Estimation of fluxes determined by SRCas resulted in higher values (around 11% for LE) with respect to EC, similarly to previously published works over homogeneous canopies.
Clearly, a Y (II) close to 0.1 of cells in the newly excised disks (Fig. 3A) was low, but then rose sharply to the highest values (around 0.4) as the chloroplasts aggregated in the center of cells (Fig. 3C).
The bicoherence, shown in Figure 5c shows significant high values around (8, 8).
The relatively conductive portion is also present as relatively high values around sites 03 and 04 within the phase pseudo-section.
SID along the latitudes does not show any trends, but rather wavy patterns, with high values around 42°30′ and 44°, and low points around 43° and 46°30′ in latitude (Fig. 4a).
high values around the buried object location and low values in the rest of the region, immunity to clutter, noise, or weak soil anomaly based signals, broad threshold selection range to mark buried object location without false alarms even in the case of difficult target detection, when a constant threshold is used.
These latitudinal trends were likely driven mostly by the high values around 60° N, i.e. the Northeast Pacific region (also see Figs. 2a and 4a).
In deeper areas, richness, evenness and AvTD showed a general decrease with depth from high values around 301 600 m (400 500 m stratum in Tolimieri [23]), while species density and VarTD peaked and declined at shallower depths, generally around 200 m.
The Strouhal number, St, initially has high values around 1.25 at 1 m/s and decreases asymptotically to values around 0.25 at 7 m/s for both bats (Fig. 5i).
