Surface energy fluxes in a drip-irrigated agroecosystem: Unique advection effect of oasis

IF 5.6 1区 农林科学 Q1 AGRONOMY Agricultural and Forest Meteorology Pub Date : 2024-08-29 DOI:10.1016/j.agrformet.2024.110204
Haichao Yu , Tianyi Yang , Sien Li , Shaozhong Kang , Taisheng Du , Yuexin Wang , Haochong Chen , Hui Guo
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Abstract

Surface energy fluxes, mainly encompassing the net radiation (Rn), latent heat flux (LE), sensible heat flux (Hs), and soil heat flux (Gs), play an important role in the land-atmosphere interactions. However, almost all sites face the problem of energy imbalance, and advection fluxes associated with large inhomogeneous surfaces have been ignored, especially in arid oasis areas. In this study, a three-year continuous measurement of energy fluxes with an eddy covariance system was conducted in a drip-irrigated oasis agroecosystem in Northwest China. Reanalysis data including air temperature (Ta), soil moisture (θ), and leaf area index (LAI) in our cropland and surrounding deserts were also collected. The results showed that multi-year mean turbulent fluxes (LE+Hs) accounted for 75 ± 8 % (mean ± standard deviation) of available energy (RnGs). To be precise, LE took up 72 ± 10 % of available energy, and 7.8 ± 2.8 % of it was induced by higher sensible heat advection, proving a pronounced advection effect in this study. When advection was present, most likely during the heading stage, the threshold value for the Priestley–Taylor parameter α, an indicator to reflect the advection effect, fell in the range of 0.88–1.34. Additionally, after a significant irrigation event, α showed a good linear relationship with differences in air temperature (ΔTa), soil moisture (Δθ), and leaf area index (ΔLAI) between our cropland and surrounding deserts. It's worth mentioning that Δθ was the most significant factor, showing a negative correlation with the advection effect. This study has deepened our understanding of the energy balance in oasis agriculture, emphasizing that the advection effect should not be overlooked.

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滴灌农业生态系统的地表能量通量:绿洲的独特平流效应
地表能量通量主要包括净辐射(Rn)、潜热通量(LE)、显热通量(Hs)和土壤热通量(Gs),在陆地-大气相互作用中发挥着重要作用。然而,几乎所有地点都面临着能量不平衡的问题,与大面积不均匀表面相关的平流通量一直被忽视,尤其是在干旱的绿洲地区。本研究利用涡度协方差系统对中国西北地区滴灌绿洲农业生态系统的能量通量进行了为期三年的连续测量。同时还收集了耕地和周边沙漠的气温(Ta)、土壤水分(θ)和叶面积指数(LAI)等再分析数据。结果表明,多年平均湍流通量(LE+Hs)占可用能量(Rn-Gs)的 75 ± 8 %(平均值 ± 标准偏差)。准确地说,LE 占可用能量的 72 ± 10 %,其中 7.8 ± 2.8 % 是由较高的显热平流引起的,这证明了本研究中存在明显的平流效应。当出现平流时,很可能是在茎秆生长阶段,反映平流效应的指标普里斯特利-泰勒参数α的临界值在 0.88-1.34 之间。此外,在一次重要的灌溉事件之后,α 与耕地和周围沙漠之间的气温差异(ΔTa)、土壤湿度差异(Δθ)和叶面积指数差异(ΔLAI)呈良好的线性关系。值得一提的是,Δθ 是最重要的因素,与平流效应呈负相关。这项研究加深了我们对绿洲农业能量平衡的理解,强调平流效应不容忽视。
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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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