Abstract

BackgroundMost North American temperate forests are plantation or regrowth forests, which are actively managed. These forests are in different stages of their growth cycles and their ability to sequester atmospheric carbon is affected by extreme weather events. In this study, the impact of heat and drought events on carbon sequestration in an age-sequence (80, 45, and 17 years as of 2019) of eastern white pine (Pinus strobus L.) forests in southern Ontario, Canada was examined using eddy covariance flux measurements from 2003 to 2019.ResultsOver the 17-year study period, the mean annual values of net ecosystem productivity (NEP) were 180 ± 96, 538 ± 177 and 64 ± 165 g C m–2 yr–1 in the 80-, 45- and 17-year-old stands, respectively, with the highest annual carbon sequestration rate observed in the 45-year-old stand. We found that air temperature (Ta) was the dominant control on NEP in all three different-aged stands and drought, which was a limiting factor for both gross ecosystem productivity (GEP) and ecosystems respiration (RE), had a smaller impact on NEP. However, the simultaneous occurrence of heat and drought events during the early growing seasons or over the consecutive years had a significant negative impact on annual NEP in all three forests. We observed a similar trend of NEP decline in all three stands over three consecutive years that experienced extreme weather events, with 2016 being a hot and dry, 2017 being a dry, and 2018 being a hot year. The youngest stand became a net source of carbon for all three of these years and the oldest stand became a small source of carbon for the first time in 2018 since observations started in 2003. However, in 2019, all three stands reverted to annual net carbon sinks.ConclusionsOur study results indicate that the timing, frequency and concurrent or consecutive occurrence of extreme weather events may have significant implications for carbon sequestration in temperate conifer forests in Eastern North America. This study is one of few globally available to provide long-term observational data on carbon exchanges in different-aged temperate plantation forests. It highlights interannual variability in carbon fluxes and enhances our understanding of the responses of these forest ecosystems to extreme weather events. Study results will help in developing climate resilient and sustainable forestry practices to offset atmospheric greenhouse gas emissions and improving simulation of carbon exchange processes in terrestrial ecosystem models.

Highlights

  • Most North American temperate forests are plantation or regrowth forests, which are actively man‐ aged

  • While the decline in net ecosystem productivity (NEP) at the two younger stands was caused by decreases in gross ecosystem productivity (GEP) and simultaneous increases in RE, the decline in NEP at the 80-year-old stand was primarily caused by the increase in annual RE from 2016 to 2018

  • When all data were considered, Ta was the dominant control of carbon fluxes at all three sites; when the analysis was conducted using data for hot days only ­(Tmax > 27.5 °C), Relative Extractable Water (REW) became a significant driver of GEP and RE

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Summary

Introduction

Most North American temperate forests are plantation or regrowth forests, which are actively man‐ aged These forests are in different stages of their growth cycles and their ability to sequester atmospheric carbon is affected by extreme weather events. The temperate forests in Eastern North America are dominated by different-aged stands that have been either planted or have naturally regrown since the last major harvests in the nineteenth and twentieth century (OMNRF 1986). Many of these forests have been actively managed to enhance their growth and timber production (Gilliam 2016). Increased carbon uptake due to warmer spring temperatures in 2012 helped in compensating the reduction in carbon sequestration due to summer drought, rapid depletion of soil water content enhanced summer heating through land surface–atmosphere feedbacks (Wolf et al 2016; Pan and Schimel 2016)

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