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The air velocity distribution at each measuring station was analyzed using an air velocity contour map generated with Surfer®.
To investigate the correlation between the air velocity distribution and the deviation of the two air velocity measuring methods, the standard deviation at each measuring station was calculated using the nine measured fixed-point velocities.
The mean observed sky brightness for fully overcast skies at our urban measuring station was 16.5 mag/arcsec2, a luminance approximately 10600% brighter than that observed for dark nights at the dark-sky park in Hungary.
The measuring station was located in Reykjavik (Additional file 1).
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Two of the flow measuring stations were designed with a β value of 0.405 and 0.418.
Likewise, if the distance of two buildings to the measuring station is similar, the bedrock energy loss is deemed to be comparable.
In order to assess the equivalent-linear model for seismic wave propagation, a comparison between the actual and computed ground shaking of a nearby measuring station is conducted.
(2) In-plane acceleration time history of ground motion that exhibits highest peak ground acceleration (PGA) at a measuring station is used in the analysis.
To minimize the error in the calculation of the correction factors, the air velocities from the two methods at each measuring station were averaged and used for the correction factors analysis.
Altitude of the measuring station is 203 m.
Data from one measuring station were used to estimate exposure for the entire study population in this study, and while inaccurate exposure assignment across the study area can cause a non-differential error, it is unlikely to skew the results, but decreases the statistical power [ 30].
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