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50<br />

3.5. Discussion<br />

Re<strong>la</strong>tionship b<strong>et</strong>ween abundance of porcupines and so<strong>la</strong>r irradiance<br />

We observed a strong <strong>de</strong>cline in abundance of porcupines from 2000 ongoing. Density of<br />

porcupines concomitantly dropped (from ca. 40 to ca. three animaIs per km 2 b<strong>et</strong>ween 2000<br />

and 2006, Y. Lemay UQAR, unpublished data) in other areas of the Parc National <strong>du</strong> Bic<br />

where no captures were performed so that we are confi<strong>de</strong>nt that our study <strong>de</strong>sign is not<br />

responsible for the observed <strong>de</strong>c\ine. As it was hypothesized from Klvana <strong>et</strong> al. (2004),<br />

changes in abundance of porcupines were corre<strong>la</strong>ted to so<strong>la</strong>r irradiance at our study site. Our<br />

first prediction was therefore supported. We now discuss how so<strong>la</strong>r activity could <strong>influence</strong><br />

abundance of porcupines in eastern Québec through cascading effects on winter precipitation,<br />

win ter <strong>sur</strong>vival rates, and predation rates on porcupines.<br />

Re<strong>la</strong>tionship b<strong>et</strong>ween so<strong>la</strong>r irradiance and winter precipitation<br />

We found that high so<strong>la</strong>r activity was associated with low levels of winter precipitation.<br />

Klvana <strong>et</strong> al. (2004) also found a link b<strong>et</strong>ween so<strong>la</strong>r activity and winter precipitation when<br />

analysing weather records for the same area for the 1877-2000 time period. In their study,<br />

both time series showed regu<strong>la</strong>r periodicities, with a <strong>la</strong>g of four to five years b<strong>et</strong>ween the two<br />

cycles. A significant number of studies have found corre<strong>la</strong>tions b<strong>et</strong>ween so<strong>la</strong>r activity and<br />

different m<strong>et</strong>eorological param<strong>et</strong>ers (reviews in Tsiropou<strong>la</strong> 2003, Versteegh 2005). Positive,<br />

negative or non-existent corre<strong>la</strong>tions have been reported b<strong>et</strong>ween local weather and so<strong>la</strong>r<br />

activity. Sorne were direct (e.g. Currie 1993, Lean <strong>et</strong> al. 1995) white others were <strong>de</strong><strong>la</strong>yed<br />

corre<strong>la</strong>tions (e.g. Perry 1994, 2006). Such conflicting evi<strong>de</strong>nce gives a confusing and<br />

contradictory picture of so<strong>la</strong>r <strong>influence</strong>s on the earth 's <strong>climat</strong>e. One reason for this confusion<br />

may be that so<strong>la</strong>r effects on m<strong>et</strong>eorological param<strong>et</strong>ers differ in various geographical regions<br />

and at different time periods. In<strong>de</strong>ed, sorne reversaIs b<strong>et</strong>ween so<strong>la</strong>r activity and weather<br />

variables have been reported in the literature. We found no significant corre<strong>la</strong>tion b<strong>et</strong>ween<br />

so<strong>la</strong>r irradiance, snowfall and spring tempe rature b<strong>et</strong>ween 1998 and 2004 white Klvana <strong>et</strong> al.<br />

(2004) found those series to remain in phase b<strong>et</strong>ween 1877 and 2000. One exp<strong>la</strong>nation may<br />

be that we were faced with a breakdown of the link b<strong>et</strong>ween so<strong>la</strong>r irradiance and sorne local<br />

param<strong>et</strong>ers. Alternatively, the statistical tool we used (i .e. direct corre<strong>la</strong>tions) may have been

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