La niña translates as 'girl-child' and is the opposite enso phase to el niño coupled because enso involves interaction between the ocean and the atmosphere – both of which play a role in reinforcing changes in each other – it is known as a coupled ocean–atmosphere phenomenon. Difference between la nina and el nino january 17, 2011 posted by aron la nina vs el nino although both la nina and el nino are phenomena possibly caused by global warming, they both are two different conditions that occur in the ocean surface temperature across the central and eastern tropical pacific fishermen off the west coast of south.
The phenomenon known as el niño is sometimes reverses, leading to strong trade winds, colder than normal water off the coast of peru, and warmer than normal water near australia this cold counterpart to el niã±o is known as la niña. Shared characteristics: of el nino and la nina el niño and la niña are pacific ocean-atmospheric systems the most powerful phenomenon on earth alters more than half the planet's climate what caused and increased number of hurricanes (la niña) due to strong trade winds.
El niño and la niña: what are they both el niño and la niña are opposite effects of the same phenomenon: the enso (el niño southern oscillation) both are an oscillation in the temperatures between the atmosphere and the ocean of the eastern equatorial pacific region, roughly between the international dateline and 120 degrees west (2. Temperature during el niño precipitation during el niño : temperature during la niña precipitation during la niña : for a more complete look at temperature and precipitation in the us, see the climate prediction center's la niña and el niño impact pages. La niña (/ l ɑː ˈ n iː n j ə /, spanish pronunciation: ) is a coupled ocean-atmosphere phenomenon that is the counterpart of el niño as part of the broader el niño–southern oscillation climate pattern.
La nina is a climate pattern that describes the cooling of surface ocean water along the tropical west coast of south america both el niño and la niña affect patterns of rainfall, atmospheric pressure, and global atmospheric circulation (el nio), and atmospheric pressure decreases at the ocean surface in the western tropical pacific.
In the northern hemisphere, the peak season for el nino and la nina is during the winter characteristics of an el nino cycle a large pool of warm water is located in the central and western part of the pacific ocean atmospheric conditions can increase the temperature of the surface water.
A long-lasting warm spell in the central-eastern tropical pacific is one of the criteria for el niño el niño and la niña are the warm and cool phases of a recurring climate pattern across the tropical pacific—the el niño-southern oscillation, or “enso” for short.
What is la nina and el nino la nina is described as cooler-than-normal sea surface temperatures in the central and eastern pacific ocean, near the equator off the west coast of south america el nino is like la nina's brother, the totally opposite and attention grabbing brother.
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. El nino and la nina are caused by the sea-surface temperatures in the tropical part of the pacific ocean interacting with the atmosphere the cycle of the water temperature changing from warm to. The enso cycle, both el niño and la niña, cause global changes of both temperatures and rainfall over california and the south-western united states, there is a weak relationship between el nino and above-average precipitation, as it strongly depends on the strength of the el niño event and other factors. What happens during a typical el niño the trade winds that blow from east-to-west cease, decrease in intensity, or reverse trade winds normally keep warm water pushed to the west side of the equatorial pacific.