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Sensitivity of gross primary production and evapotranspiration to heat and drought stress in a young temperate plantation in northern China

Hongxian Zhao, Zeyuan Zhou, Feng Zhang, Charles P.‐A. Bourque, Xin Jia, Xinhao Li, Peng Liu, Haiqun Yu, Yun Tian, Chuan Jin, Shaorong Hao, Tianshan Zha

2024Forest Ecosystems10 citationsDOIOpen Access PDF

Abstract

Assessing the sensitivities of ecosystem functions to climatic factors is essential to understanding the response of ecosystems to environmental change. Temperate plantation forests contribute to global greening and climate change mitigation, yet little is known as to the sensitivity of gross primary production (GPP) and evapotranspiration (ET) of these forests to heat and drought stress. Based on near-continuous, eddy-covariance and hydrometeorological data from a young temperate plantation forest in Beijing, China (2012–2019), we used a sliding-window-fitting technique to assess the seasonal and interannual variation in ecosystem sensitivity (i.e., calculated slopes, S GPP-Ta , S ET-Ta , S GPP-EF , and S ET-EF ) in GPP and ET to anomalies in air temperature ( T a ) and evaporative fraction (EF). The EF was used here as an indicator of drought. Seasonally, daily S GPP-Ta , S ET-Ta , and S GPP-EF were greatest in summer, reaching maxima of 1.12 ​± ​0.56 ​g ​C·m −2 ·d −1 ⋅°C −1 , 1.36 ​± ​0.56 ​g H 2 O·m −2 ·d −1 ⋅°C −1 , and 0.37 ​± ​0.35 ​g ​C·m −2 ·d −1 , respectively. Evapotranspiration was constrained by drought, especially during the spring-to-summer period, S ET-EF reaching −0.51 ​± ​0.34 ​g H 2 O·m −2 ·d −1 . Variables EF, T a , soil water content (SWC), vapor pressure deficit (VPD), and precipitation (PPT) were the main controls of sensitivity, with S GPP-Ta and S ET-Ta increasing with T a , VPD, and PPT (<50 ​mm·d −1 ) during both spring and autumn. Increased drought stress during summer caused the positive response in GPP and ET to decrease with atmospheric warming. Variable S ET-EF intensified (i.e., became more negative) with decreasing EF and increasing T a . Interannually, annual S GPP-Ta and S ET-Ta were positive, S GPP-EF near-neutral, and S ET-EF negative. Interannual variability in S GPP-Ta , S ET-Ta , S ET-EF , and S GPP-EF was largely due to variations in bulk surface conductance. Our study suggests that the dynamics associated with the sensitivity of ecosystems to changes in climatic factors need to be considered in the management of plantation forests under future global climate change. • We assessed S GPP-Ta , S GPP-EF , S ET-Ta and S ET-EF in a plantation forest over 2012–2019. • EF, T a , SWC, VPD, and PPT mainly controlled seasonal S GPP-Ta , S GPP-EF , S ET-Ta and S ET-EF . • Annual S GPP-Ta and S ET-Ta were positive, S GPP-EF near 0.0 and S ET-EF was negative. • G s promoted S GPP-Ta , S GPP-EF , S ET-Ta and S ET-EF at interannual timescales. • Drought stress had greater negative effect on the plantation forest than heat stress.

Topics & Concepts

Temperate climateEvapotranspirationEnvironmental sciencePrimary productionChinaProduction (economics)Heat stressEcosystemForestryAgroforestryGeographyAtmospheric sciencesEcologyGeologyEconomicsArchaeologyBiologyMacroeconomicsPlant Water Relations and Carbon DynamicsTree-ring climate responsesGreenhouse Technology and Climate Control
Sensitivity of gross primary production and evapotranspiration to heat and drought stress in a young temperate plantation in northern China | Litcius