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首页> 外文期刊>Atmospheric Measurement Techniques >Infrared and millimetre-wave scintillometry in the suburban environment – Part 2: Large-area sensible and latent heat fluxes
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Infrared and millimetre-wave scintillometry in the suburban environment – Part 2: Large-area sensible and latent heat fluxes

机译:郊区环境中的红外和毫米波闪烁法-第2部分:大面积感热通量和潜热通量

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摘要

A millimetre-wave scintillometer was paired with an infrared scintillometer,enabling estimation of large-area evapotranspiration across northernSwindon, a suburban area in the UK. Both sensible and latent heat fluxes canbe obtained using this "two-wavelength" technique, as it is able to provideboth temperature and humidity structure parameters, offering a majoradvantage over conventional single-wavelength scintillometry. The firstpaper of this two-part series presented the measurement theory andstructure parameters. In this second paper, heat fluxes are obtainedand analysed. These fluxes, estimated using two-wavelength scintillometryover an urban area, are the first of their kind. Source area modellingsuggests the scintillometric fluxes are representative of 5–10 km2. Forcomparison, local-scale (0.05–0.5 km2) fluxes were measured by an eddycovariance station. Similar responses to seasonal changes are evident at thedifferent scales but the energy partitioning varies between source areas.The response to moisture availability is explored using data from 2 consecutive years with contrasting rainfall patterns (2011–2012). Thisextensive data set offers insight into urban surface-atmosphere interactionsand demonstrates the potential for two-wavelength scintillometry to deliverfluxes over mixed land cover, typically representative of an area 1–2 ordersof magnitude greater than for eddy covariance measurements. Fluxes at thisscale are extremely valuable for hydro-meteorological model evaluation andassessment of satellite data products.
机译:将毫米波闪烁仪与红外闪烁仪搭配使用,可以估算出英国郊区史云顿北部的大面积蒸散量。使用这种“双波长”技术可以同时获得显热通量和潜热通量,因为它能够同时提供温度和湿度结构参数,与传统的单波长闪烁法相比具有很大的优势。这个由两部分组成的系列的第一篇文章介绍了测量理论和结构参数。在第二篇论文中,获得了热通量并进行了分析。这些通量是使用双波长闪烁法在市区范围内估算的,是同类产品中的第一个。震源面积建模建议闪烁通量代表5-10 km 2 。为了比较,通过涡度方差站测量了局部尺度(0.05–0.5 km 2 )的通量。在不同尺度上,对季节性变化的响应相似,但在源区之间的能量分配也有所不同。使用连续两年的数据(降雨模式相反)(2011-2012)探索了对水分有效性的响应。这一广泛的数据集提供了对城市地表与大气相互作用的洞察力,并证明了双波长闪烁法在混合土地覆盖物上传递通量的潜力,通常代表比涡旋协方差测量大1-2个数量级的区域。这种规模的通量对于水文气象模型评估和卫星数据产品评估非常有价值。

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