Main environmental driver and seasonality of water use efficiency in tropical forests

IF 6.3 1区 地球科学 Q1 ENGINEERING, CIVIL
Yiyan Zeng , Ya Liu , Pinghua Hong , Panxing He , Jun Ma
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Abstract

This study investigates Water Use Efficiency (WUE) in tropical forests, emphasizing the principal environmental drivers and their seasonal variations. Tropical forests play a pivotal role in global carbon and water cycles; however, the dominant environmental drivers influencing tropical forest WUE and its seasonal differences remain inadequately understood. Using simulations from terrestrial biosphere models covering the period from 1901 to 2010, this research reveals that (i) WUE increased in 98.9 % of tropical forests, with an average increase of 0.318 g C kg H2O–1 over this period, (ii) the average contributions of elevated CO2, climate change, nitrogen deposition, and land cover change to WUE variations in tropical forests were 82.02 %, 5.64 %, 11.64 %, and 0.69 %, respectively, (iii) 83.5 % of tropical forests experienced an increase in WUE of more than 0.1 g C kg H2O–1 per year under the influence of elevated CO2, with a smaller positive contribution from nitrogen deposition, while land cover change and climate change had negative impacts on WUE in 63.8 % and 59.2 % of tropical forests, and (iv) average tropical forest WUE during the dry season was 0.719 g C kg H2O–1 higher than that in the wet season, with the increasing trend of CO2 and the interannual variability of climate change being the primary factors influencing WUE changes at the per-grid level. This study enhances our understanding of the dynamics of carbon and water cycles in tropical forests during periods of varying water availability and provides essential insights for predicting future shifts in tropical forest WUE under global change.
热带森林水分利用效率的主要环境驱动因素和季节性
本研究探讨了热带森林水分利用效率(WUE)的主要环境驱动因素及其季节变化。热带森林在全球碳和水循环中发挥着关键作用;然而,影响热带森林用水效率及其季节差异的主要环境驱动因素仍未得到充分了解。利用1901—2010年陆地生物圈模式的模拟结果表明,热带森林WUE增加了98.9%,平均增加了0.318 g C kg H2O-1; CO2升高、气候变化、氮沉降和土地覆盖变化对热带森林WUE变化的平均贡献分别为82.02%、5.64%、11.64%和0.69%。(iii)在CO2升高的影响下,83.5%的热带森林的WUE每年增加超过0.1 g C kg H2O-1,氮沉降的正贡献较小,而土地覆盖变化和气候变化对63.8%和59.2%的热带森林的WUE有负影响;(iv)旱季热带森林的平均WUE比雨季高0.719 g C kg H2O-1。CO2的增加趋势和气候变化的年际变率是影响用水效率变化的主要因素。该研究增强了我们对不同水分可用性时期热带森林碳和水循环动态的理解,并为预测全球变化下热带森林WUE的未来变化提供了重要见解。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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