Littérature scientifique sur le sujet « Ocean interior »
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Articles de revues sur le sujet "Ocean interior"
Rigby, Frances E., et Nikku Madhusudhan. « On the ocean conditions of Hycean worlds ». Monthly Notices of the Royal Astronomical Society 529, no 1 (27 février 2024) : 409–24. http://dx.doi.org/10.1093/mnras/stae413.
Texte intégralDeVries, Tim, et François Primeau. « Dynamically and Observationally Constrained Estimates of Water-Mass Distributions and Ages in the Global Ocean ». Journal of Physical Oceanography 41, no 12 (1 décembre 2011) : 2381–401. http://dx.doi.org/10.1175/jpo-d-10-05011.1.
Texte intégralBiersteker, John B., Benjamin P. Weiss, Corey J. Cochrane, Camilla D. K. Harris, Xianzhe Jia, Krishan K. Khurana, Jiang Liu, Neil Murphy et Carol A. Raymond. « Revealing the Interior Structure of Icy Moons with a Bayesian Approach to Magnetic Induction Measurements ». Planetary Science Journal 4, no 4 (1 avril 2023) : 62. http://dx.doi.org/10.3847/psj/acc331.
Texte intégralDong, Shenfu, Silvia Garzoli et Molly Baringer. « The Role of Interocean Exchanges on Decadal Variations of the Meridional Heat Transport in the South Atlantic ». Journal of Physical Oceanography 41, no 8 (1 août 2011) : 1498–511. http://dx.doi.org/10.1175/2011jpo4549.1.
Texte intégralSiegelman, Lia. « Energetic Submesoscale Dynamics in the Ocean Interior ». Journal of Physical Oceanography 50, no 3 (mars 2020) : 727–49. http://dx.doi.org/10.1175/jpo-d-19-0253.1.
Texte intégralYang, Xiaoting, et Eli Tziperman. « The Vertical Middepth Ocean Density Profile : An Interplay between Southern Ocean Dynamics and Interior Vertical Diffusivity ». Journal of Physical Oceanography 52, no 10 (octobre 2022) : 2479–92. http://dx.doi.org/10.1175/jpo-d-21-0188.1.
Texte intégralBower, Dan J., Kaustubh Hakim, Paolo A. Sossi et Patrick Sanan. « Retention of Water in Terrestrial Magma Oceans and Carbon-rich Early Atmospheres ». Planetary Science Journal 3, no 4 (1 avril 2022) : 93. http://dx.doi.org/10.3847/psj/ac5fb1.
Texte intégralBower, Dan J., Kaustubh Hakim, Paolo A. Sossi et Patrick Sanan. « Retention of Water in Terrestrial Magma Oceans and Carbon-rich Early Atmospheres ». Planetary Science Journal 3, no 4 (1 avril 2022) : 93. http://dx.doi.org/10.3847/psj/ac5fb1.
Texte intégralBlanke, Bruno, Sabrina Speich, Gurvan Madec et Rudy Maugé. « A global diagnostic of interior ocean ventilation ». Geophysical Research Letters 29, no 8 (avril 2002) : 108–1. http://dx.doi.org/10.1029/2001gl013727.
Texte intégralRutberg, Randye L., et Synte L. Peacock. « High-latitude forcing of interior ocean δ13C ». Paleoceanography 21, no 2 (17 mai 2006) : n/a. http://dx.doi.org/10.1029/2005pa001226.
Texte intégralThèses sur le sujet "Ocean interior"
Wilson, Jamie. « Constraining marine carbon fluxes in the ocean interior ». Thesis, Cardiff University, 2015. http://orca.cf.ac.uk/74714/.
Texte intégralCavan, Emma. « Sink or swim : the fate of particulate organic carbon in the interior ocean ». Thesis, University of Southampton, 2016. https://eprints.soton.ac.uk/401166/.
Texte intégralSiegelman, Lia. « Ageostrophic dynamics in the ocean interior A correction for the thermal mass–induced errors of CTD tags mounted on marine mammals, in the Journal of Atmospheric and Oceanic Technology 35 (6), June 2018 Submesoscale ocean fronts act as biological hotspot for southern elephant seal, in Scientific Reports 9, 2019 Ocean‐scale interactions from space, in Earth and Space Science 6(5), May 2019 Correction and accuracy of high- and low-resolution CTD data from animal-borne instruments, in the Journal of Atmospheric and Oceanic Technology 36 (5), May 2019 Diagnosing ocean‐wave‐turbulence interactions from space, in Geophysical Research Letters 46(15), August 2019 Sub‐mesoscale fronts modify elephant seals foraging behavior, in Limnology and Oceanography Letters, 4(6), December 2019 ». Thesis, Brest, 2019. http://www.theses.fr/2019BRES0094.
Texte intégralThe ocean is the largest solar energy collector on Earth. The amount of heat it can store is modulated by its complex circulation, which spans a broad range of spatial scales, from centimeters to thousands of kilometers. This dissertation investigates two types of physical processes: mesoscale eddies (100-300 km size) and submesoscale fronts (£ 50 km size). To date, ageostrophic submesoscale motions are thought to be mainly trapped within the ocean surface mixed layer, and to be weak in the ocean interior. This is because, in the classical paradigm, motions below the mixed layer are broadly assumed to be in quasigeostrophic balance, preventing the formation of strong buoyancy gradients at depth. This dissertation introduces a paradigm shift; based on a combination of high-resolution in situ CTD data collected by instrumented elephant seals, satellite observations of sea surface height, and high-resolution model outputs in the Antarctic Circumpolar Current, we show that ageostrophic motions (i) are generated by the backgound mesoscale eddy field via frontogenesis processes, and (ii) are not solely confined to the ocean surface mixed layer but, rather, can extend in the ocean interior down to depths of 1 000 m. Deepreaching ageostrophic fronts are shown to drive an anomalous upward heat transport from the ocean interior back to the surface that is larger than other contributions to vertical heat transport and of comparable magnitude to air-sea fluxes. This effect can potentially alter oceanic heat uptake and will be strongest in eddy-rich regions such as the Antarctic Circumpolar Current, the Kuroshio Extension, and the Gulf Stream, all of which are key players in the climate system. As such, ageostrophic fronts at submesoscale provide an important, yet unexplored, pathway for the transport of heat, chemical and biological tracers, between the ocean interior and the surface, with potential major implications for the biogeochemical and climate systems
Freund, Madeleine [Verfasser], Martin [Akademischer Betreuer] Visbeck et Andreas [Gutachter] Oschlies. « Dispersion of a Tracer in the Eastern Tropical South Pacific - an Investigation of Interactions from the Benthic Boundary Layer to the Ocean Interior - / Madeleine Freund ; Gutachter : Andreas Oschlies ; Betreuer : Martin Visbeck ». Kiel : Universitätsbibliothek Kiel, 2020. http://d-nb.info/1210052229/34.
Texte intégralSilvy, Yona. « Emergence des changements de température et de salinité dans l’océan intérieur en réponse au changement climatique : échelles de temps et mécanismes ». Electronic Thesis or Diss., Sorbonne université, 2022. http://www.theses.fr/2022SORUS124.
Texte intégralHuman-induced climate change is already affecting every inhabited region of the planet. Yet, over 90% of the excess heat associated with human activities has been absorbed by the ocean since the 1970s, which acts to largely damp atmospheric warming, but has large impacts on human societies and marine life. In this thesis, I explore when and where thermohaline changes in the ocean interior become large enough to be unambiguously set apart from internal variability and investigate their associated physical drivers, using ensembles of climate models and dedicated numerical experiments. We find that the climate signal in the upper ocean water-masses emerges between the late 20th century and the first decades of the 21st. The Southern Hemisphere mid-latitude Mode Waters emerge before their Northern Hemisphere counterparts. The associated warming at these timescales is mostly caused by the uptake of heat from the atmosphere, passively transported into the ocean interior. In the deeper parts of the ocean, circulation changes play a more important role in the emergence timescales of the climate signals. Increased buoyancy gain at the surface in the subpolar areas cause a slowdown in the meridional overturning circulation. This warms the subsurface and abyssal waters in the Southern Ocean as soon as the mid-20th century, adding up to the weaker passive uptake of heat, but counteracts it in the deep North Atlantic over the 21st, delaying the emergence. Although climate models miss some important aspects of the ocean response to climate change, they allow to shed light on the balance of processes at play, and suggest anthropogenic influence has already spread to large parts of the ocean
Rossi, Tristan. « Contribution à l'étude géologique de la frontière Sud-Est de la plaque Caraïbes : La Serrania Del Interior Oriental (Venezuela) sur le transect Cariaco-Maturin : Synthèses paléogéographique et géodynamique ». Brest, 1985. http://www.theses.fr/1985BRES0001.
Texte intégralKomacek, Thaddeus D., et Dorian S. Abbot. « EFFECT OF SURFACE-MANTLE WATER EXCHANGE PARAMETERIZATIONS ON EXOPLANET OCEAN DEPTHS ». IOP PUBLISHING LTD, 2016. http://hdl.handle.net/10150/622455.
Texte intégralPotie, Gilbert. « Contribution à l'étude géologique de la frontière SE de la plaque caraibe : la serrania del interior oriental sur le transect Cumana-Urica et le bassin de Maturin (Vénézuela) : application de données géophysiques et géologiques à une interpretation structurale ». Brest, 1989. http://www.theses.fr/1989BRES2005.
Texte intégralKrawczynski, Michael James. « Experimental studies of melting and crystallization processes in planetary interiors ». Thesis, Massachusetts Institute of Technology, 2011. http://hdl.handle.net/1721.1/69467.
Texte intégralCataloged from PDF version of thesis.
Includes bibliographical references (p. 191-202).
Melting and crystallization processes on the Earth and Moon are explored in this thesis, and the topics of melt generation, transport, and crystallization are discussed in three distinct geologic environments: the Moon's mantle, the Greenland ice sheet, and the Earth's crust. Experiments have been conducted to determine the conditions of origin for two high-titanium magmas from the Moon. The lunar experiments (Chapter 2) were designed to explore the effects of variable oxygen fugacity (fo₂) on the high pressure and high temperature crystallization of olivine and orthopyroxene in high-Ti magmas. The results of these experiments showed that the source regions for the high-Ti lunar magmas are distributed both laterally and vertically within the lunar mantle, and that it is critical to estimate the pre-eruptive oxygen fugacity in order to determine true depth of origin for these magmas within the lunar mantle. Chapter 3 models the behavior of water flow through the Greenland ice sheet driven by hydrofracture of water through ice. The results show that melt water in the ablation zone of Greenland has almost immediate access to the base of the ice sheet in areas with up two kilometers of ice. Chapter 4 is an experimental study of two hydrous high-silica mantle melts from the Mt. Shasta, CA region. Crystallization is simulated at H₂O saturated conditions at all crustal depths, and a new geobarometer-hygrometer based on amphibole magnesium number is calibrated. In Chapter 5 I use the new barometer to study a suite of mafic enclaves from the Mt. Shasta region, and apply it to amphiboles in these enclaves. Evidence for pre-eruptive H₂O contents of up to 14 wt% is presented, and bulk chemical analyses of the inclusions are used to show that extensive magma mixing has occurred at all crustal depths up to 35 km beneath Mt. Shasta.
by Michael James Krawczynski.
Ph.D.
Allain, Stéphanie. « L'évolution du moment cinétique des étoiles pré-séquence principale de faible masse ». Grenoble 1, 1997. http://www.theses.fr/1997GRE10167.
Texte intégralLivres sur le sujet "Ocean interior"
Jake, Townsend, dir. Coastal modern : Sophisticated homes inspired by the ocean. New York : Clarkson Potter, 2012.
Trouver le texte intégralMuseum of the City of New York., dir. The fabulous interiors of the great ocean liners in historic photographs. New York : Dover Publications, 1985.
Trouver le texte intégralGio Ponti : Le navi : il progetto degli interni navali, 1948-1953. Viareggio (Lucca) : Idea books, 2007.
Trouver le texte intégralDanish design at sea : Ship interior architecture and furnishing. Copenhagen : Polyteknisk Forlag, 2021.
Trouver le texte intégralLe paquebot France. Paris : Norma, 2006.
Trouver le texte intégralVian, Louis-René. Arts décoratifs à bord des paquebots français, 1880-1960. Paris : Editions Fonmare, 1992.
Trouver le texte intégralUnited States. Minerals Management Service. MMS : Securing ocean energy and economic value for America : U.S. Department of the Interior, Minerals Management Service, 2003-2004. Washington, D.C : MMS, 2004.
Trouver le texte intégralRiccesi, Donato. Gustavo Pulitzer Finali : Il disegno della nave : allestimenti interni 1925-1967. Venezia : Marsilio, 1985.
Trouver le texte intégralTo establish in the Department of the Interior an Under Secretary for Energy, Lands, and Minerals and a Bureau of Ocean Energy, an Ocean Energy Safety Service, and an Office of Natural Resources Revenue, and for other purposes : Report together with dissenting views (to accompany H.R. 3404) (including cost estimate of the Congressional Budget Office). Washington, D.C : U.S. G.P.O., 2012.
Trouver le texte intégralFisheries, United States Congress House Committee on Merchant Marine and. National Seabed Hard Minerals Act of 1988 : Report together with additional views (to accompany H.R. 1260 which ... was referred jointly to the Committee on Interior and Insular Affairs and the Committee on Merchant Marine and Fisheries) (including cost estimate of the Congressional Budget Office). [Washington, D.C. ? : U.S. G.P.O., 1988.
Trouver le texte intégralChapitres de livres sur le sujet "Ocean interior"
McCreary, Julian P., et Satish R. Shetye. « Interior Ocean ». Dans Observations and Dynamics of Circulations in the North Indian Ocean, 313–31. Singapore : Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-5864-9_12.
Texte intégralHowell, Samuel M., et Erin J. Leonard. « Ocean Worlds : Interior Processes and Physical Environments ». Dans Handbook of Space Resources, 873–906. Cham : Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-030-97913-3_26.
Texte intégralHonjo, S. « Ocean Particles and Fluxes of Material to the Interior of the Deep Ocean ; The Azoic Theory 120 Years Later ». Dans Facets of Modern Biogeochemistry, 62–73. Berlin, Heidelberg : Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-73978-1_7.
Texte intégralHe, Jingguang, Qingnan Li et Jinjin Wang. « Cruise color analysis system for interior color scheme under complicated ocean lighting conditions ». Dans Developments in Maritime Technology and Engineering, 383–89. London : CRC Press, 2021. http://dx.doi.org/10.1201/9781003216582-43.
Texte intégralLionello, P., et J. Pedlosky. « On the Effect of a Surface Density Front on the Interior Structure of the Ventilated Ocean Thermocline ». Dans IUTAM Symposium on Advances in Mathematical Modelling of Atmosphere and Ocean Dynamics, 183–89. Dordrecht : Springer Netherlands, 2001. http://dx.doi.org/10.1007/978-94-010-0792-4_23.
Texte intégralMachado, Pedro. « Maritime Passages in the Indian Ocean Slave Trade ». Dans The Palgrave Handbook of Global Slavery throughout History, 359–78. Cham : Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-13260-5_20.
Texte intégral« Mixing in the Stratified Interior ». Dans Ocean Mixing, 283–320. Cambridge University Press, 2021. http://dx.doi.org/10.1017/9781316795439.009.
Texte intégralFox-Kemper, B., R. Lumpkin et F. O. Bryan. « Lateral Transport in the Ocean Interior ». Dans International Geophysics, 185–209. Elsevier, 2013. http://dx.doi.org/10.1016/b978-0-12-391851-2.00008-8.
Texte intégralLasc, Anca I. « Epilogue : The presentness of historicism : the Musée centennal du mobilier et de la décoration and the legacy of proto-interior designers ». Dans Interior decorating in nineteenth-century France, 227–34. Manchester University Press, 2018. http://dx.doi.org/10.7228/manchester/9781526113382.003.0007.
Texte intégralMacKinnon, Jennifer, Lou St Laurent et Alberto C. Naveira Garabato. « Diapycnal Mixing Processes in the Ocean Interior ». Dans International Geophysics, 159–83. Elsevier, 2013. http://dx.doi.org/10.1016/b978-0-12-391851-2.00007-6.
Texte intégralActes de conférences sur le sujet "Ocean interior"
Pinkel, Robert. « HF Doppler Acoustic Imaging of the Ocean Surface and Interior ». Dans HIGH FREQUENCY OCEAN ACOUSTICS : High Frequency Ocean Acoustics Conference. AIP, 2004. http://dx.doi.org/10.1063/1.1843017.
Texte intégralMelwani Daswani, Mohit, et Steven D. Vance. « Evolution of Volatiles from Europa's Interior into its Ocean ». Dans Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1777.
Texte intégralYacobucci, Margaret M. « SPECIES DISTRIBUTION MODELING OF WESTERN INTERIOR AMMONOIDS DURING OCEAN ANOXIC EVENT 2 ». Dans GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355164.
Texte intégralSen, Debabrata, et Jai Ram Saripilli. « Numerical Studies on Slosh-Induced Loads Using Coupled Algorithm for Sloshing and 3D Ship Motions ». Dans ASME 2017 36th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/omae2017-61159.
Texte intégralRobinson, L. J., K. S. George, J. H. Whiteside, S. Gibbs et R. Twitchett. « Biomarker and Isotopic Transect Across the Cretaceous Interior Seaway : Drivers of Ocean Anoxia ». Dans 29th International Meeting on Organic Geochemistry. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902754.
Texte intégralLi, Hui, Baoli Deng, Chunlei Liu, Jian Zou et Huilong Ren. « Prediction of Wave-Induced Motions and Loads of Ships With Forward Speed by Matching Method ». Dans ASME 2020 39th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/omae2020-18614.
Texte intégralSheng, Wanan, Anthony Lewis et Raymond Alcorn. « Numerical Studies of a Floating Cylindrical OWC WEC ». Dans ASME 2012 31st International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/omae2012-83041.
Texte intégralHayes, Joseph, Daniel Kelly, Brian L. Beard, Michael Tappa et Annie Bauer. « RECONSTRUCTING OCEAN CIRCULATION ALONG THE EASTERN MARGIN OF THE WESTERN INTERIOR SEAWAY DURING THE LATE CRETACEOUS COOLDOWN ». Dans Joint 56th Annual North-Central/ 71st Annual Southeastern Section Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022nc-375566.
Texte intégralMondal, Bipul Chandra, et Ashutosh Sutra Dhar. « Corrosion Effects on the Strength of Steel Pipes Using FEA ». Dans ASME 2015 34th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/omae2015-42003.
Texte intégralLi, Hui, Hao Lizhu, Huilong Ren et Xiaobo Chen. « Zero Speed Rankine-Kelvin Hybrid Method With a Cylinder Control Surface ». Dans ASME 2015 34th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/omae2015-41565.
Texte intégralRapports d'organisations sur le sujet "Ocean interior"
Testor, Pierre, Thibaut Wagener, Anthony Bosse, Remy Asselot, Virginie Thierry et Johannes Karstensen. Estimate of magnitude and drivers of regional carbon variability for both regions. EuroSea, 2022. http://dx.doi.org/10.3289/eurosea_d7.3.
Texte intégralAndersen, Gisle, Christine Merk, Marie L. Ljones et Mikael P. Johannessen. Interim report on public perceptions of marine CDR. OceanNets, 2022. http://dx.doi.org/10.3289/oceannets_d3.4.
Texte intégralScanlan, E. J., M. Leybourne, D. Layton-Matthews, A. Voinot et N. van Wagoner. Alkaline magmatism in the Selwyn Basin, Yukon : relationship to SEDEX mineralization. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328994.
Texte intégralJoint Expert Group on Food Contact Materials Interim Position Paper on ocean bound plastic. Food Standards Agency, mars 2022. http://dx.doi.org/10.46756/sci.fsa.kdy447.
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