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  2. Gulf Stream - Wikipedia

    en.wikipedia.org/wiki/Gulf_Stream

    Surface temperatures in the western North Atlantic: Most of the North American landmass is black and dark blue (cold), while the Gulf Stream is red (warm). Source: NASA The Gulf Stream is a warm and swift Atlantic ocean current that originates in the Gulf of Mexico and flows through the Straits of Florida and up the eastern coastline of the United States, then veers east near 36°N latitude ...

  3. Loop Current - Wikipedia

    en.wikipedia.org/wiki/Loop_Current

    A map of the Loop Current. A parent to the Florida Current, the Loop Current is a warm ocean current that flows northward between Cuba and the Yucatán Peninsula, moves north into the Gulf of Mexico, loops east and south before exiting to the east through the Florida Straits and joining the Gulf Stream.

  4. California Current - Wikipedia

    en.wikipedia.org/wiki/California_Current

    The cooler ocean current along the west coast also makes summer temperatures cooler on the west coast compared to the east coast. For example, Half Moon Bay at 37°N has no month with an average high above 67 °F (19 °C) and San Francisco often stays below 70 °F (21 °C) in summer, while Virginia Beach, VA , close to the same latitude, has ...

  5. Gulf of Mexico - Wikipedia

    en.wikipedia.org/wiki/Gulf_of_Mexico

    The Gulf of Mexico (Spanish: Golfo de México) is an ocean basin and a marginal sea of the Atlantic Ocean, [3] [4] mostly surrounded by the North American continent. [5] It is bounded on the northeast, north, and northwest by the Gulf Coast of the United States; on the southwest and south by the Mexican states of Tamaulipas, Veracruz, Tabasco, Campeche, Yucatán, and Quintana Roo; and on the ...

  6. Gulf of California - Wikipedia

    en.wikipedia.org/wiki/Gulf_of_California

    The temperature of the water in the gulf generally experiences lows of 16 °C (61 °F) in winter and highs of 24 °C (75 °F) in summer. But temperatures can vary greatly in the gulf, and the water is almost always warmer by the coast than the open ocean.

  7. Thermohaline circulation - Wikipedia

    en.wikipedia.org/wiki/Thermohaline_circulation

    Effect of temperature and salinity upon sea water density maximum and sea water freezing temperature. It has long been known that wind can drive ocean currents, but only at the surface. [12] In the 19th century, some oceanographers suggested that the convection of heat could drive deeper currents.

  8. Latitude of the Gulf Stream and the Gulf Stream north wall index

    en.wikipedia.org/wiki/Latitude_of_the_Gulf...

    This model has also been tested using data from a coupled ocean-atmosphere model. [21] The latitude of the Gulf Stream is also affected by the El Nino-Southern Oscillation in the equatorial Pacific Ocean. [22] Silver et al. have combined wind-forcing and buoyancy in a forecast scheme. [23]

  9. North Pacific Current - Wikipedia

    en.wikipedia.org/wiki/North_Pacific_Current

    The Gulf of Alaska and the California Current receive different volumes and flows of warm water from the North Pacific Current. The Gulf of Alaska receives about 60% of the flow of the NPC while the California Current receives the remaining 40%. [1] These values may fluctuate, resulting in changes in the volume and the speed of the NPC water ...