The records were divided into three reference datasets representing different compromises between spatial coverage and minimum record length, followed by further filtering based on continent, Köppen-Weiger climate classification, presence of dams, forest cover changes and catchment size.
For body weight, 440 records were divided randomly in 11 groups, each with 40 individuals.
Briefly, the SAP series derived from each recording were divided into 300 beat segments with a 50% overlap.
The records were divided between two reviewers who read the title and abstract of each record for an evaluation of relevance.
When the anomaly detection model was used, the records were divided into two peer groups, with an anomaly index cutoff of 1.760.
Figure 3 also shows the inconsistencies between the scales when the VAS records were divided into a five equidistant category scale.
The mean adherence to HAART for each eligible record was computed and the records were divided into two categories: adherent (average adherence greater than 95%) and non-adherent (≤ 95% adherence).
To evaluate the accuracy of the method we assumed feedback would be given at the end of each analysis interval; consequently records were divided into nonoverlapping consecutive analysis intervals of duration T w.
Past time on Earth, as inferred from the rock record, is divided into four immense periods of time called eons.
Firstly, the noisy seismic record is divided into some overlapping fragments.
