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Dissertation - HQ

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Oriented swimming and passive advection 157<br />

and those initial dispersal routes are therefore ignored in the present<br />

temperature situation while they become available after the 2ºC increase.<br />

And some of them are optimal, hence chosen. In those trajectories, the<br />

maximum distance from the release point is greater than along all<br />

others, thereby increasing the mean distance at the population level. In<br />

addition, a closer look at the promontory case for example (Figure 6.20),<br />

shows that, for some trajectories, the maximum distance from the release<br />

point does not change, yet the shapes of optimal trajectories change<br />

within this range. In particular, some larvae spend more time far from<br />

the release site after the 2ºC increase (inset in Figure 6.20). This increases<br />

the mean distance from the release point along such trajectories. Both<br />

effects (increased maximum distance in some trajectories and increased<br />

mean distance in others) contribute to the unexpected result that mean<br />

distance from the release point at population level is larger after a 2ºC<br />

increase in temperature, even though self-recruitment rate is higher.<br />

Constant maximum<br />

but increased mean<br />

Figure 6.20 Comparison between five trajectories of P. amboinensis in the present<br />

situation (top) and after a 2ºC increase in water temperature (bottom), in the<br />

promontory case. In the climate change scenario, larvae spend more time farther<br />

down in the lee of the promontory than in present conditions. One trajectory<br />

is highlighted in the main figure and presented alone in the insert to highlight<br />

this fact more clearly.

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