A layer of neurons is estimated by its weight matrix, a transfer function and a bias vector.
This has added an extra layer of uncertainty to the estimates that should be borne in mind when interpreting the results, but which reinforces our first caveat.
The C density of pre-fire ground layer expressed as kg C m-2 per cm depth of the ground layer, our estimate of 0.34 kg C m-2 per cm depth is comparable to the 0.36 kg C m-2 per cm depth derived from the data of Kasischke et al. [21], but higher than the 0.21 kg C m-2 per cm depth reported by Kane et al. [22].
The C density of pre-fire ground layer expressed as kg C m-2 per cm depth of the ground layer, our estimate of 0.34 kg C m-2 per cm depth is comparable to the 0.36 kg C m-2 per cm depth derived from the data of Kasischke et al. [ 21], but higher than the 0.21 kg C m-2 per cm depth reported by Kane et al. [ 22].
As a first approximation, we consider the thickness of pure gold: the layer of gold can be estimated around 1.5 μm in the frame of the text (painted area) whereas it is approximately 0.1 μm as gold leaf.
Here, we also compare the locations of the upper-plane seismic belt and the down-dip end of the seismic low-velocity layer with thermal petrological estimates of the positions of the dehydration reaction boundaries in the slab crust, although there is high uncertainty in their positions because of error in the estimation of temperature distribution in the subducting slab.
The single neuron in the output layer then estimates the class of the unknown compound x by comparing all the probability density function from the summation neurons and choosing the class with the highest probability density function.
The uncertainty of the conductivity of each layer is estimated by evaluating the distribution of the acceptable models obtained through numerous inversion runs with different constraints, following our previous studies (Baba et al. 2010, 2013a).
But the specific deposit resistance of the protein layer is estimated to be of the order of 6 × 1015 m/kg at a pressure of 130 kPa, much higher than for red cells.
The other evidence was that the quantity ratio for the surface and inner layers, viz., oxidized and not-oxidized layers, was estimated to be about 2 1 from thermogravimetric analysis, and this value largely coincided with the surface and inner ratio of layer numbers estimated from the histogram for the layer number.
