Historical Archaeology

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Global changes in the weather linked with the La Nisa phenomenon , on the other hand , have been observed to be less prominent and in particular area , are likely to behave in the opposite way with regards to what is experienced with the El Niso phenomenon An El Niso episode has been determined to start with the presence of winds blowing in the easterly direction in the Pacific region , which is immediately opposite of the normal flow from east to west

During the 1960s , the strong correlation was established between the Southern Oscillation of the atmosphere and the El Niso phenomenon of the ocean , resulting in the compound event now known as the El Niso Southern Oscillation (ENSO The El Niso Southern Oscillation has been determined to carry two conditions that are described as extreme

Another phrase was coined in the 20st century – Southern Oscillation , which refers to the increase in pressure in the eastern Pacific region , which in turn results in the lowering of pressure in the western Pacific region (Murphy et al 2007

The central zone for rain is also modified to the easterly direction , pointing towards to the central Pacific region , resulting in an extended dry season in Indonesia , the Philippines and most of the northern region of Australia The Pacific region carries a higher temperature by the west side of South America

The use of terms related to the El Niso Southern Oscillation has been reported to be confusing because the phrase El Niso is often employed to describe issues relating to the phenomenon of El Niso Southern Oscillation

The cycle consists of the increase and decrease in temperature of the eastern Pacific bodies of water which influences the changes in the air pressure in the Pacific region

Employment of statistical tools showed that these weather changes were associated with the Southern Oscillation , such as the Asian monsoon and it provided a means in forecasting seasonal changes in the weather

In addition these easterly winds blow with a weak intensity

The warm event was earlier called El Niso , while the cold event was later coined as La Nisa

Due to the insufficiency of nutrients , the production of plankton is limited , influencing the rest of the food levels in the food chain , including the fishes and birds The level of the sea on either side of the Pacific is also disturbed by this effect

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