Abstract

Indian Ocean Dipole (IOD) is a large-scale physical ocean phenomenon in the Indian Ocean that plays an important role in predicting the El Nino Southern Oscillation in the tropical Pacific. Predicting the occurrence of IOD is of great significance to the study of climate change and other marine phenomena. Generally, the IOD index is calculated to judge whether the IOD occurs. In this paper, a convolutional LSTM (convLSTM) neural network is used to build the deep learning model to predict the sea surface temperature in the next seven months and calculate the IOD index. Through the analysis of marine atmospheric data with complex temporal and spatial relationships, the wind field signal knowledge of the physical ocean is introduced to predict IOD phenomenon by combining the prior knowledge of the physical ocean and deep learning. The experimental results show that the average correlation of IOD index time series to the true IOD index time series is 82.87% from 2015 to 2018, seven months ahead for IOD prediction. IOD manifests as sea surface temperature (SST) anomaly changes, and this thesis verifies that the wind field signal information has a positive impact on the prediction of IOD changes. Moreover, the convLSTM can predict this anomaly better. The IOD index line graph can generally fit the real IOD index variation trend, which has a profound impact on the study of the IOD phenomenon.

Highlights

  • IntroductionIndian Ocean Dipole (IOD) is one of the important systems affecting climate anomalies in Asia

  • Received: 23 December 2021Indian Ocean Dipole (IOD) is one of the important systems affecting climate anomalies in Asia

  • For the selection of features, this paper considers the complex characteristics of the marine atmosphere dataset, including sea surface temperature, underwater temperature, underwater velocity, atmospheric temperature, humidity, and so on

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Summary

Introduction

IOD is one of the important systems affecting climate anomalies in Asia. Proposed the concept of IOD in 1999. Saji defined the IOD index as the mean sea surface temperature in the western Indian Ocean (50◦ E~70◦ E, 10◦ S~10◦ N) minus the mean sea surface temperature in the eastern Indian Ocean (90◦ E~110◦ E, 10◦ S~0◦ ). IOD has significant seasonal phase-locking characteristics, which usually start to develop in summer, reaching their peak in autumn, and decaying rapidly in winter [2]. Since 1999, IOD has attracted the attention of scientists at home and abroad. IOD is of great help in predicting El Nino Southern oscillation [3]. IOD can affect the global climate through large-scale teleconnection [4].

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