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首页> 外文期刊>Journal of hydrometeorology >Evaluation of a Two-Source Snow-Vegetation Energy Balance Model for Estimating Surface Energy Fluxes in a Rangeland Ecosystem
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Evaluation of a Two-Source Snow-Vegetation Energy Balance Model for Estimating Surface Energy Fluxes in a Rangeland Ecosystem

机译:评估牧场生态系统中表面能通量的两源雪植被能量平衡模型的评估

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The utility of a snow-vegetation energy balance model for estimating surface energy fluxes is evaluatedwith field measurements at two sites in a rangeland ecosystem in southwestern Idaho during the winter of 2007: one site dominated by aspen vegetation and the other by sagebrush. Model parameterizations are adopted from the twosource energy balance (TSEB)modeling scheme, which estimates fluxes from the vegetation and surface substrate separately using remotely sensed measurements of land surface temperature. Modifications include development of routines to account for surface snowmelt energy flux and snow masking of vegetation. Comparisons between modeled and measured surface energy fluxes of net radiation and turbulent heat showed reasonable agreement when consideringmeasurement uncertainties in snow environments and the simplified algorithm used for the snow surface heat flux, particularly on a daily basis. There was generally better performance over the aspen field site, likely due to more reliable input data of snow depth/snow cover. The model was robust in capturing the evolution of surface energy fluxes during melt periods. The model behavior was also consistent with previous studies that indicate the occurrence of upward sensible heat fluxes during daytime owing to solar heating of vegetation limbs and branches, which often exceeds the downward sensible heat flux driving the snowmelt. However, model simulations over aspen trees showed that the upward sensible heat flux could be reversed for a lower canopy fraction owing to the dominance of downward sensible heat flux over snow. This indicates that reliable vegetation or snow cover fraction inputs to the model are needed for estimating fluxes over snow-covered landscapes.
机译:在2007年冬季,通过对爱达荷州西南部牧场生态系统中的两个地点进行实地测量,评估了雪-植被能量平衡模型用于估算表面能通量的效用:一个地点由白杨植被主导,另一个由鼠尾草为主。从两源能量平衡(TSEB)建模方案中采用模型参数化,该方案使用遥感的地面温度测量值分别估算来自植被和表层基质的通量。修改内容包括开发例程以解决表面融雪能量通量和植被的雪掩蔽问题。考虑到雪环境中的测量不确定性以及用于雪表面热通量的简化算法(尤其是每天)时,对模型辐射和湍流热的表面能通量的建模和测量值的比较显示出合理的一致性。通常,白杨野外站点的性能更好,这可能是由于雪深/积雪的输入数据更可靠。该模型在捕获融化期间表面能通量的演变方面非常强大。该模型的行为也与先前的研究一致,后者表明白天由于植被的四肢和树枝的太阳加热而出现了向上感热通量,该通量经常超过驱动融雪的向下感热通量。但是,在白杨树上进行的模型仿真表明,由于在雪上向下感热通量占主导地位,因此对于较低的冠层分数,可以将向上感热通量反转。这表明模型需要可靠的植被或积雪分数输入来估算积雪景观的通量。

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