Instantaneous load estimates are derived from all observation in the estimation dataset using: hat{L}_{AMLE} = exp left( {a_{0} + sumlimits_{j = 1}^{M} {a_{j} X_{j} } } right)H a,b,s^{2},alpha,kappa ) (1 where ( hat{L}_{AMLE} ) is the AMLE instantaneous load estimate, a and b are explanatory variable functions, α and κ are gamma distribution parameters and s 2 is the residual variance [32 34].
Its initial estimates are derived from a mix of comprehensive data, samples and educated guesswork, and are refined over time.
First because climate sensitivity estimates are derived from computer models which may not correctly capture the various feedbacks on which the result depends.
The poverty estimates are derived from the household consumption expenditure data based on calories intake.
In [25], short-term FER estimates are derived from measurements of the signal-to-interference-plus-noise ratio (SINR).
By default, the decision values for calibrating the probability estimates are derived from a fivefold cross-validation of the training data set.
All estimates are derived from global databases and the scales, carbon pools, and time frame for each activity are given in Table 1.
We consider "direct" methods based on time-integrated measuring of mass flux, as well as "indirect" methods, where estimates are derived from concentration measurements.
