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Soil NH4-N and NO3-N exhibited high spatial variability in depth and time during the irrigation season with CU values ranging from 23 to 97% and the coefficient of variation ranging from 0.04 to 1.06.
A significant amount of this variability in depth could be explained by illumination from the light of the moon (Fig. 8).
A relatively small proportion of off target capture was observed, and inter-sample variability in depth of coverage for a given locus was small.
While A ρ and l c account for the variability in depth of staining and image size, the third parameter of the correlation function, D, uniquely quantifies the shape of the mass density spatial correlation function.
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However, the validation question analysis did not show a consistently poor VQ; although VQ4 demonstrated a high variability, further in-depth analysis (Table 4) provided an explanation for this finding.
While enormously successful, DE analysis also suffers from systematic noise and sequencing biases, such as sequence quality bias, wrong base calls, variability in sequence depth across the transcriptome, and the coverage depth differences of replicate samples [ 1].
We first evaluated the variability in the depth of coverage of short-insert reads by plotting the cumulative fraction of normalized depth of correctly paired read coverage that covers a given cumulative fraction of genome (Fig. 2).
Table 1 documents the variability in the depth of post-war U.S. recessions.
Complementary ERT data revealed local heterogeneity in the subsurface resistivity, largely related to variability in the depth to salinity along the survey line.
The connectivity variability was also related to variability in sulcal depth but not cortical thickness, positively correlated with the degree of long-range connectivity but negatively correlated with local connectivity.
In areas on the North Slope of Alaska where topography strongly controlled the flow and redistribution of surface water, NDVI change was found to be strongly related to the variability in the depth of the active (thawed) soil layers of tundra [16].
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