Abstract

Mean sea level rise is a significant emerging risk from climate change. This research paper is based on the use of artificial intelligence models to assess and predict the trend on mean sea level around northern Australian coastlines. The study uses sea-level times series from four sites (Broom, Darwin, Cape Ferguson, Rosslyn Bay) to make the prediction. Multivariate adaptive regression splines (MARS) and artificial neural network (ANN) algorithms have been implemented to build the prediction model. Both models show high accuracy (R2 > 0.98) and low error values (RMSE < 27%) overall. The ANN model showed slightly better performance compared to MARS over the selected sites. The ANN performance was further assessed for modelling storm surges associated with cyclones. The model reproduced the surge profile with the maximum correlation coefficients ~0.99 and minimum RMS errors ~4 cm at selected validating sites. In addition, the ANN model predicted the maximum surge at Rosslyn Bay for cyclone Marcia to within 2 cm of the measured peak and the maximum surge at Broome for cyclone Narelle to within 7 cm of the measured peak. The results are comparable with a MARS model previously used in this region; however, the ANN shows better agreement with the measured peak and arrival time, although it suffers from slightly higher predictions than the observed sea level by tide gauge station.

Highlights

  • Since the Artificial Neural Network (ANN) and Multivariate Adaptive Regression Splines (MARS) models can model out the non-linearity in a given set of data, this study aims to compare the performance of ANN model to the previously used model (MARS) in order to select the best method for predicting sea level at the northern Australian region

  • Results obtained from the MARS and ANN model for forecasting mean sea level around northern Australian coastlines were assessed to validate the study

  • All root mean square error (RMSE) metrics at all locations generated by the ANN model were slightly lower than those of the MARS model

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Summary

Introduction

During the last two decades, the rate of sealevel rise around the Australian region has not been consistent, with the sea-level trend due the dynamic influence induced by internal climate modes about three times greater than the global mean sea-level around the north and north-west of Australia [1,2]. The MR model slightly underestimates the observed sea-level variability. This is due to the fact that the linear MR model may not be able to closely fit the reality of sea-level features, which are naturally non-linear and vary greatly over time [6,7,8] highlighted the non-linearity of mean sea-level rise based on analysis of the world’s longest records

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