Prediction of Salinity Based on Meteorological Data Using the Backpropagation Neural Network Method

A. Azizah, D. C. R. Novitasari, Putroue Keumala Intan, F. Setiawan, Ghaluh Indah Permata Sari
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引用次数: 2

Abstract

Salinity is the level of salt dissolved in water. The salinity level of seawater can affect the hydrological balance and climate change. The salinity level of seawater in each area varies depending on the influencing factors, that is evaporation and precipitation (rainfall). One way to find out the salinity level is by taking seawater samples, which requires a long time and costs a lot. In this study, the salinity level of seawater can be predicted by utilizing time series data patterns from evaporation and precipitation using artificial neural network learning, namely the backpropagation neural network. The evaporation and precipitation data used were derived from the ECMWF dataset, while the salinity data were derived from NOAA where each data was taken at the coordinate point of 9,625 113,625 in the south of Java island. Seawater salinity, evaporation, and precipitation data were formed into a 7-day time series data. This study conducted several backpropagation architectural experiments, that is the learning rate, hidden layer, and the number of nodes in the hidden layer to obtain the best results. The results of the seawater salinity prediction were obtained at a MAPE value of 2.063% with a model architecture using 14 input layers, 2 hidden layers with 10 nodes and 2 nodes, 1 output layer, and a learning rate of 0.7. Predicted sea water salinity data ranging from 33 to 35 ppt. Therefore, the prediction system for seawater salinity using the backpropagation method can be said to be good in providing information about the salinity level of sea water on the island of Java.
基于气象资料的反向传播神经网络预测盐度
盐度是指溶解在水中的盐的含量。海水的盐度水平会影响水文平衡和气候变化。每个地区的海水盐度水平取决于影响因素,即蒸发和降水(降雨)。一种确定盐度水平的方法是采集海水样本,这需要很长时间和很多费用。在本研究中,利用人工神经网络学习,即反向传播神经网络,利用蒸发和降水的时间序列数据模式来预测海水的盐度水平。蒸发量和降水量数据来源于ECMWF数据集,盐度数据来源于NOAA数据集,每项数据均取自爪哇岛南部9,625 113,625坐标点。海水盐度、蒸发和降水数据形成一个7天的时间序列数据。本研究进行了几个反向传播架构实验,即学习率,隐藏层,隐藏层中的节点数,以获得最佳结果。海水盐度预测结果为MAPE值为2.063%,模型架构为14个输入层、2个10节点隐含层和2个节点隐含层、1个输出层,学习率为0.7。预测海水盐度数据范围为33至35 ppt。因此,使用反向传播方法的海水盐度预测系统可以说是很好的提供了爪哇岛海水盐度水平的信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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