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In this paper, we call (1) the classical estimate (approach).
Indeed, if with, (1.12) is reduced to the classical estimate.
The optimum interstage pressure, thus obtained, deviate from the classical estimate of geometric mean of gas cooler and evaporator pressure.
It is based on the original exploitation of a result related to compensated compactness rather than on a classical estimate on the space and time translates in the spirit of Simon [49].
For instance, for solutions u ∈ W 1, p ( R n ) to (13) defined in the whole R n, the classical estimate via classical Riesz potentials | D u ( x ) | p - 1 ≤ c ∫ R n d | μ | ( y ) | x - y | n - 1 follows immediately.
Similar(55)
Indeed, if with, (1.8) is reduced to classical estimates.
This illustrates the masking effect: classical estimates can be highly affected by outlying observations.
Our results suggest complementing the classical estimates of life expectancy by adjustments using Horiuchi-Coale, Mitra, or other appropriate methods and avoiding the extrapolation method as a tool for estimating the life expectancy.
At this point it is clear that the classical estimates (5) embed in the family of interpolating estimates (12) as particular borderline cases corresponding to the choices α = 0 and α = 1, respectively.
Applying classical estimates (see [9]), we can see that ∥ u ε ∥ L ∞ ( Q T ) is bounded by ∥ f ∥ L ∞ ( Q T ), and u ε is Hölder continuous in Q T.
In order to evaluate the applicability of the proposed hierarchical Bayesian model for regional flood frequency analysis, we estimate flood quantiles for three randomly chosen out-of-sample sites and compare with classical estimates using the index flood method.
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