La Niñ Climate Analysis

By the global conveyor belt transferring heat, it affects the climate. The Gulf Stream is a part of the thermohaline circulation, it is another current that allows Western Europe to be warmer in winter then any other country at the same latitude. The La Niña can be referred to as the extensive cooling of the Pacific Ocean, it is often accompanied by much warmer sea water then the surface temperatures (SSTs) in the western Pacific Ocean, and the north of Australia. The El Niño is currently the best known extreme of the Southern Oscillation, it is also classified as one of the most important influences on the climate in Australia. (Pearson, 2015). Surface currents keep the Earth's temperatures normal. As surface currents travel, they absorb the heat from the tropical regions surrounding the equator and release it into the colder regions near the North and South Pole. Deep water currents move extremely slow,
This is related to salinity and temperature levels. Water that is cold and salty is a lot heavier than water that is warm and fresh. Water near the North and South poles is colder and much saltier than water closer to the equator. The cold water travels below the ocean surface currents towards the equator, where it is then warmed. The water then rises and replaces the water that the surface currents carry towards the North and South poles. (Science clarified, 2015). The Southern Oscillation is the pattern of changes in which the way the atmosphere and water circulate together across the Indonesian Islands and Pacific Ocean. The Southern Oscillation also gives rise to the El Niño and La Niña effects. The southern Oscillation Index (SOI) is the measure of the ocean and atmospheric conditions across the Pacific Ocean, it can be calculated by using the difference in air pressure between Tahiti and Darwin. The ocean currents and atmosphere interact together as they both transfer heat energy across the