2020
DOI: 10.5194/esd-11-835-2020
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Reconstructing coupled time series in climate systems using three kinds of machine-learning methods

Abstract: Abstract. Despite the great success of machine learning, its application in climate dynamics has not been well developed. One concern might be how well the trained neural networks could learn a dynamical system and what will be the potential application of this kind of learning. In this paper, three machine-learning methods are used: reservoir computer (RC), backpropagation-based (BP) artificial neural network, and long short-term memory (LSTM) neural network. It shows that the coupling relations or dynamics a… Show more

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Cited by 16 publications
(9 citation statements)
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“…Normally, the Pearson feature selection is used for linear relationships, but a weak linear correlation does not mean that there is no coupling relation between the variables (Huang et al, 2020) used similar approach for complex models.…”
Section: Data Descriptionmentioning
confidence: 99%
“…Normally, the Pearson feature selection is used for linear relationships, but a weak linear correlation does not mean that there is no coupling relation between the variables (Huang et al, 2020) used similar approach for complex models.…”
Section: Data Descriptionmentioning
confidence: 99%
“…However, links between climate fields can be nonlinear (Schneider et al, 2018;Dueben and Bauer, 2018;Huntingford et al, 2019;Nadiga, 2020). Nonlinear machine-learning-based CFR methods (for instance, artificial neural networks, ANN) could help capture underlying linear and nonlinear relationships between proxy records and the large-scale climate (Rasp and Lerch, 2018;Schneider et al, 2018;Rolnick et al, 2019;Huang et al, 2020;Nadiga, 2020;Chattopadhyay et al, 2020;Lindgren et al, 2021). Moreover, machine-learning methods do not necessarily rely on statistical methods to first obtain the principal spatial climate patterns, such as principal component analysis (PCA).…”
Section: Introductionmentioning
confidence: 99%
“…However, climate change is dynamic and chaotic, and many links between climate fields can be non-linear (Schneider et al, 2018;Dueben and Bauer, 2018;Huntingford et al, 2019;Nadiga, 2020). Nonlinear machine leaning-based CFR methods (for instance, Artificial Neural Networks-ANN) could help capture capture underlying linear and nonlinear relationships between proxy records and the large-scale climate as realistically as possible (Rasp and Lerch, 2018;Schneider et al, 2018;Rolnick et al, 2019;Huang et al, 2020;Nadiga, 2020;Chattopadhyay et al, 2020;Lindgren et al, 2021). Moreover, machine-learning methods do not necessarily rely on statistical methods to first obtain the principal spatial climate patterns, such as Principal Component Analysis-PCA.…”
mentioning
confidence: 99%
“…The state of the output gate ot is calculated from the previous hidden state and the current input variables (equation 11). This output is used to compute the updated hidden state ht using the state of the cell output Ct (equation 12)(Huang et al, 2020;Chattopadhyay et al, 2020).In the present application to climate reconstructions, we have a set of input pseudoproxy data𝑿 𝑡 𝑛 = [xt-i,…, xt-1]and an output target temperature time series 𝒀 𝑡 𝑚 = [yt-i,…, yt-1]. The forward LSTM hidden state sequence 𝒉 𝑡 ⃑⃑⃑⃑ (note the arrow direction) is calculated employing inputs information in a positive direction from time t-1 to time t-n iteratively, and for backward LSTM…”
mentioning
confidence: 99%