Integrating LUCC and forest aging to project and attribute subtropical forest NEP in Zhejiang Province under four SSP-RCP scenarios

IF 5.7 1区 农林科学 Q1 AGRONOMY Agricultural and Forest Meteorology Pub Date : 2025-04-15 Epub Date: 2025-02-27 DOI:10.1016/j.agrformet.2025.110462
Zihao Huang , Xuejian Li , Fangjie Mao , Lei Huang , Yinyin Zhao , Meixuan Song , Jiacong Yu , Huaqiang Du
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Abstract

Net ecosystem productivity (NEP) serves as a key indicator of the ecosystem carbon balance. However, the combined effects of various drivers, particularly land use/cover change (LUCC) and forest aging, on NEP remain uncertain, leading to uncertainties in regional and global future NEP simulations. This study integrated Future Land Uses Simulation (FLUS), System Dynamic (SD), and optimized Integrated Terrestrial Ecosystem Carbon-budget (InTEC) models to account for future LUCC and its induced changes in forest age structure into future forest NEP simulations. Taking the Zhejiang Province as the study area, we applied four SSP-RCP scenarios (i.e., SSP1–2.6, SSP2–4.5, SSP3–7.0, and SSP5–8.5) to simulate its subtropical forest NEP from 1980 to 2100. Our simulations indicate that the forests existing in 2020 will function as a carbon sink from 2020 to 2060 but will transition to a carbon source from 2060 to 2100, primarily due to the gradual aging of existing forests and the combined influences of climate and CO2 changes. Nonetheless, after considering LUCC such as afforestation, the overall cumulative NEP will continue to increase after 2060. By 2100, cumulative forest carbon sinks from 2020 will reach 631.74 Tg C under SSP1–2.6, 681.75 Tg C under SSP2–4.5, 586.41 Tg C under SSP3–7.0, and 601.28 Tg C under SSP5–8.5. Among these contributions, aging forests existing in 2020 with climate and CO2 changes account for 27.04 % to 63.30 % of cumulative NEP. Climate change exerts a negative impact ranging from -47.39 % to -14.39 %, while CO2 fertilization has a positive contribution of 6.31 % to 73.79 %. Regarding LUCC, afforestation/reforestation contributes significantly, accounting for 43.66 % to 53.65 %, whereas deforestation has a negative impact of -22.77 % to -10.49 %. Additionally, continuous regeneration further supports NEP growth, contributing 12.85 % to 34.77 %. Finally, Partial Least Squares Structural Equation Modeling (PLS-SEM) was used to elucidate the interactions between these factors. The analysis revealed that future LUCC has significant positive impacts on forest NEP whereas forest aging has significant negative impacts. These findings are crucial for understanding the future carbon cycle of subtropical forests and informing adaptation strategies in response to global climate change.
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4种SSP-RCP情景下,基于土地利用变化和森林老化的浙江省亚热带森林新能源政策预测与属性
净生态系统生产力(NEP)是生态系统碳平衡的重要指标。然而,各种驱动因素,特别是土地利用/覆盖变化(LUCC)和森林老化对NEP的综合影响仍然不确定,导致区域和全球未来NEP模拟存在不确定性。本研究将未来土地利用模拟(FLUS)、系统动力学(SD)和优化的陆地生态系统碳收支(InTEC)模型整合到未来森林NEP模拟中,以解释未来土地利用变化及其引起的森林年龄结构变化。以浙江省为研究区,采用SSP1-2.6、SSP2-4.5、SSP3-7.0和SSP5-8.5 4种情景,模拟了1980 - 2100年浙江省亚热带森林NEP。我们的模拟表明,2020年存在的森林将在2020年至2060年期间发挥碳汇的作用,但在2060年至2100年期间将转变为碳源,这主要是由于现有森林的逐渐老化以及气候和二氧化碳变化的综合影响。尽管如此,考虑到植树造林等土地利用/土地利用变化,2060年后总体累积NEP将继续增加。到2100年,SSP1-2.6、SSP2-4.5、SSP3-7.0、SSP5-8.5分别为631.74 Tg C、681.75 Tg C、586.41 Tg C和601.28 Tg C。其中,随气候变化和CO2变化的2020年存在的老化森林占累积NEP的27.04% ~ 63.30%。气候变化的负向贡献范围为- 47.39% ~ - 14.39%,而CO2施肥的正向贡献范围为6.31% ~ 73.79%。在土地利用变化方面,造林/再造林贡献显著,占43.66% ~ 53.65%,而森林砍伐的负影响为- 22.77% ~ - 10.49%。此外,持续再生进一步支持新经济政策的增长,贡献12.85%至34.77%。最后,利用偏最小二乘结构方程模型(PLS-SEM)分析了这些因素之间的相互作用。结果表明,未来土地利用变化对森林NEP具有显著的正向影响,而森林老化对森林NEP具有显著的负向影响。这些发现对于了解亚热带森林未来的碳循环和为应对全球气候变化的适应策略提供信息至关重要。
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来源期刊
CiteScore
10.30
自引率
9.70%
发文量
415
审稿时长
69 days
期刊介绍: Agricultural and Forest Meteorology is an international journal for the publication of original articles and reviews on the inter-relationship between meteorology, agriculture, forestry, and natural ecosystems. Emphasis is on basic and applied scientific research relevant to practical problems in the field of plant and soil sciences, ecology and biogeochemistry as affected by weather as well as climate variability and change. Theoretical models should be tested against experimental data. Articles must appeal to an international audience. Special issues devoted to single topics are also published. Typical topics include canopy micrometeorology (e.g. canopy radiation transfer, turbulence near the ground, evapotranspiration, energy balance, fluxes of trace gases), micrometeorological instrumentation (e.g., sensors for trace gases, flux measurement instruments, radiation measurement techniques), aerobiology (e.g. the dispersion of pollen, spores, insects and pesticides), biometeorology (e.g. the effect of weather and climate on plant distribution, crop yield, water-use efficiency, and plant phenology), forest-fire/weather interactions, and feedbacks from vegetation to weather and the climate system.
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