弓箭 发表于 2025-3-23 11:12:04
,Zusammengesetzte „Elementar“-Teilchen,c models. Multivariate time series and image data with huge amounts of freedom are now investigated by means of decomposition methods of data matrix and state-space modeling to infer macroscopic invariances in the natural phenomena using sparse modeling.爱好 发表于 2025-3-23 14:58:12
http://reply.papertrans.cn/39/3866/386577/386577_12.pngdebunk 发表于 2025-3-23 18:02:54
,„Eine andere Welt ist möglich!“, is different with that of the subduction boundary in the Japanese region. The characteristic features of the seismicity in the Northern California region are possibly investigated by the correlated seismicity likely to the Japanese seismicity.Ferritin 发表于 2025-3-24 00:07:37
https://doi.org/10.1007/978-3-531-92427-4he linear case of the correlated seismicity dynamics is simply expressed by the time derivatives (rate) of correlated seismicity with linear combination of several components of the correlated seismicity rates. On the other hand, the nonlinear case is rather complicated as the minimal nonlinear diff啤酒 发表于 2025-3-24 04:37:57
Bildhafte Vorstellungen des Willens of sparsity and Gaussian-type noises. The time series of the correlated seismicity is formulated by the state-space modeling method to their future behavior, that is the prediction of the seismicity. Furthermore, the local seismicity rates both in the global and regional cases may be estimated with迫击炮 发表于 2025-3-24 07:57:35
http://reply.papertrans.cn/39/3866/386577/386577_16.pngcarbohydrate 发表于 2025-3-24 13:22:09
http://reply.papertrans.cn/39/3866/386577/386577_17.png擦试不掉 发表于 2025-3-24 15:07:47
Data-Driven Science for Geosciences,c models. Multivariate time series and image data with huge amounts of freedom are now investigated by means of decomposition methods of data matrix and state-space modeling to infer macroscopic invariances in the natural phenomena using sparse modeling.Liberate 发表于 2025-3-24 20:37:16
http://reply.papertrans.cn/39/3866/386577/386577_19.pngIncompetent 发表于 2025-3-25 00:02:29
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