In this paper, we did not try to optimize the weights or to regularize the inverse problem but this possibility was left open on both the regional (Process 6.2) and the global scales (Process 8).
First, urbanization is now a global-scale process that affects the sustainability of our planet.
We found that some sense and order could be attained by assuming that PSSR is a global-scale process and that upwelling growth is a local-scale process.
We then hypothesize that the D2D variability is related causally to variability (in space and time) associated with the local-scale process ("'PSSR' = PSS + upwelling growth"), rather than only with the global-scale process.
In the remainder of this section, we describe the basic electrodynamics around sunset ("Electrodynamics around sunset"), mainly to differentiate the PSSR, which is a global-scale process, from upwelling growth, which is a local-scale process.
Irregularities can appear in a specific region or can be created over wide areas by global-scale processes such as magnetic storms.
Nevertheless, our results demonstrate how isotopes influenced by vastly different global-scale processes can be used effectively to track long-distance animal movement.
Combining isotopes influenced by different global-scale processes may allow researchers to link the population dynamics of animals across large geographic ranges.
Depending on the values of both, their coupling can result to enhancing the interface height overshot or increasing the global time scale process.
In this context, it is salient to note that, taken in its entirety, including the provision and purification of reactant feedstreams, on a global scale, the operation of the Haber Process currently consumes 1 2%% of the world's energy demand, e.g. [2, 3].
