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  2. Geostrophic current - Wikipedia

    en.wikipedia.org/wiki/Geostrophic_current

    The structure will eventually dissipate due to friction and mixing of water properties. A geostrophic current is an oceanic current in which the pressure gradient force is balanced by the Coriolis effect. The direction of geostrophic flow is parallel to the isobars, with the high pressure to the right of the flow in the Northern Hemisphere, and ...

  3. Ocean current - Wikipedia

    en.wikipedia.org/wiki/Ocean_current

    An ocean current is a continuous, ... A 1943 map of the world's ocean currents ... Geostrophic current – Oceanic flow in which the pressure gradient force is ...

  4. Pressure gradient - Wikipedia

    en.wikipedia.org/wiki/Pressure_gradient

    The pressure gradient is a dimensional quantity expressed in units of pascals per metre (Pa/m). Mathematically, it is the gradient of pressure as a function of position. The gradient of pressure in hydrostatics is equal to the body force density (generalised Stevin's Law). In petroleum geology and the petrochemical sciences pertaining to oil ...

  5. Cromwell Current - Wikipedia

    en.wikipedia.org/wiki/Cromwell_Current

    The Cromwell Current was discovered in 1952 [1][2] by Townsend Cromwell, a researcher with the Honolulu Laboratory of the Fish and Wildlife Service (later the United States Fish and Wildlife Service). It is 250 miles (220 nmi; 400 km) wide and flows to the east. It is hidden 300 feet (91 m) under the surface of the Pacific Ocean at the equator ...

  6. Geostrophic wind - Wikipedia

    en.wikipedia.org/wiki/Geostrophic_wind

    Geostrophic wind. In atmospheric science, geostrophic flow (/ ˌdʒiːəˈstrɒfɪk, ˌdʒiːoʊ -, - ˈstroʊ -/ [1][2][3]) is the theoretical wind that would result from an exact balance between the Coriolis force and the pressure gradient force. This condition is called geostrophic equilibrium or geostrophic balance (also known as geostrophy).

  7. Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_circulation

    Atmospheric circulation. Atmospheric circulation is the large-scale movement of air and together with ocean circulation is the means by which thermal energy is redistributed on the surface of the Earth. The Earth's atmospheric circulation varies from year to year, but the large-scale structure of its circulation remains fairly constant.

  8. North Pacific Gyre - Wikipedia

    en.wikipedia.org/wiki/North_Pacific_Gyre

    North Pacific Gyre. The North Pacific Gyre (NPG) or North Pacific Subtropical Gyre (NPSG), located in the northern Pacific Ocean, is one of the five major oceanic gyres. This gyre covers most of the northern Pacific Ocean. It is the largest ecosystem on Earth, located between the equator and 50° N latitude, and comprising 20 million square ...

  9. Surface weather analysis - Wikipedia

    en.wikipedia.org/wiki/Surface_weather_analysis

    A surface weather analysis for the United States on October 21, 2006. By that time, Tropical Storm Paul was active (Paul later became a hurricane). Surface weather analysis is a special type of weather map that provides a view of weather elements over a geographical area at a specified time based on information from ground-based weather stations.