Abstract

With the current climate changes, it is essential to understand the mechanisms that govern floods and flow regimes and their effects on the dynamics of riparian forests. The aim is to assess the effects of new hydrological conditions (increase in flood frequency) on forest stands subject to frequent floods. The sampling sites (total of 94 quadrats) are located in riverine woodlands, and the choice of location corresponds to the boundaries of the flood-risk zones established by official government maps. Our study shows that there are significant differences in the composition and diversity of forest communities following differences in the flood recurrence zones. In the active floodplains (i.e., recurrence interval of 0–20 years), the tree population stands are clearly distinguished from other intermediate flood zones (interval of 20–100 years). Differences are also noted in the structure of the communities, in particular in the frequent flood zones, which are characterized by a low renewal rate, low density and less-diversified forest stands. The frequent floods risk forest stand rejuvenation and creating decline as a result of increased tree mortality and the low renewal rate. With the expected increases in the number of flood events in the coming decades, there may be greater tree mortality and a gradual disappearance of the forest communities.

Highlights

  • A number of studies have dealt with variations in the water regime and their effects on the composition and vitality of riparian ecosystems [1,2,3]

  • There is a higher number of tree species in the intermediate zones, which act as a transition between the high flood risk zones and no-flood zones

  • This study aims at better understanding the dynamics of forest ecosystems affected by frequent floods that have increased in recent decades in the southern part of Québec

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Summary

Introduction

A number of studies have dealt with variations in the water regime and their effects on the composition and vitality of riparian ecosystems [1,2,3]. It is known that these impacts can vary at the local and regional levels, as well as based on the type of catchment and flow regime [3,4]. The hydroclimatic variations (e.g., river flow, temperature and rainfall) related to global warming could induce major changes in flow regimes and riparian ecosystems [4,5,6]. River regulation has a direct impact on river flow, which in turn can have an adverse effect on the vitality of riparian ecosystems [6,7]. Various authors [9,12,13,14,15]

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