be related to the statistical properties of abyssal hill morphology using the upward continuation formulation. In this paper, I construct a global prediction of abyssal hill root-mean-square (rms) heights from the small-scale variability of the altimetric gravity field. The abyssal hill-related component of the gravity field is derived by first masking distinct features, such as seamounts, mid-ocean ridges, and continental margins, and then applying a newly designed adaptive directional filter algorithm to remove fracture zone/discontinuity fabric. A noise field is derived empirically by correlating the rms variability of the small-scale gravity field to the altimetric noise field in regions of very low relief, and the noise variance is subtracted from the small-scale gravity variance. Suites of synthetically derived, abyssal hill formed gravity fields are generated as a function of water depth, basement rms heights, and sediment thickness and used to predict abyssal hill seafloor rms heights from corrected small-scale gravity rms height. The resulting global prediction of abyssal hill rms heights is validated qualitatively by comparing against expected variations in abyssal hill morphology and quantitatively by comparing against actual measurements of rms heights. Although there is scatter, the prediction appears unbiased.}, 1193 volume = {115}, 1194 number = {B12}, 1195 journal = {Journal of Geophysical Research: Solid Earth}, 1196 year = {2010}, 1197 pages = {B12104}, 1198 } 1199 1162 1200 @ARTICLE{Goosse_al_JGR99, 1163 1201 author = {H. Goosse and E. Deleersnijder and T. Fichefet and M. England}, 1164 1202 title = {Sensitivity of a global coupled ocean-sea ice model to the parameterization of vertical mixing}, … … note = {MERSEA-WP09-MERCA-TASK-9.1.1} 1264 1302 1265 1303 @ARTICLE{Griffies_Hallberg_MWR00, 1266 1304 author = {S.M. Griffies and R.H. Hallberg}, 1267 title = {Biharmonic friction with a smagorinsky-like viscosity for use in large-scale eddy-permitting ocean models},1305 title = {Biharmonic friction with a Smagorinsky-like viscosity for use in large-scale eddy-permitting ocean models}, 1268 1306 journal = MWR, 1269 1307 year = {2000}, 1270 1308 volume = {128}, … … note = {MERSEA-WP09-MERCA-TASK-9.1.1} 1587 1625 pages = {381--389} 1588 1626 } 1589 1627 1628 @article{Jackson_Rehmann_JPO2014, 1629 author = {P. R. Jackson and C. R. Rehmann}, 1630 title = {Experiments on differential scalar mixing in turbulence in a sheared, stratified flow}, 1631 journal = JPO, 1632 volume = {44}, 1633 issn = {0022-3670}, 1634 url = {http://dx.doi.org/10.1175/JPO-D-14-0027.1}, 1635 doi = {10.1175/JPO-D-14-0027.1}, 1636 number = {10}, 1637 year = {2014}, 1638 pages = {2661--2680}, 1639 } 1640 1590 1641 @ARTICLE{Jayne_St_Laurent_GRL01, 1591 1642 author = {S.R. Jayne and L.C. {St. Laurent}}, 1592 1643 title = {Parameterizing tidal disspiation over rough topography}, … … URL = {http://journals.ametsoc.org/doi/abs/10.1175/2517.1} 2429 2480 pages = {10,749--10,768} 2430 2481 } 2431 2482 2483 2484 @ARTICLE{Morel_Berthon_LO89, 2485 author = {A. Morel and J.-F. Berthon}, 2486 title = {Surface pigments, algal biomass profiles, and potential production of the euphotic layer: 2487 Relationships reinvestigated in view of remote-sensing applications}, 2488 journal = {Limnol. Oceanogr.}, 2489 year = {1989}, 2490 volume = {34(8)}, 2491 pages = {1545--1562} 2492 } 2493 2432 2494 @ARTICLE{Morel_Maritorena_JGR01, 2433 2495 author = {A. Morel and S. Maritorena}, 2434 2496 title = {Bio-optical properties of oceanic waters: a reappraisal}, … … URL = {http://journals.ametsoc.org/doi/abs/10.1175/2517.1} 2475 2537 2476 2538 @ARTICLE{Osborn_JPO80, 2477 2539 author = {T.R. Osborn}, 2478 title = {Estimates of the local rate of vertical di ffusion from dissipation measurements},2540 title = {Estimates of the local rate of vertical diffusion from dissipation measurements}, 2479 2541 journal = JPO, 2542 year = {1980}, 2480 2543 volume = {10}, 2481 2544 pages = {83--89} 2482 2545 }