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  2. Coastal ocean dynamics applications radar - Wikipedia

    en.wikipedia.org/wiki/Coastal_ocean_dynamics...

    In fact, “waves moving toward the receiver increase the return frequency, while waves moving away decrease the return frequency”. [11] Then a further Doppler shift (Δf ) is observed and, by measuring it, it is possible to determine the radial velocity ν s component of the surface current by using the Doppler formula: Δf = ν s / λ s

  3. Wave radar - Wikipedia

    en.wikipedia.org/wiki/Wave_radar

    A typical case is wave measurements from an offshore platform in deep water, where swift currents could make mooring a wave buoy enormously difficult. Another interesting case is a ship under way, where having instruments in the sea is highly impractical and interference from the ship's hull must be avoided.

  4. Marine radar - Wikipedia

    en.wikipedia.org/wiki/Marine_radar

    Marine radar has performance adjustment controls for brightness and contrast, also manual or automatic adjustment of gain, tuning, sea clutter and rain clutter suppression, and interference reduction. Other common controls consist of range scale, bearing cursor, fix/variable range marker (VRM) or bearing/distance cursor (EBL).

  5. General Bathymetric Chart of the Oceans - Wikipedia

    en.wikipedia.org/wiki/General_Bathymetric_Chart...

    The GEBCO chart series was initiated in 1903 by an international group of geographers and oceanographers, under the leadership of Prince Albert I of Monaco.At that time there was an explosion of interest in the study of the natural world and this group recognized the importance of a set of maps describing the shape of the ocean floor.

  6. Weather buoy - Wikipedia

    en.wikipedia.org/wiki/Weather_buoy

    Weather Buoy / Data Buoy / Oceanographic Buoy operated by the Marine Data Service. The first known proposal for surface weather observations at sea occurred in connection with aviation in August 1927, when Grover Loening stated that "weather stations along the ocean coupled with the development of the seaplane to have an equally long range, would result in regular ocean flights within ten years."

  7. Ocean surface topography - Wikipedia

    en.wikipedia.org/wiki/Ocean_surface_topography

    The sea surface height is then the difference between the satellite's altitude relative to the reference ellipsoid and the altimeter range. The satellite sends microwave pulses to the ocean surface. The travel time of the pulses ascending to the oceans surface and back provides data of the sea surface height.

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    mail.aol.com

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  9. Nautical chart - Wikipedia

    en.wikipedia.org/wiki/Nautical_chart

    A 1976 United States NOAA chart of part of Puerto Rico A nautical chart of the Warnemünde harbor shown on OpenSeaMap. A nautical chart or hydrographic chart is a graphic representation of a sea region or water body and adjacent coasts or banks.