The SMB values are estimated for the 27 glacier drainage basins.
Water use values are estimated for urban/domestic, agricultural, industrial, livestock, and tourism water users.
Hourly average radiation values are estimated from daily values using a statistical model.
Then, using this model, unknown values are estimated based on a limited number of random samples.
It is shown that the deviations between the predicted and experimental values are estimated within ±12% for 75% experimental conditions.
Depending upon model specification, per person per trip values are estimated to be in the range of $76 to $135.
In order to perform a dynamic and powerful control action, future error values are estimated by gray modeling technique.
The values are estimated from a field-gradient force, mχB dB/dx), that is applied on the particle as it translates through the gap of the circuit; detail of calculation is described in Fig. 3 (Supplementary Note B).
Afterwards, the TOC values are estimated from well log data by using the individual Artificial Neural Network (ANN) models constructed for each EF.
These flamelets are then used to generate a turbulent look-up table where mean values are estimated by integration over presumed probability density functions.
Q values are estimated for other volcanoes.
