Three assimilation variables are also tested in our analysis: temporal duration, age at migration, and acculturation.
Four assimilation scenarios corresponding to different potential field applications were tested.
The results show that there are significant differences in soil moisture variations and streamflow estimates when the three assimilation approaches were applied.
In the tessellation models, trees that are underneath the influence functions of other trees have zero assimilation, and do not participate in the displacements unless movement of their competitors changes their circumstances.
2.4. Figure 6 shows the results of three assimilation experiments following the final assimilation step at t = 360 days.
4. Step 3 is repeated at t = 60, 120, 180, 240, 300, and 360 days, for a total of seven assimilation steps and six forecast cycles.
Furthermore, the AMOC in the three assimilation runs are similar (pairwise correlations are 0.7 or higher) and compare reasonably well with RAPID observations [ Hermanson et al., 2014].
Specifically, the predicted order of discriminability associated with these three assimilation patterns, which we will refer to as cross-language mappings in this article, would be TC > CG > SC (Best, 1995; Best et al., 2001).
We investigate the role of ocean dynamics and its predictability by assessing predictions against the ocean analysis used for initialization for temperature or density and against the average of the three assimilation integrations for heat convergence.
