Abstract
The El Niño Southern Oscillation (ENSO) is a well-known cause of year-to-year climatic variations on Earth. Floods, droughts, and other natural disasters have been linked to the ENSO in various parts of the world. Hence, modeling the ENSO’s effects and the anomaly of the ENSO phenomenon has become a main research interest. Statistical methods, including linear and nonlinear models, have intensively been used in modeling the ENSO index. However, these models are unable to capture sufficient information on ENSO index variability, particularly on its temporal aspects. Hence, this study adopted functional data analysis theory by representing a multivariate ENSO index (MEI) as functional data in climate applications. This study included the functional principal component, which is purposefully designed to find new functions that reveal the most important type of variation in the MEI curve. Simultaneously, graphical methods were also used to visualize functional data and capture outliers that may not have been apparent from the original data plot. The findings suggest that the outliers obtained from the functional plot are then related to the El Niño and La Niña phenomena. In conclusion, the functional framework was found to be more flexible in representing the climate phenomenon as a whole.
Highlights
The El Niño Southern Oscillation (ENSO) is an erratic climate phenomenon caused by coupled atmospheric–ocean interactions in the tropical Pacific Ocean
This study looked at how the multivariate ENSO index (MEI) changes are correlated with El Niño and La Niña
The findings indicate that Functional data analysis (FDA) could effectively describe changes in the MEI curve based on their derivatives, which can be calculated from their function
Summary
The El Niño Southern Oscillation (ENSO) is an erratic climate phenomenon caused by coupled atmospheric–ocean interactions in the tropical Pacific Ocean. The El Niño phenomenon refers to the prolonged heating of surface temperatures over the eastern and central Pacific Ocean for a half-year period of two to seven years. Different heating positions in the tropical Pacific Ocean have resulted in a wide range of consequences and climate anomalies all across the world. La Niña, on the other hand, is the polar opposite of El Niño and happens when ocean surface temperatures in the central and eastern Pacific Oceans fall below average. It brings in heavy rainfall in some locations, while others experience dry spells.
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