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首页> 外文期刊>Present Environment and Sustainable Development >AIR-TEMPERATURE SINGULARITIES AND DIFFERENCES BETWEEN INTRA- AND EXTRA-URBAN WEATHER STATIONS. CASE STUDY: BUCHAREST-FILARET AND BUCHAREST-B?NEASA
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AIR-TEMPERATURE SINGULARITIES AND DIFFERENCES BETWEEN INTRA- AND EXTRA-URBAN WEATHER STATIONS. CASE STUDY: BUCHAREST-FILARET AND BUCHAREST-B?NEASA

机译:空气温度奇异和城市内外天气站之间的差异。案例研究:布加勒斯特 - Filaret和Bucharest-B?NEASA

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It is already a well-known fact that air-temperature is the most important climatic factor of differentiation between intra- and extra-urban areas, mainly due to the characteristics of the underlying active surface. Bucharest town-area is no exception to the rule. Ranking as Romania’s largest city, its air-temperature singularities and differences account for the most important example expressing the role that the artificial ground layer may play in the creation of specific urban climates. The thermal differences as well as singularities between the Bucharest town-area (Bucharest-Filaret) and its surroundings (Bucharest-B?neasa) are analyzed by means of multiple air-temperature parameters: hourly measurements (01, 07, 13 and 19 hrs.), daily, monthly, yearly values of maximum, average and minimum means, over a 30 year period (1981-2010). Besides, the analysis of some air-temperature singularities or records highlight the clear differences of air heating processes, mostly due to the different interaction patterns between solar radiation and the underlying active layer, at local scales. However, in general, although the intra-urban areas should keep warmer in summer and cooler in winter, the cooling effects seem to still remain lower in the city because of the greater artificial heat input that is being added to the built-in environment.
机译:它已经是一个众所周知的事实,空气温度是内部和地区之间分化的最重要气候因素,主要是由于潜在的活性表面的特征。布加勒斯特市区对规则也不例外。作为罗马尼亚最大的城市排名,其空气温度奇点和差异占表达人造地面层可能在特定城市气候的创造中发挥作用的最重要的例子。通过多种空气温度参数分析了布加勒斯特城区(布加勒斯特 - 菲拉特)及其周边环境(Bucharest-B?Neasa)之间的热差异:每小时测量(01,07,13和19小时。),每日,每月,最大值,平均和最低手段的年度价值,超过30年(1981-2010)。此外,对一些空气温度奇异性或记录的分析突出了空气加热过程的明显差异,主要是由于太阳辐射和底层有源层之间的不同相互作用图案,在本地尺度。然而,一般而言,虽然城市内部地区应在夏季和冬季凉爽的凉爽凉爽,但由于正在添加到内置环境中的人工热输入,这座城市的冷却效应似乎仍然较低。

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