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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

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