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In response to the need for predicted chlorophyll concentrations in modeled climate scenarios, Sarmiento et al. [22] predict annual mean log chlorophyll using a linear regression against temperature, salinity, length of the growing season, and the maximum winter mixed layer depth over 33 biogeochemical provinces.
While numerous environmental signals have been examined in modeled microgravity conditions for their effects on bacteria [ 3, 12], few studies have utilized yeast.
In modeled melts, consequently to increasing α, not only Cl increases because of increasing fluid input, but F increases as well because D F mineral / melt decreases with increasing H2O content.
Temporal variability in ENP concentrations can be mainly explained by temporal variability in modeled river water discharge (in the model, higher river water discharge usually causes higher dilution for ENPs from sewage effluent).
However, accuracy in modeled estimates declined overtime which suggested that accounting models should not be used exclusively as long-term population monitoring devices for deer management.
To understand how the physical and surface properties of NPs affect their diffusion in mucus, we have developed a coarse-grained molecular dynamics model to study the diffusion of NPs in modeled mucus layer.
The observed variation in modeled velocity is similar to that in the initial model.
Tropical low cloud feedback, the predominant factor for uncertainty in modeled ECS, diverges both in sign and magnitude among climate models.
The assimilation of SWOT observations computed with this nominal orbit into the hydraulic model leads to a decrease of 59%and66%6% in the mean spatial and temporal RMSE in modeled channel water depth, respectively.
The map generated using the model of recruitment based on the 0.05 m temperature data shows greater topographic variation in modeled black oak seedling recruitment and generally lower recruitment probability, especially at the upper elevations of Teakettle, and higher predicted recruitment in the lower elevation areas surrounding the study area (Figure 7b).
Despite the good agreement between TSEB and METRIC at discrete locations sampled by the flux towers, a spatial intercomparison of gridded model output (i.e., comparing output on a pixel-by-pixel basis) revealed significant discrepancies in modeled turbulent heat flux patterns that were largely correlated with vegetation density.
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