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Urban Heat Island Effect on Coimbatore City: A Study Using Temperature Trend

机译:城市热岛对哥印拜陀市的影响:基于温度趋势的研究

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摘要

The local temperature is one of the major climatic elements to record the changes in the atmospheric environment brought about by industrialization, increasing population and massive urbanization. The present study dealt with the annual and seasonal temperature anomalies and trends for mean maximum and minimum temperatures of the three stations of the Coimbatore, Sulur and Kinattukkadavu for the past three decades and their association with the development through urbanization activities. The annual rise in mean maximum and minimum temperature anomaly is identified in Coimbatore as 0.04° to 0.1°C and 0.02°C to 0.2°C respectively. There was no significant rise in mean maximum and minimum temperature was obtained in both Sulur and Kinattukkadavu. Theprocedure was based on Mann-Kendall test for the trend and the nonparametric Sen's method for the magnitude of the trend. The results indicated significant positive trend in mean maximum and minimum temperature was observed at Coimbatore during post monsoon and monsoon respectively. There was in significant trend of mean maximum and minimum temperature was identified both Sulur and Kinattukkadavu. The urbanization pattern within Coimbatore was reflected by the temperature anomalies and trends of annualmean minimum and temperature of the two stations within the city namely Sulur and Kinattukkadavu. The presence of trend in annual and seasonal mean maximum and maximum temperature series determined by Mann-Kendall Z statistics and Sen's Slope estimatorreflected in temperature variations which were reflected on urban heat island effect (UHIE).
机译:当地温度是记录由工业化,人口增加和大规模城市化带来的大气环境变化的主要气候要素之一。本研究研究了过去三十年中,哥印拜陀,苏鲁尔和基纳图克卡达沃的三个站点的年度和季节温度异常以及平均最高和最低温度的趋势,以及它们与城市化活动与发展的关系。在哥印拜陀,平均最高和最低温度异常的年均上升分别为0.04°至0.1°C和0.02°C至0.2°C。 Sulur和Kinattukkadavu的平均最高和最低温度均无明显升高。该程序基于趋势的Mann-Kendall检验,基于趋势的大小的非参数Sen方法。结果表明,季风爆发后和季风爆发期间,哥印拜陀的平均最高和最低温度有明显的正趋势。 Sulur和Kinattukkadavu的平均最高和最低温度都有明显的趋势。哥印拜陀内的城市化模式反映在苏鲁尔和基纳图卡卡达武两个城市的温度异常和年平均最小值和温度的趋势上。由Mann-Kendall Z统计数据和Sen的斜率估算器确定的年度和季节性平均最高和最高温度序列中存在趋势,反映在温度变化中,反映在城市热岛效应(UHIE)上。

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