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  2. Heceta Bank - Wikipedia

    en.wikipedia.org/wiki/Heceta_Bank

    The upwelling front is accompanied by a geostrophic upwelling jet. During the summer upwelling season, the southward flowing jet off of central Oregon lies mid-shelf at approximately the 100-m isobath. [14] Its near-surface speed averages 0.35 m/s, with individual events exceeding 0.80 m/s. [15] This is faster than the surrounding water ...

  3. Upwelling - Wikipedia

    en.wikipedia.org/wiki/Upwelling

    For example, off the coast of Oregon, there are four or five strong upwelling events separated by periods of little to no upwelling during the six-month season of upwelling. In contrast, tropical latitudes have a more constant temperature contrast, creating constant upwelling throughout the year.

  4. Coos Bay - Wikipedia

    en.wikipedia.org/wiki/Coos_Bay

    Seasonal winds cause tides and upwelling that influence nutrients and the biogeochemistry of Coos Bay estuary. One third of macrophyte production in the estuary is attributed to upwelling. [22] In the summer, wind primarily comes from the North along the Oregon coast, bringing up nutrient-rich deep water and boosting primary production. [23]

  5. California Current - Wikipedia

    en.wikipedia.org/wiki/California_Current

    Additionally, extensive upwelling of colder sub-surface waters occurs, caused by the prevailing northwesterly winds acting through the Ekman Effect. The winds drive surface water to the right of the wind flow, that is offshore, which draws water up from below to replace it. The upwelling further cools the already cool California Current.

  6. Nutrient cycling in the Columbia River Basin - Wikipedia

    en.wikipedia.org/wiki/Nutrient_cycling_in_the...

    Rather, the primary source of nitrate into the estuary is from ocean exchange caused by wind-driven seasonal upwelling off the Oregon and Washington coasts. [8] This influx of nitrate, generally the primary limiting nutrient to biological communities in the estuary, is an important driver of primary productivity in estuarine plumes of river ...

  7. Front (oceanography) - Wikipedia

    en.wikipedia.org/wiki/Front_(Oceanography)

    The contrast between the cold water from depth and warmer surface water leads to the formation of coastal upwelling fronts. [21] Examples of such fronts occur off the coast of Washington-Oregon-California and Peru-Chile. [9]

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    mail.aol.com

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  9. List of ecoregions in Oregon - Wikipedia

    en.wikipedia.org/wiki/List_of_ecoregions_in_Oregon

    The task of defining and mapping these ecoregions was carried out by the Oregon Ecoregion Project, a collaborative effort involving the EPA, the United States Geological Survey (USGS), the United States Forest Service (USFS), and other state and federal agencies. The new classification system they developed may differ from previous frameworks ...