Ocean dynamics

Results: 1909



#Item
1The ocean as a natural fluid dynamics laboratory  AMOCEW waves and turbulence in the ocean interior

The ocean as a natural fluid dynamics laboratory AMOCEW waves and turbulence in the ocean interior

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Source URL: kai.coas.oregonstate.edu

- Date: 2002-12-03 17:31:40
    22012 Upgrades to the Operational GFDL Hurricane Model Morris A. Bender Geophysical Fluid Dynamics Laboratory, NOAA 3-D Ocean Coupling

    2012 Upgrades to the Operational GFDL Hurricane Model Morris A. Bender Geophysical Fluid Dynamics Laboratory, NOAA 3-D Ocean Coupling

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    Source URL: www.hfip.org

    - Date: 2012-06-14 19:31:17
      3Hydrobiologia:265–280 DOIs10750C RA T E R L A K E , O R E G O N  Seasonal nutrient and plankton dynamics

      Hydrobiologia:265–280 DOIs10750C RA T E R L A K E , O R E G O N Seasonal nutrient and plankton dynamics

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      Source URL: memg.ocean.dal.ca

      - Date: 2006-11-28 21:13:38
        4http://www.earthonlinemedia.com/ebooks/tpe_3e/atmosphere/atmospheric_structure.html  Marshall & Plumb, Atmosphere, Ocean, and Climate Dynamics, 2008 Marshall & Plumb, Atmosphere, Ocean, and Climate Dynamics, 2008

        http://www.earthonlinemedia.com/ebooks/tpe_3e/atmosphere/atmospheric_structure.html Marshall & Plumb, Atmosphere, Ocean, and Climate Dynamics, 2008 Marshall & Plumb, Atmosphere, Ocean, and Climate Dynamics, 2008

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        Source URL: climate-dynamics.org

        - Date: 2015-11-04 07:06:03
          5Homework 5 (due December: Climate and the Global Circulation of the Atmosphere (Problems adapted from Hartmann, chUse the bulk aerodynamic formula to calculate the evaporation rate from the ocean,

          Homework 5 (due December: Climate and the Global Circulation of the Atmosphere (Problems adapted from Hartmann, chUse the bulk aerodynamic formula to calculate the evaporation rate from the ocean,

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          Source URL: climate-dynamics.org

          - Date: 2015-11-17 17:21:10
            6Remote Sensing of the Atmosphere and Ocean (11:670:451/16:712:552) Fall 2012 Class website: Sakai Site and http://marine.rutgers.edu/dmcs/ms552 Dr. Mark Miller, Room 233, ENR,  Dr. John Wilkin,

            Remote Sensing of the Atmosphere and Ocean (11:670:451/16:712:552) Fall 2012 Class website: Sakai Site and http://marine.rutgers.edu/dmcs/ms552 Dr. Mark Miller, Room 233, ENR, Dr. John Wilkin,

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            Source URL: meteorology.rutgers.edu

            Language: English - Date: 2015-08-18 09:57:03
            7Harvesting the Motion of the Ocean AquaEnergy Group Alla Weinstein, AquaEnergy Group

            Harvesting the Motion of the Ocean AquaEnergy Group Alla Weinstein, AquaEnergy Group

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            Source URL: hydropower.inel.gov

            Language: English - Date: 2006-02-14 18:23:58
            8Microsoft Word - CLIOTOP_SP_FINAL_3.doc

            Microsoft Word - CLIOTOP_SP_FINAL_3.doc

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            Source URL: www.imber.info

            Language: English - Date: 2015-07-06 04:46:01
            9Waves Ocean covers most of the earth, and waves roam most of the ocean. Waves also cross puddles and ponds. What makes them move, and what determines their speed? By applying and extending the techniques of approx

            Waves Ocean covers most of the earth, and waves roam most of the ocean. Waves also cross puddles and ponds. What makes them move, and what determines their speed? By applying and extending the techniques of approx

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            Source URL: www.inference.phy.cam.ac.uk

            Language: English - Date: 2006-01-24 08:12:21
            10SEMINAR Multi-Scale Modeling of Dilute Two-Phase Flows with an Application to Turbulent Suspension of Sediment in an Open Channel Flow Professor Zhenhua Huang Department of Ocean and Resources Engineering

            SEMINAR Multi-Scale Modeling of Dilute Two-Phase Flows with an Application to Turbulent Suspension of Sediment in an Open Channel Flow Professor Zhenhua Huang Department of Ocean and Resources Engineering

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            Source URL: www.ore.hawaii.edu

            Language: English - Date: 2015-11-25 18:05:30