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Although this latter approach may prove to be informative, we question whether it would reveal large scale processes that seem to be inherent in our system.
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It forms a multidisciplinary framework for interrelating many other geologic disciplines, and thus it provides an integrated understanding of large-scale processes that have shaped the development of our planet.
The evolution of the substorm concept to include phenomena outside the ionosphere began with a paper by Jelly and Brice (1967) which noted that "…auroral precipitation is not a spatially isolated phenomenon, but is intimately connected with large-scale processes that occupy a substantial part of the magnetosphere".
To understand biological diversification, it is important to account for large-scale processes that affect the evolutionary history of groups of co-distributed populations of organisms.
A commercially large-scale process that was designed based on the strategy achieves 12.3% carbon yields at low (9.1 30.0 wt%) concentrations of reactants, and requires an efficient separation system to obtain high recovery of products with low energy requirements.
Considering the relatively small specific surface area of large scale process equipment, it is assumed that only negligible amounts of heating energy are needed during the holding time of the pretreatment, the solid-liquid separation and the recycle of water and acid.
This study has also generated a quick and large scale screening process that could be used for screening microorganisms to check their suitability as CBP agents.
One way is to examine details of the large-scale atmospheric processes that are known to influence climate such as the El Nino Southern Oscillation (ENSO), the Madden-Julian Oscillation (MJO), the Hadley circulation, and the baroclinic circulation of the mid-latitudes.
Consequently, we unveiled both large-scale evolutionary processes that shape the genomes of extant oomycetes as well as the complex evolution trajectories that lead to highly abundant gene families in this important class of pathogens.
In addition, since the rise of process geomorphology, geomorphologists have often assumed that small-scale processes directly cause large-scale, long-term landscape evolution; that for understanding or predicting the large-scale behaviors, the details of the small-scale processes matter; and that large-scale processes do not directly cause behaviors at much smaller scales.
We review the main mechanisms and causes of emulsion formation during fermentation, because a better understanding on the microscale can give insights into how to improve large-scale processes and the process technology options that can address these challenges.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com