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Regional climate change and local urbanization effects on weather variables in Southeast China

机译:中国东南部区域气候变化和局部城市化对天气变量的影响

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This paper presents the analyses of regional climate change features and the local urbanization effects on different weather variables over Southeast China. The weather variables considered are: daily mean (T_m), minimum (T_(min)), and maximum (T_(max)) near surface air temperature, diurnal temperature range (DTR), relative humidity (RH), and precipitation (P). With analysis of two datasets (a station dataset for the period from 1960 to 2005 that is mainly used and a grid dataset for the period 1960-2000), this study reveals that the trends in the variations of these weather variables can be separated into two periods, before and after 1984. Before 1984, there were no significant urbanization effects, and T_(min), RH, and P steadily increased but T_(max) decreased, resulting in a considerable decrease in DTR and a slight decrease in T_m. After 1984, T_(min) and T_(max) increased considerably, and the urbanization influence on T_(m;n), but not T_(max), is observable. The urbanization effect causes an extra increasing trend in T_(min) with a rate of about 0.6°C/decade and, accordingly, extra decreasing trends in DTR and RH. The analysis of the seasonal trends reveals that the urbanization influence results in a near-uniform increase of T_(min) for all four seasons and a strong decrease of RH in summer and autumn. Moreover, there is no significant change in P at the annual scale and an increasing rate of 11.8%/decade in summer. With the urbanization influence, a considerable increase in P is noticeable at the annual scale; specifically, the increasing rates of 18.6%/decade in summer and 13.5%/decade in autumn are observed.
机译:本文分析了中国东南部地区气候变化特征以及当地城市化对不同天气变量的影响。考虑的天气变量为:地表气温附近的每日平均(T_m),最小值(T_(min))和最大值(T_(max)),日温度范围(DTR),相对湿度(RH)和降水(P )。通过分析两个数据集(主要使用1960年至2005年期间的站点数据集和1960-2000年期间的网格数据集),这项研究表明,这些天气变量的变化趋势可以分为两个1984年之前和之后的时期。1984年之前,没有明显的城市化影响,T_(min),RH和P稳定增加,但T_(max)减少,导致DTR显着下降,T_m略有下降。 1984年之后,T_(min)和T_(max)显着增加,并且可以观察到城市化对T_(m; n)的影响,但对T_(max)的影响不明显。城市化效应导致T_(min)的额外增加趋势,约为每10摄氏度0.6°C,因此DTR和RH的额外减少趋势。对季节趋势的分析表明,城市化影响导致所有四个季节的T_(min)几乎均匀增加,而夏季和秋季的RH则大大降低。此外,磷在年尺度上没有显着变化,夏季增长了11.8%/十年。受到城市化的影响,P的年均增长显着。具体而言,夏季增长了18.6%/十年,秋季增长了13.5%/十年。

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