El Niño is a climate phenomenon characterized by the warming of sea surface temperatures in the central and eastern tropical Pacific Ocean. It can lead to changes in weather patterns around the world, including increased rainfall in some areas and drought in others. El Niño events typically occur every 2-7 years and can have significant impacts on agriculture, fisheries, and extreme weather events.
El Niño and La Niña (collectively called El Niño Southern Oscillation or ENSO) don't just affect the US. They affect the whole world. As of October 2013, the current condition is ENSO neutral, meaning we have neither El Niño nor La Niña, but are somewhere in between.
ENSO stands for "El Nino Southern Oscillation," which is the full name of the phenomena commonly referred to as El Nino. ENSO is the preferred nomenclature of the phenomena because El Nino only refers to the warm phase of the oscillation, while La Nina is the cool phase. ENSO refers to both these phases in the phenomena. ENSO has a variety of complex, poorly-understood causes, but it does tend to oscillate between its two phases every three to seven years. El Nino is characterized by a reversal of the Trade Winds in the equatorial Pacific. This results in warmer water moving east all the way to the coast of South America, where cold water is typically up-welled. La Nina is an enhanced phase of the "normal" conditions, which feature stronger Trade Winds. This allows the up-welling to become more pronounced and keeps the warm water confined to the Western Pacific. In terms of what this does to tropical cyclones, the results vary among the different ocean basins. In the Eastern Pacific, for example, hurricane activity is increased during an El Nino and decreased in the La Nina. However, the opposite occurs in the Atlantic Basin, primarily due to increased wind shear (during El Nino), which disrupts cyclone formation. ENSO is one of several mechanisms that can influence the amount of cyclone activity in a particular year in a given basin. Properly attributing the level of activity to one specific forcing, or to a combination of specific forcings, is nearly impossible.
Enso results from dynamic and thermodynamic interactions. These interactions happen in the atmosphere, oceans, and land surfaces, although specificallywhat causes ENSO is unclear. Aside from that, scientists believe air pressure changes and wind currents play a vital role in starting El Nino/ Southern Oscillation. Some researcher think greenhouse gases may play a role. Others say underwater activity; underwater earthquakes for example, cause El Nino.
The weather phenomenon is known as El Nino.
La Niña and El Niño occur at different times and are opposite phases of the El Niño-Southern Oscillation (ENSO) cycle. It is rare for them to occur at the same time, but it can happen during a transition period when one phase is weakening and the other is starting to strengthen. This transitional phase is known as ENSO neutral.
El Nino-Southern Oscillation
El Nino-Southern Oscillation
the state of ENSO can be used to help forecasters in prediction of calamities like El Nino and El Nina
ENSO- El Nino Southern Oscillations The ENSO has influence on the strength and schedule of SW Monsoon in India, making it weaker than normal during the El Nino period. But the La Nina has opposite effect than El Nino. La Nina years have a particularly better signs of monsoon in India.
El Niño and La Niña (collectively called El Niño Southern Oscillation or ENSO) don't just affect the US. They affect the whole world. As of October 2013, the current condition is ENSO neutral, meaning we have neither El Niño nor La Niña, but are somewhere in between.
la Nina
ENSO stands for "El Nino Southern Oscillation," which is the full name of the phenomena commonly referred to as El Nino. ENSO is the preferred nomenclature of the phenomena because El Nino only refers to the warm phase of the oscillation, while La Nina is the cool phase. ENSO refers to both these phases in the phenomena. ENSO has a variety of complex, poorly-understood causes, but it does tend to oscillate between its two phases every three to seven years. El Nino is characterized by a reversal of the Trade Winds in the equatorial Pacific. This results in warmer water moving east all the way to the coast of South America, where cold water is typically up-welled. La Nina is an enhanced phase of the "normal" conditions, which feature stronger Trade Winds. This allows the up-welling to become more pronounced and keeps the warm water confined to the Western Pacific. In terms of what this does to tropical cyclones, the results vary among the different ocean basins. In the Eastern Pacific, for example, hurricane activity is increased during an El Nino and decreased in the La Nina. However, the opposite occurs in the Atlantic Basin, primarily due to increased wind shear (during El Nino), which disrupts cyclone formation. ENSO is one of several mechanisms that can influence the amount of cyclone activity in a particular year in a given basin. Properly attributing the level of activity to one specific forcing, or to a combination of specific forcings, is nearly impossible.
Enso results from dynamic and thermodynamic interactions. These interactions happen in the atmosphere, oceans, and land surfaces, although specificallywhat causes ENSO is unclear. Aside from that, scientists believe air pressure changes and wind currents play a vital role in starting El Nino/ Southern Oscillation. Some researcher think greenhouse gases may play a role. Others say underwater activity; underwater earthquakes for example, cause El Nino.
El Nino is bad
The weather phenomenon is known as El Nino.
'El Nino' means 'the christ child'
El nino jesus