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From these measurements we calculated the phase-breaking length (Lϕ = 72 nm).
From the hemodynamic measurements, we calculated systemic vascular resistance (SVR) from [ MAP-Rap)/CO)*80].
Through electrophysiological and ultrastructural measurements, we calculated release site probabilities to differ considerably between terminals (0.33 versus 0.11).
On the basis of the measurements, we calculated the theoretical load index by solving the model for inner surface temperature of the building envelope based on the modified radiant heat transfer method.
In order to evaluate the precision of the measurements, we calculated the standard deviation of M s (σ Ms) for |B| > 300 mT. The σ Ms values were calculated to be ~100 pAm2 for all samples.
Based on the continuous PMO concentration measurements, we calculated the daily deposition rate D d using the daily mean concentration and the deposition velocity v D according to (9).
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By upscaling short-term measurements, we calculate that approximately 90 ± 77 Tg CH4 yeand1 and 4540 ± 1480 Tg CO2 yeare1 areleasedsed from tropical wetlands globally.
For the 12-week period before each DAS28 measurement, we calculated the proportion of days of DMARD underuse.
For each measurement, we calculated the trimester and gestational week, based on the participant's last menstrual period.
In the 1st and 2nd cIMT measurement, we calculated an intraobserver variability of 2.5% and 2.1%, respectively.
To determine the benefits of continued screening after a baseline PSA measurement, we calculated the number of men needed to screen and the number of men needed to be diagnosed to prevent one man from developing metastatic disease or dying from prostate cancer by 15 years.
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criteria we calculated
standards we calculated
axis we calculated
requirements we calculated
extent we calculated
size we calculated
measurements we analyzed
measurements we added
measurements we removed
measurements we found
measurements we requested
measurements we tested
measurements we followed
measurements we used
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