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Estimating the Urban Heat Island Contribution to Urban and Rural Air Temperature Differences over Complex Terrain: Application to an Arid City

机译:估算复杂地形上城市热岛对城乡气温差的贡献:在干旱城市中的应用

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This study proposes a method for estimating the canopy-layer net urban heat island (UHI) in regions with complex terrain that lack preurban observations. The approach is based on a linear relationship between the urban-rural temperature difference (DELTA T_(u-r)), measured via screen-level air temperature, and the population of the city, which was found to have the highest correlation with observations. The linear relation is extrapolated to zero population to yield the desired preurban value. The difference between the zero population DELTA T_(u-r) and the current one is proposed to represent the net UHI. Given the uncertainties of the population method, the relatively short time period of the temperature record, and possible inhomogeneity in the data, the results should be regarded as a first-order approximation of the net UHI contribution. The UHI was evaluated for an arid city, Beer Sheba, Israel, for the minimum and maximum air temperatures for the summer and the winter. The study region resembles the combined effect of complex terrain (i.e., the concave topography of the city in contrast with the plateau landscape surrounding it), the UHI, and the regional warming trend. The study assumes that the regional warming does not affect theDELTA T_(u-r). The concave topography of the city dominates over the UHI contribution during nighttime, resulting in an average lower minimum temperature in the city relative to the rural area. This difference has decreased considerably during the study period and has even reversed for the summer nights toward the end of the period. The estimated net UHI contribution in Beer Sheba varies between +0.8° and +3.1°c, with the highest values during the night hours. The high positive UHI during the night is in linewith previous studies. The positive UHI in the summer implies further aggravation of heat stress beyond that occurring, and that predicted to increase, over the region.
机译:这项研究提出了一种方法,用于估计缺乏前期观测的复杂地形地区的树冠层净城市热岛(UHI)。该方法基于通过屏幕级气温测量的城乡温差(DELTA T_(u-r))与城市人口之间的线性关系,该城市人口与观测值的相关性最高。将线性关系外推到零总体以产生所需的城市前值。零人口DELTA T_(u-r)与当前人口之间的差被提出来代表净UHI。考虑到总体方法的不确定性,温度记录的相对较短的时间段以及数据中可能的不均匀性,应将结果视为UHI净贡献的一阶近似值。针对干旱的城市,以色列的贝尔谢巴,对UHI进行了夏季和冬季的最低和最高气温评估。研究区域类似于复杂地形(即城市的凹形地形与其周围的高原景观形成对比),UHI和区域变暖趋势的综合影响。研究假设区域变暖不影响ΔT_(u-r)。在夜间,城市的凹形地形主导着UHI的贡献,导致城市的最低最低温度相对于农村地区平均较低。在研究期间,这种差异已经大大减少,甚至在夏夜期间都已逆转,直到研究期末。贝尔谢巴的UHI净贡献估计值在+ 0.8°C和+ 3.1°C之间变化,在夜间最高。夜间的高阳性UHI与以前的研究一致。夏季UHI的正值意味着该地区的热应力将进一步加剧,超过已发生的热应力,并且预计还会增加。

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