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Four distance thresholds (2, 4, 8, 12 km) were considered to compare the patch importance of connectivity by dECA values.
Quetta area has a shallow seismicity hence earthquakes of focal depth less than 30 km were considered.
Five typical algorithms (Correlation coefficients (CC), Euclidean distance (ED), Mahalanobis distance (MD), Angle cosine (AC), and k-medoids (KM)) were considered for the identification in the SAM model.
In this study, to evaluate the distribution of response in far- and near-field earthquakes, two sets of records were chosen from PEER (2012) strong ground motion database with magnitude equal or >5 that recorded soil type I. Earthquakes with fault-to-site distance <15 km were considered as near-field, and higher than 15 were considered as far-field.
Distances of up to 15 km were considered in the analysis.
Consequently, all areas where mean PfPR2 10 was ≥ 1% and where population density was also ≥ 1 person per km were considered priority areas for the future distribution of LLINs in Kenya.
Similar(51)
Even though 73% of Europeans live in urban areas – the most urbanised of the four global regions – the urbanisation density threshold is low, meaning that areas with more than 314 people/sq km are considered urban, contrasting with India where this threshold is over 10 times higher.
A rectangular area of 2 ×2 km is considered.
Two constellations with satellite orbit altitudes of only 800 km or 1000 km are considered first.
Each 1 km was considered as the unit cost to convert this distance to cost.
Events shallower than 300 km are defined as intermediate-depth earthquakes, and those deeper than 300 km are considered deep-focus earthquakes.
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