The reversal of oceanic currents in the equatorial Pacific is commonly called El Niño. This phenomenon involves a periodic warming of sea surface temperatures in the central and eastern tropical Pacific, which can disrupt normal weather patterns globally. El Niño events typically occur every few years and can have significant impacts on climate, marine ecosystems, and weather-related phenomena.
The North Equatorial Current and South Equatorial Current in the Pacific Ocean are both warm, fast-moving currents that flow towards the west. They are driven by the trade winds. One key difference is that the North Equatorial Current is influenced by the North Pacific Gyre, while the South Equatorial Current is influenced by the South Pacific Gyre.
The Pacific Equatorial Undercurrent is also known as the Equatorial Undercurrent. It is a narrow, deep, and swift eastward-flowing ocean current located in the equatorial region of the Pacific Ocean.
A periodic reversal of the pattern of mid-Pacific ocean currents is known as the El Niño Southern Oscillation (ENSO). This phenomenon involves the warming of ocean temperatures in the central and eastern tropical Pacific, leading to changes in atmospheric circulation patterns and global weather impacts. These events typically occur every 2-7 years and can have significant effects on weather patterns worldwide.
It doesn't. El Nino has impacts all around the world. The ultimate trigger, though relates to the reversal of a wind current over the equatorial Pacific, which produces the characteristic warming of the surface waters. A few other patterns similar to El Nino have been identified, but these are separate events.
Three major surface currents are the Gulf Stream in the North Atlantic Ocean, the Kuroshio Current in the North Pacific Ocean, and the Antarctic Circumpolar Current in the Southern Ocean. These currents play a significant role in distributing heat and nutrients around the globe.
The North Equatorial Current and South Equatorial Current in the Pacific Ocean are both warm, fast-moving currents that flow towards the west. They are driven by the trade winds. One key difference is that the North Equatorial Current is influenced by the North Pacific Gyre, while the South Equatorial Current is influenced by the South Pacific Gyre.
The warm, low salinity waters from Pacific are transported into Indian Ocean's South Equatorial Current.
El Nino
The Pacific Equatorial Undercurrent is also known as the Equatorial Undercurrent. It is a narrow, deep, and swift eastward-flowing ocean current located in the equatorial region of the Pacific Ocean.
A periodic reversal of the pattern of mid-Pacific ocean currents is known as the El Niño Southern Oscillation (ENSO). This phenomenon involves the warming of ocean temperatures in the central and eastern tropical Pacific, leading to changes in atmospheric circulation patterns and global weather impacts. These events typically occur every 2-7 years and can have significant effects on weather patterns worldwide.
El Nino (~over the n)
Robert H. Harvey has written: 'Bottom current and pressure measurements from the central equatorial Pacific' -- subject(s): Measurement, Ocean currents, Oceanography, Pressure
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Only some of it which is known as the Equatorial Pacific, or Tropical Pacific. The rest of the pacific isn't tropical though
It doesn't. El Nino has impacts all around the world. The ultimate trigger, though relates to the reversal of a wind current over the equatorial Pacific, which produces the characteristic warming of the surface waters. A few other patterns similar to El Nino have been identified, but these are separate events.
Because the Equatorial counter current lies in the pacific and Indian oceans.
Three major surface currents are the Gulf Stream in the North Atlantic Ocean, the Kuroshio Current in the North Pacific Ocean, and the Antarctic Circumpolar Current in the Southern Ocean. These currents play a significant role in distributing heat and nutrients around the globe.