Abstract

An understanding of the interactions between climate change and forest structure on tree growth are needed for decision making in forest conservation and management. In this paper, we investigated the relative contribution of tree features and stand structure on Atlas cedar (Cedrus atlantica) radial growth in forests that have experienced heavy grazing and logging in the past. Dendrochronological methods were applied to quantify patterns in basal-area increment and drought sensitivity of Atlas cedar in the Middle Atlas, northern Morocco. We estimated the tree-to-tree competition intensity and quantified the structure in Atlas cedar stands with contrasting tree density, age, and decline symptoms. The relative contribution of tree age and size and stand structure to Atlas cedar growth decline was estimated by variance partitioning using partial-redundancy analyses. Recurrent drought events and temperature increases have been identified from local climate records since the 1970s. We detected consistent growth declines and increased drought sensitivity in Atlas cedar across all sites since the early 1980s. Specifically, we determined that previous growth rates and tree age were the strongest tree features, while Quercus rotundifolia basal area was the strongest stand structure measure related to Atlas cedar decline. As a result, we suggest that Atlas cedar forests that have experienced severe drought in combination with grazing and logging may be in the process of shifting dominance toward more drought-tolerant species such as Q. rotundifolia.

Highlights

  • Climate-related tree decline and mortality is a recurrent phenomenon that has been reported in a variety of forest communities around the world [1,2,3,4,5]

  • Many factors may be involved in the Atlas cedar dieback, in the present study we focus on temperature and precipitation trends, and extreme drought events and stand-structure features

  • Cedar and stumps neighborhoods and competition index were not significant. Both tree age and mean 20th century basal area increments (BAI) showed a highly significant effect when they were included in the model, which indicates that old trees and trees with low mean growth rate had the maximum likelihood of decline

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Summary

Introduction

Climate-related tree decline and mortality is a recurrent phenomenon that has been reported in a variety of forest communities around the world [1,2,3,4,5]. Duration, and severity of drought and heat stress associated with climate change could substantially alter the composition, structure, and biogeography of forests in many regions [11,12]. Land-cover changes greatly influence surface energy balances and climate [20,21]. Variations in surface-radiation regimes and convective heat, derived from drought-induced tree decline and mortality, can considerably influence local, regional, and global climatic conditions [22].

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