El Niño and La Niña are opposite phases of what is known as the El Niño-Southern Oscillation (ENSO) cycle. The ENSO cycle is a scientific term that describes the fluctuations in temperature between the ocean and atmosphere in the east-central Equatorial Pacific (approximately between the International Date Line and 120 degrees West).
La Niña is sometimes referred to as the cold phase of ENSO and El Niño as the warm phase of ENSO. These deviations from normal surface temperatures can have large-scale impacts not only on ocean processes, but also on global weather and climate.
El Niño and La Niña episodes typically last nine to 12 months, but some prolonged events may last for years. They often begin to form between June and August, reach peak strength between December and April, and then decay between May and July of the following year. While their periodicity can be quite irregular, El Niño and La Niña events occur about every three to five years. Typically, El Niño occurs more frequently than La Niña.
El Niño and La Niña are opposite phases of what is known as the El Niño-Southern Oscillation (ENSO) cycle. The ENSO cycle is a scientific term that describes the fluctuations in temperature between the ocean and atmosphere in the east-central Equatorial Pacific (approximately between the International Date Line and 120 degrees West).La Niña is sometimes referred to as the cold phase of ENSO and El Niño as the warm phase of ENSO. These deviations from normal surface temperatures can have large-scale impacts not only on ocean processes, but also on global weather and climate.El Niño and La Niña episodes typically last nine to 12 months, but some prolonged events may last for years. They often begin to form between June and August, reach peak strength between December and April, and then decay between May and July of the following year. While their periodicity can be quite irregular, El Niño and La Niña events occur about every three to five years. Typically, El Niño occurs more frequently than La Niña.
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El Niño and La Niña are opposite phases of what is known as the El Niño-Southern Oscillation (ENSO) cycle. The ENSO Cycle is a Scientific term that describes The Fluctuations in Temperature between The Ocean and atmosphere in The East-Central Equatorial Pacific (approximately between The International Date Line and 120 Degrees West). La Niña is sometimes referred to As The cold Phase of ENSO. and El Niño as the warm phase of ENSO. These deviations from normal surface temperatures Large-Scale Can Have Not only impacts on Ocean processes, but also on Global Climate and weather. El Niño and La Niña Episodes Typically Last Nine to 12 months, but some events prolonged May Last for years. They often begin to form between June and August, reach peak strength between December and April, and then decay between May and July of the following year. While their periodicity can be quite irregular, El Niño and La Niña events occur about every three to five years. Typically, El Niño occurs more frequently than La Niña.
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El Ni ñ O and La Ni ñ a are opposite phases of what is known as the El Ni ñ o-Southern Oscillation (ENSO) cycle. The ENSO cycle. Is a scientific term that describes the fluctuations in temperature between the ocean and atmosphere in the east-central. Equatorial Pacific (approximately between the International Date Line and 120 degrees West).
.La Ni ñ A is sometimes referred to as the cold phase of ENSO and El Ni ñ o as the warm phase of ENSO. These deviations from. Normal surface temperatures can have large-scale impacts not only on ocean processes but also, on global weather and climate.
El. Ni ñ O and La Ni ñ a episodes typically last nine to 12 months but some, prolonged events may last for years.They often begin to form between June and August reach peak, strength between December, and April and then decay between. May and July of the following year. While their periodicity can be quite irregular El Ni, ñ O and La Ni ñ a events occur about. Every three to five years. Typically El Ni, ñ o occurs more frequently than La Ni ñ a.
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