Changeset 7538 for branches/2016/dev_merge_2016
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- 2017-01-10T14:17:18+01:00 (8 years ago)
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- branches/2016/dev_merge_2016/DOC/TexFiles
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branches/2016/dev_merge_2016/DOC/TexFiles/Bibliography/Biblio.bib
r6320 r7538 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}, … … 787 799 volume = {34}, 788 800 pages = {8--13} 801 } 802 803 @article{de_lavergne_JPO2016_mixing, 804 author = {C. de Lavergne and G. Madec and J. Le Sommer and A. J. G. Nurser and A. C. Naveira Garabato }, 805 title = {On Antarctic Bottom Water consumption in the abyssal ocean}, 806 issn = {0022-3670}, 807 url = {http://dx.doi.org/10.1175/JPO-D-14-0201.1}, 808 doi = {10.1175/JPO-D-14-0201.1}, 809 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.}, 810 journal = {Journal of Physical Oceanography}, 811 year = {2016}, 812 volume = {46}, pages = {635-–661} 813 } 814 815 @article{de_lavergne_JPO2016_efficiency, 816 author = {C. de Lavergne and G. Madec and J. Le Sommer and A. J. G. Nurser and A. C. Naveira Garabato }, 817 title = {The impact of a variable mixing efficiency on the abyssal overturning}, 818 issn = {0022-3670}, 819 url = {http://dx.doi.org//10.1175/JPO-D-14-0259.1}, 820 doi = {10.1175/JPO-D-14-0259.1}, 821 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.}, 822 journal = {Journal of Physical Oceanography}, 823 year = {2016}, 824 volume = {46}, pages = {663-–681} 789 825 } 790 826 … … 1160 1196 } 1161 1197 1198 @article{goff_JGR2010, 1199 author = {J. A. Goff}, 1200 title = {Global prediction of abyssal hill root-mean-square heights from small-scale altimetric gravity variability}, 1201 issn = {2156-2202}, 1202 url = {http://dx.doi.org/10.1029/2010JB007867}, 1203 doi = {10.1029/2010JB007867}, 1204 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.}, 1205 volume = {115}, 1206 number = {B12}, 1207 journal = {Journal of Geophysical Research: Solid Earth}, 1208 year = {2010}, 1209 pages = {B12104}, 1210 } 1211 1162 1212 @ARTICLE{Goosse_al_JGR99, 1163 1213 author = {H. Goosse and E. Deleersnijder and T. Fichefet and M. England}, … … 1264 1314 1265 1315 @ARTICLE{Griffies_Hallberg_MWR00, 1266 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},1316 author = {S.M. Griffies and R.W. Hallberg}, 1317 title = {Biharmonic friction with a Smagorinsky-like viscosity for use in large-scale eddy-permitting ocean models}, 1268 1318 journal = MWR, 1269 1319 year = {2000}, … … 1586 1636 volume = {12}, 1587 1637 pages = {381--389} 1638 } 1639 1640 @article{Jackson_Rehmann_JPO2014, 1641 author = {P. R. Jackson and C. R. Rehmann}, 1642 title = {Experiments on differential scalar mixing in turbulence in a sheared, stratified flow}, 1643 journal = JPO, 1644 volume = {44}, 1645 issn = {0022-3670}, 1646 url = {http://dx.doi.org/10.1175/JPO-D-14-0027.1}, 1647 doi = {10.1175/JPO-D-14-0027.1}, 1648 number = {10}, 1649 year = {2014}, 1650 pages = {2661--2680}, 1588 1651 } 1589 1652 … … 2430 2493 } 2431 2494 2495 @ARTICLE{Morel_Berthon_LO89, 2496 author = {A. Morel and J.-F. Berthon}, 2497 title = {Surface pigments, algal biomass profiles, and potential production of the euphotic layer: 2498 Relationships reinvestigated in view of remote-sensing applications}, 2499 journal = {Limnol. Oceanogr.}, 2500 year = {1989}, 2501 volume = {34(8)}, 2502 pages = {1545--1562} 2503 } 2504 2432 2505 @ARTICLE{Morel_Maritorena_JGR01, 2433 2506 author = {A. Morel and S. Maritorena}, … … 2476 2549 @ARTICLE{Osborn_JPO80, 2477 2550 author = {T.R. Osborn}, 2478 title = {Estimates of the local rate of vertical diffusion from dissipation measurements}, 2479 journal = JPO, 2551 title = {Estimates of the local rate of vertical diffusion from dissipation measurements}, 2552 journal = JPO, 2553 year = {1980}, 2480 2554 volume = {10}, 2481 2555 pages = {83--89} … … 2714 2788 } 2715 2789 2790 @ARTICLE{Rousset_GMD2015, 2791 author = {C. Rousset and M. Vancoppenolle and G. Madec and T. Fichefet and S. Flavoni 2792 and A. Barth\'{e}lemy and R. Benshila and J. Chanut and C. L\'{e}vy and S. Masson and F. Vivier }, 2793 title = {The Louvain-La-Neuve sea-ice model LIM3.6: Global and regional capabilities}, 2794 journal= {Geoscientific Model Development}, 2795 year = {2015}, 2796 volume = {8}, pages={2991--3005}, 2797 doi = {10.5194/gmd-8-2991-2015}, 2798 url = {http://dx.doi.org/10.5194/gmd-8-2991-2015} 2799 } 2800 2716 2801 @ARTICLE{Sadourny1975, 2717 2802 author = {R. Sadourny}, … … 2794 2879 year = {2004}, 2795 2880 pages = {245--263}, 2881 } 2882 2883 @INBOOK{Smagorinsky_93, 2884 author = {Smagorinsky, J.}, 2885 chapter = {Some historical remarks on the use of non-linear viscosities}, 2886 title = {Large Eddy Simulation of Complex Engineering and Geophysical Flows}, 2887 pages = {3--36}, 2888 year = {1993}, 2889 publisher = {Cambridge University Press, B. Galperin and S. A. Orszag (eds.)}, 2796 2890 } 2797 2891 -
branches/2016/dev_merge_2016/DOC/TexFiles/Top_Matter.tex
r6998 r7538 17 17 %\date{\today} 18 18 \date{ 19 January 201 6\\20 {\small -- version 3.6 stable--} \\19 January 2017 \\ 20 {\small -- version 4.0 alpha --} \\ 21 21 ~ \\ 22 22 \textit{\small Note du P\^ole de mod\'{e}lisation de l'Institut Pierre-Simon Laplace No 27 }\\
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