Dissertation - HQ
Dissertation - HQ
Dissertation - HQ
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74 Spatial distribution of larvae<br />
Objective analysis<br />
of the flow to reveal<br />
its large scale direction<br />
the displacement occurred along a straight line (which appears as a<br />
safe assumption for a 22 s drift). Then, the drift vector was suppressed<br />
from the velocity measured. Finally, instantaneous measurement were<br />
averaged over the 4 min of recording. As the apparatus tended to drop<br />
some data at depth, in each depth layer the mean was computed only<br />
when more than four individual measurements were available. This<br />
mean speed is used in the following.<br />
Finally, to resolve the general direction of the flow field, CTD and<br />
ADCP data were jointly interpolated through multivariate optimal<br />
statistical interpolation (also called “objective analysis”) 178 . Dynamic<br />
height was computed from CTD data, with a reference layer at 90 m.<br />
This depth was sampled at all stations. At 90 m, the range of variation in<br />
dynamic height between stations was small, around 0.3 dyn cm for all<br />
rotations. In addition, deeper CTD records did not reveal any noteworthy<br />
decline. Hence, 90 m was chosen as reference. CTD and ADCP data<br />
were assessed independently and showed good agreement. Guided<br />
by this agreement and previous studies 178–180 , the cross-correlation<br />
parameter between the stream function and the geostrophic stream<br />
function was set to 0.95, the divergence to total variance ratio to 0.05,<br />
and the noise-to-signal ratio to 0.1. A critical parameter for the analysis<br />
is the characteristic scale of the correlation function. Given the size of<br />
the grid (ca. 10 km) there was no point in trying to resolve the structures<br />
possibly generated by the atoll (size ca. 7-14 km) which are too small.<br />
The characteristic scale was set to 25 km, which satisfied the requirement<br />
of being at least twice the grid size and erased small scale variability<br />
to reveal the global direction of the flow. The final interpolation grid<br />
had square grid cells with 4 km sides and four layers corresponding to<br />
the average depths of each of the four ascending MOCNESS nets (12.5,<br />
37.5, 62.5, and 87.5 m).<br />
4.2.3 Statistical analysis<br />
Explicitly spatial<br />
comparisons<br />
For spatial analysis, the vertical dimension was not considered so, at<br />
each station, the catches for nets 1-4 were pooled together. As the sampling<br />
effort is not the same at all stations, abundances were divided by<br />
volumes filtered to convert them to concentrations. When it was more<br />
appropriate to deal explicitly with counts, concentrations were multiplied<br />
by a constant volume, hence providing abundances which did not<br />
suffer from bias in sampling effort, called “standardised” abundances.<br />
Data was then analysed along two frameworks.<br />
Spatial distributions of different families or ontogenetic stages were<br />
compared two by two with Syrjala’s non-parametric test 181 . The method<br />
tests for a difference between the distributions of two populations and<br />
proceeds as follows. Consider a rectangle containing all K sampling<br />
points, of coordinates (x k , y k ), k = 1, . . . , K. Divide the abundances (d)<br />
of each population (subscripted i) by their total abundance, so that the