A novel three-direction datum transformation of geodetic coordinates for Egypt using artificial neural network approach
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"A novel three-direction datum trans..." refers background or methods in this paper
...Although many different functions could be a successful transfer function, usually a differentiable and bounded function is used (Haykin 1994; Hagan et al. 1995)....
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...The training process continues until the network error reaches an acceptable value or has a stable state of estimated unknown parameters (Haykin 1994; Hagan et al. 1995)....
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...Three layers are the component of the ANN; these are input, hidden, and output layers; each layer contains one or more neurons (Ziggah et al. 2016; Haykin 1994; Hagan et al. 1995), as presented in Fig....
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...Three layers are the component of the ANN; these are input, hidden, and output layers; each layer contains one or more neurons (Ziggah et al. 2016; Haykin 1994; Hagan et al. 1995), as presented in Fig....
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18,794 citations
"A novel three-direction datum trans..." refers background or methods in this paper
...In this study, the standard multilayer feedforward network with a sigmoid transfer function in the hidden layer and a linear transfer function in the output layer is used because of its ability to approximate any measurable function to any desired degree of accuracy provided sufficiently many hidden units; in other word, it is a universal mapping tool (Hornik et al. 1989; Hagan et al. 1995)....
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...…the hidden layer and a linear transfer function in the output layer is used because of its ability to approximate any measurable function to any desired degree of accuracy provided sufficiently many hidden units; in other word, it is a universal mapping tool (Hornik et al. 1989; Hagan et al. 1995)....
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"A novel three-direction datum trans..." refers background in this paper
...observations in radian units, and there is no correlation between them (Mikhail 1976)....
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...…weights and biases as constants and geodetic coordinates (ϕ,λ) as independent observations in radian units, and there is no correlation between them (Mikhail 1976). σ2T̂ ¼ JΣxx J T ð16Þ where σ2 T̂ represents the variance of the estimated shift, Jis the Jacobian matrix relative to the geodetic…...
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