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Analysis of diurnal surface temperature variations for the assessment of surface urban heat island effect over Indian cities

机译:分析日表面温度变化以评估印度城市的地表热岛效应

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Alterations in the urban surfaces elevate the surface and air temperature in the urban boundary than the surrounding rural area result in urban heat island effect. The present study has been carried out to explore the urban heat island effect for the two-time-frame i.e. day time and night time using remote sensing data from Moderate-Resolution Imaging Spectroradiometer (MODIS) sensor of two Indian cities, Ahmedabad and Jaipur. Land surface temperature is used as the key parameter for surface urban heat island studies in the present study. Inverse or negative surface urban heat island effect has been observed over Jaipur whereas moderate or very weak surface urban heat island effect is observed over Ahmedabad during the daytime, whereas strong surface urban heat island effect is observed during night time over both cities. The study indicates that the higher temperature has been observed during the daytime, but the phenomenon of urban heat island is prevalent only during night time. The contrast diurnal land surface temperature variations over these cities have been analyzed in the current study. To support this remote sensing analysis, in-situ surface temperature measurement study has been conducted on various surfaces (anthropogenic and natural) at Jaipur for 24 h temperature monitoring. The study illustrates that soil has a property of rapidly heating up as well as cooling down than the anthropogenic materials like road and concrete observed under this in-situ temperature measurement. Thermal characteristics of various surface materials influence the diurnal behavior of land surface temperature. The study shows that vegetation cover has the lowest temperature during the entire duration of observation. Time of observation is very important for analyzing the efficacy of remote sensing data for surface temperature variations for different land covers and surface urban heat island studies. Urban heat island varies during the day, and it is more significant during the eveningight. In general, heat island phenomenon is apparent at nighttime. (C) 2017 Elsevier B.V. All rights reserved.
机译:与周围农村地区相比,城市表面的变化使城市边界的地表温度和空气温度升高,从而导致城市热岛效应。本研究已经进行了探索,使用了来自印度两个城市艾哈迈达巴德和斋浦尔的中分辨率成像光谱仪(MODIS)传感器的遥感数据,研究了两个时间段(即白天和晚上)的城市热岛效应。在本研究中,地表温度被用作地表城市热岛研究的关键参数。在斋浦尔,观测到的地表城市热岛效应为负或负,而白天在艾哈迈达巴德观测到的地表城市热岛效应为中度或极弱,而在这两个城市的夜间观测到的地表城市热岛效应强。研究表明,白天白天观测到的温度较高,但城市热岛现象仅在夜间普遍存在。在当前的研究中已经分析了这些城市的对比昼夜地表温度变化。为了支持这种遥感分析,已经在斋浦尔对各种表面(人为和天然)进行了原位表面温度测量研究,以进行24小时温度监测。研究表明,与在这种现场温度测量下观察到的人为材料(如道路和混凝土)相比,土壤具有快速加热和冷却的特性。各种地表材料的热特性影响着地表温度的日变化。研究表明,在整个观测期间,植被覆盖的温度最低。观察时间对于分析遥感数据对不同土地覆盖和地表城市热岛研究的地表温度变化的有效性非常重要。城市热岛在白天会有所不同,而在傍晚/夜晚则更为重要。通常,在夜间会出现热岛现象。 (C)2017 Elsevier B.V.保留所有权利。

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