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By avoiding traditional procedures that require long, continuous data segments, the Berkeley Earth methodology can also accommodate unusually short sequences: for example, those provided by temporary weather stations.
This methodology can also be used with nonlinear plant models.
The methodology can also be used where limited quantitative inputs are available.
The methodology can also be used to guide other grid adaptability tests.
The criticality assessment methodology can also be defined, considering different area scales.
The methodology can also construct one-sided functions for high-order interpolation and differentiation.
The generalized methodology can also be used for other relevant measurements.
The developed methodology can also apply to other proteins and biomolecular systems.
The modeling methodology can also be extended to other heat exchangers.
The calibration methodology can also be extended to more advanced LB methods.
Even more, the modeling methodology can also be extended to other heat exchangers.
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