高寒生态系统能量平衡和蒸腾分数的年代际动态:模拟和观测研究

IF 2.5 3区 环境科学与生态学 Q2 ECOLOGY
Ecohydrology Pub Date : 2025-03-27 DOI:10.1002/eco.70029
Yao Wu, Pei Wang
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引用次数: 0

摘要

蒸散发(Evapotranspiration, ET)是土壤-植物-大气连续体的重要组成部分,对生态系统的水分和能量平衡具有重要影响。然而,现有的ET研究主要集中在生长季节或特定年份,有限的长期分析跨越几十年。本研究旨在分析黑河流域高寒生态系统ET的组成,重点研究植被蒸腾(T)和土壤蒸发(Ev)的动态变化。利用SPAC模式,综合2013 - 2022年气象观测资料和涡旋相关方差资料,研究了太阳辐射和植被动态对ET及其分配的影响。实测和模拟的能量通量(净辐射和潜能通量)与土壤温度之间的一致性强调了模型性能的有效性。此外,利用底层水分利用效率法进行比较,发现生长季节的T/ET值一致,进一步证实了模型的准确性。结果表明:10年研究期间的年平均T/ET为0.41±0.03,接近全球平均值,但低于温暖湿润地区。季节分析表明,T/ET在生长季(4 - 10月)显著增加,特别是在5月和6月,与永久冻土融化和土壤水分增加相一致。此外,研究发现叶面积指数和冠层气孔导度与T/ET呈对数关系,土壤温度和向下长波辐射与T/ET呈指数关系。本研究强调了了解高山生态系统中气孔导度动态及其对蒸腾过程的控制的重要性。通过提供对这些环境的水文过程的关键见解,它为适应气候变化的影响提供了指导。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Decadal Dynamics of Energy Balance and Transpiration Fraction in an Alpine Ecosystem: A Modelling and Observational Study

Evapotranspiration (ET) is a critical component of the soil–plant–atmosphere continuum, significantly influencing the water and energy balance of ecosystems. However, existing studies on ET have primarily focused on the growing season or specific years, with limited long-term analyses spanning decades. This study aims to analyse the components of ET within the alpine ecosystem of the Heihe River Basin, specifically investigating the dynamics of vegetation transpiration (T) and soil evaporation (Ev). Utilizing the SPAC model and integrating meteorological observations and eddy covariance data from 2013 to 2022, we investigate the impact of solar radiation and vegetation dynamics on ET and its partitioning (T/ET). The agreement between measured and simulated energy fluxes (net radiation and latent energy flux) and soil temperature underscores the validity of the model's performance. Additionally, a comparison employing the underlying water use efficiency method reveals consistent T/ET values during the growing season, further confirming the model's accuracy. Results indicate that the annual average T/ET during the 10-year study period is 0.41 ± 0.03, close to the global average but lower than in warmer, humid regions. Seasonal analysis reveals a significant increase in T/ET during the growing season (April to October), particularly in May and June, coinciding with the thawing of permafrost and increased soil moisture. In addition, the study finds that the leaf area index and canopy stomatal conductance exhibit a logarithmic relationship with T/ET, whereas soil temperature and downward longwave radiation show an exponential relationship with T/ET. This study highlights the importance of understanding the stomatal conductance dynamics and their controls of transpiration process within alpine ecosystems. By providing key insights into the hydrological processes of these environments, it offers guidance for adapting to climate change impacts.

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来源期刊
Ecohydrology
Ecohydrology 环境科学-生态学
CiteScore
5.10
自引率
7.70%
发文量
116
审稿时长
24 months
期刊介绍: Ecohydrology is an international journal publishing original scientific and review papers that aim to improve understanding of processes at the interface between ecology and hydrology and associated applications related to environmental management. Ecohydrology seeks to increase interdisciplinary insights by placing particular emphasis on interactions and associated feedbacks in both space and time between ecological systems and the hydrological cycle. Research contributions are solicited from disciplines focusing on the physical, ecological, biological, biogeochemical, geomorphological, drainage basin, mathematical and methodological aspects of ecohydrology. Research in both terrestrial and aquatic systems is of interest provided it explicitly links ecological systems and the hydrologic cycle; research such as aquatic ecological, channel engineering, or ecological or hydrological modelling is less appropriate for the journal unless it specifically addresses the criteria above. Manuscripts describing individual case studies are of interest in cases where broader insights are discussed beyond site- and species-specific results.
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