Decadal Dynamics of Energy Balance and Transpiration Fraction in an Alpine Ecosystem: A Modelling and Observational Study

环境科学 能量平衡 蒸腾作用 生态系统 观察研究 水平衡 大气科学 可预测性 气候学 生态学 地质学 光合作用 统计 数学 植物 岩土工程 生物
作者
Yao Wu,Pei Wang
出处
期刊:Ecohydrology [Wiley]
卷期号:18 (2)
标识
DOI:10.1002/eco.70029
摘要

ABSTRACT 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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