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  2. Sea state - Wikipedia

    en.wikipedia.org/wiki/Sea_state

    The significant wave height H 1/3 — the mean wave height of the highest third of the waves. The mean wave period, T 1. In addition to the short-term wave statistics presented above, long-term sea state statistics are often given as a joint frequency table of the significant wave height and the mean wave period.

  3. Ocean Prediction Center - Wikipedia

    en.wikipedia.org/wiki/Ocean_Prediction_Center

    The Ocean Applications Branch plays an important role in enhancing OPC operations and services. One example is the adaptation of ocean surface winds observed from the QuikSCAT satellite in early 2000. Prior to the QuikSCAT launch, there was no ability to observe, verify, and warn of hurricane-force wind conditions, areas where wind speed ...

  4. Significant wave height - Wikipedia

    en.wikipedia.org/wiki/Significant_wave_height

    The RMS wave height, which is defined as square root of the average of the squares of all wave heights, is approximately equal to H s divided by 1.4. [2] [8] For example, according to the Irish Marine Institute: [9] "… at midnight on 9/12/2007 a record significant wave height was recorded of 17.2m at with [sic] a period of 14 seconds."

  5. Wind wave - Wikipedia

    en.wikipedia.org/wiki/Wind_wave

    The Pacific Ocean is 19,800 km ... It is composed of a wave height spectrum ... Current global map of significant wave heights This page was ...

  6. Columbia Bar - Wikipedia

    en.wikipedia.org/wiki/Columbia_Bar

    The waves are partially caused by the deposition of sediment as the river slows, as well as mixing with ocean waves. The waves, wind, and current are hazardous for vessels of all sizes. The Columbia current varies from 4 to 7 knots (7.4 to 13.0 km/h ) westward, and therefore into the predominantly westerly winds and ocean swells, creating ...

  7. Ocean surface topography - Wikipedia

    en.wikipedia.org/wiki/Ocean_surface_topography

    Ocean surface topography or sea surface topography, also called ocean dynamic topography, are highs and lows on the ocean surface, similar to the hills and valleys of Earth's land surface depicted on a topographic map. These variations are expressed in terms of average sea surface height (SSH) relative to Earth's geoid. [1]

  8. 'Rogue' or 'sneaker?' What caused the giant wave in the ... - AOL

    www.aol.com/weather/rogue-sneaker-caused-giant...

    You've probably seen the viral video of a large wave inundating a building. A triple-screen view from several cellphone cameras proves even more impressive. The big wave happened on Saturday, Jan ...

  9. Pacific Ocean - Wikipedia

    en.wikipedia.org/wiki/Pacific_Ocean

    The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions.It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on the definition, to Antarctica) in the south, and is bounded by the continents of Asia and Australia in the west and the Americas in the east.