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Pacific Ocean Currents. The arrows show the direction of ocean currents recorded by William Dampier while crossing “La Grande Mer du Sud”—the Pacific Ocean. The map appeared in Dampier’s second book, Voyages and Descriptions, published in early 1699.
- North Equatorial Current (Warm): The north equatorial current originates off the western coast of Mexico and flows in westerly direction (fig. 29.2) and reaches the Philippines coast after covering a distance of 7500 nautical miles.
- South Equatorial Current (Warm): The south equatorial current is originated due to the influence of south-east trade winds and flows from east to west.
- Counter Equatorial Current (Warm): The current flowing west to east between the north and south equatorial currents is termed counter equatorial current.
- Kuroshio System (Warm): The Kuroshio system comprised of several currents and drifts is similar to the Gulf Stream system of the Atlantic Ocean. This system runs from Taiwan to the Bering Strait and consists of the Kuroshio Current, the Kuroshio extension, the north Pacific drift, the Tsushima current and the counter Kuroshio Current.
The Southern Pacific Gyre is part of the Earth's system of rotating ocean currents, bounded by the Equator to the north, Australia to the west, the Antarctic Circumpolar Current to the south, and South America to the east.
Aug 1, 2011 · Winds, water density, and tides all drive ocean currents. Coastal and sea floor features influence their location, direction, and speed. Earth’s rotation results in the Coriolis effect which also influences ocean currents.
3 days ago · Ocean Prediction Center - Pacific Marine. Analysis – Graphical Forecasts – Text Forecasts – Hazards – Gridded – Other Marine. Pacific Analysis. Click on the map below or choose from: W Pacific.
The visualizer allows you to select a region of the ocean and study changes happening in the region. Each map has arrows showing the current direction and the colors indicate the strength of the current speed, the current direction, the current convergence or the current vorticity.
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The simplified map in Fig. 3.13 shows the surface winds that flow from regions of high atmospheric pressure over the world’s oceans. These are winds that drive the system of surface currents in the ocean. Surface currents are only 50 to 100 meters deep (Table 3.1).
