“…More importantly, optimization algorithms such as stochastic gradient descent (SGD), root mean square propagation (RMSprop), adaptive grad (AdaGrad), adaptive delta (AdaDelta), adaptive moment estimation (Adam), adaptive maximum (Adamax), and Nesterov‐accelerated adaptive moment estimation (Nadam) are absent in the typhoon rainfall forecasting model based on the DL model (Huang et al., 2018; Lin & Chen, 2005; Lin & Wu, 2009; Wei & Chou, 2020). These optimization algorithms have successfully been applied in rainfall forecasting (Barrera‐Animas et al., 2021; Fadilah et al., 2021; Manoj & Ananth, 2020; Prasetya & Djamal, 2019; Sari et al., 2020; Zhang et al., 2018), spatial prediction of landslides (Bui et al., 2019), wind speed and wind direction forecasting (Puspita Sari et al., 2020; Saputri et al., 2020), evapotranspiration forecasting (Walls et al., 2020), run‐off forecasting (Nath et al., 2021), air quality index prediction (H. He & Luo, 2020), river stage, flash flood susceptibility and streamflow forecasting (Hitokoto et al., 2017; Rahimzad et al., 2021; Tien Bui et al., 2020), water demand forecasting (Koo et al., 2021), temperature and global solar radiation prediction (Del & Starchenko, 2021; Ghimire et al., 2019).…”