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In this work, we set the upper boundary height for the IRI-2007 model to be 20,000 km, the maximum value which the IRI-2007 model allows, to include not only the electrons in the ionosphere, but also in the plasmasphere as well.
The arrow and bars in C illustrate the shift in boundary height between high (bottom bar) and low (top bar) go trial probability conditions.
We also compared different models of contextual modulation in which penalty and proactive cuing either modulated the drift rate, onset time, or boundary height of the execution process.
To evaluate these possibilities, we fit four versions of our DPM in which either the drift, onset, onset and drift, or boundary height parameters were left free when fitting the baseline and caution conditions separately.
These results are consistent with previous studies implicating SMA and preSMA in uncertainty-related and conflict-related modulation of boundary height in the traditional drift-diffusion model, achieved through connections with the striatum and subthalamic nucleus (STN) (Forstmann et al., 2010; Frank et al., 2015; Jahfari et al., 2012).
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It is perhaps worth noting that the actual boundary heights change with location and season, and the mesopause height may be nearer 100 km at mid-latitudes in winter (e.g., Fan et al. 2014).
This is because conditions with lower boundary heights (i.e., greater certainty of a go-trial), allow less time for the process to be active and a shorter distance to travel and thus predict lower levels of summed activity.
These measurements were performed in the Virginia Tech Anechoic Wall Jet Facility for step heights that ranged from approximately 10percentto100percentcent of the incoming boundary layer height.
The recycling technique is utilized to control the mean-velocity profile and boundary layer height.
Rather, it is implied that changes in the mixed boundary layer height resulted in higher night- than daytime concentrations at the urban and coastal sites.
The abnormal weak positive or strong negative AOD PM2.5 associations result from the relatively small portion of anthropogenic aerosols and the changing atmospheric boundary layer height.
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