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Spatial-temporal patterns of urban anthropogenic heat discharge in Fuzhou, China, observed from sensible heat flux using Landsat TM/ETM+ data

机译:使用Landsat TM / ETM +数据从感热通量观察的中国福州城市人为热排放的时空格局

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摘要

The urban heat island (UHI) effect is the phenomenon of increased surface temperatures in urban environments compared to their surroundings. It is linked to decreased vegetation cover, high proportions of artificial impervious surfaces, and high proportions of anthropogenic heat discharge. We evaluated the surface heat balance to clarify the contribution of anthropogenic heat discharges into the urban thermal environment. We used a heat balance model and satellite images (Landsat Thematic Mapper (TM) and Enhanced Thematic Mapper Plus (ETM+) images acquired in 1989 and 2001), together with meteorological station data to assess the urban thermal environment in the city of Fuzhou, China. The objective of this study was to estimate the anthropogenic heat discharge in the form of sensible heat flux in complex urban environments. In order to increase the accuracy of the anthropogenic heat flux analysis, the sub-pixel fractional vegetation cover (FVC) was calculated by linear spectral unmixing. The results were then used to estimate latent heat flux in urban areas and to separate anthropogenic heat discharge from heat radiation due to insolation. Spatial and temporal distributions of anthropogenic heat flux were analysed as a function of land-cover type, percentage of impervious surface area, and FVC. The accuracy of heat fluxes was assessed using the ratios of sensible heat flux (H), latent heat flux (L), and ground heat flux (G) to net radiation (R ), which were compared to the results from other studies. It is apparent that the contribution of anthropogenic heat is smaller in suburban areas and larger in high-density urban areas. However, seasonal disparities of anthropogenic heat discharge are small, and the variance of anthropogenic heat discharge is influenced by urban expansion, land-cover change, and increasing energy consumption. The results suggest that anthropogenic heat release probably plays a significant role in the UHI effect, and must be considered in urban climate change adaptation strategies. Remote sensing can play a role in mapping the spatial and temporal patterns of UHIs and can differentiate the anthropogenic heat from the solar radiative fluxes. The findings presented here have important implications for urban development planning.
机译:与城市环境相比,城市热岛(UHI)效应是城市环境中地表温度升高的现象。它与植被覆盖率降低,人造不透水表面比例高以及人为热量排放比例高有关。我们评估了地表热量平衡,以澄清人为热量排放对城市热环境的贡献。我们使用了热平衡模型和卫星图像(分别在1989年和2001年获得的Landsat Thematic Mapper(TM)和Enhanced Thematic Mapper Plus(ETM +)图像)以及气象站数据来评估中国福州的城市热环境。 。这项研究的目的是估计在复杂的城市环境中以显热通量形式的人为热量排放。为了提高人为热通量分析的准确性,通过线性光谱分解来计算亚像素分数植被覆盖度(FVC)。然后将结果用于估算城市地区的潜热通量,并将人为的热量排放与日照引起的热辐射分开。分析了人为热通量的时空分布与土地覆盖类型,不透水面积百分比和FVC的关系。使用显热通量(H),潜热通量(L)和地面热通量(G)与净辐射(R)之比来评估热通量的准确性,并与其他研究的结果进行比较。显然,在郊区,人为热量的贡献较小,而在高密度城市地区,人为热量的贡献较大。但是,人为排放的季节性差异很小,人为排放的差异受城市扩张,土地覆盖变化和能源消耗增加的影响。结果表明,人为热量释放可能在超高热效应中起重要作用,并且必须在城市气候变化适应策略中予以考虑。遥感可以在绘制UHI的时空格局中发挥作用,并可以将人为热量与太阳辐射通量区分开。本文介绍的发现对城市发展规划具有重要意义。

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