In the 'Des Vieux Arbres' ecological reserve situated within northwestern Q
uebec, 40 band dendrometers were installed on 7 of the major boreal tree sp
ecies. The late Spring-early Summer daily radial activity registered in 199
7 was related to daily weather variables. For each tree species, the daily
mean i) cumulative radial increment and ii) radial activity indexed series
obtained by first-difference standardization were analyzed. The results ind
icate the existence of strong similarities among the 7 species. All showed
strong synchronous fluctuations in radius during late winter and early spri
ng. This period ended with a short but sharp increase in radial increments
that marked the passage of water into the stem. This initial swelling, less
obvious in Pinus species was followed by a prolonged period of little chan
ge in radial activity. Meteorological data indicated that air temperature w
as positively related to stem swelling during the late winter-early spring
period. Both air and soil temperatures became negatively related to radial
expansion once the passage of water has occurred in the stem. Starting in e
arly June, all species registered a sustained increase in radial increments
possibly associated with active cell division. After this, radial expansio
n was negatively related to air temperature and positively to rainfall.