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It is difficult to compare the magnitudes (Table 3) directly with each other because all three organizations, and this study, provided different types of magnitude.
Furthermore, historical and instrumental seismicity records prove that the area has produced a number of earthquakes from moderate to large magnitudes (Table 1).
Different seasonal patterns (Fig. 3) and magnitudes (Table 3) of EWUEGPP and EWUENEP and the difference in the relationships between NEE or GPP and ET (Additional file 2: Table S1) across sites indicate differences in trade-off between carbon uptake and water loss by ENFs.
In the remaining 7 sign motifs, the sign of d depends not only on the signs of
Maximum and minimum temperature variabilities also showed statistically significant relationships with DBP, but small parameter estimates indicated associations of negligible magnitudes (Table 1).
Regarding epidermal hydration, however, a dramatically different reality was registered, with a consistent improvement of superficial and deep hydration in both groups, although with different magnitudes (Table 2).
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The number of recorded events decreases with increasing magnitude (Table 4).
The upper bound magnitude, by contrast, fits well the seismic slip required (Earthquake rupture model 1934_H1, maximum magnitude, Table 1).
Generally, the saturation remanence of olivine was stronger than that of plagioclase by ~1 order of magnitude (Table 4).
The affinity of CFT for DAT and NET is of the same order of magnitude (Table 1).
Using its lower bound magnitude, 172 % of afterslip would be required to fully release the seismic moment deficit since 1255 (Earthquake rupture model 1934_H1, minimum magnitude, Table 1).
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CEO of Professional Science Editing for Scientists @ prosciediting.com