Study on variability in certain meteorological parameters in Cuddalore district, Tamil Nadu State

S. Sivaprakasam, A. Murugappan
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Abstract

The earth climate is generally defined as the average weather over a long period of time. A place or region's climate is determined by both natural and anthropogenic factors. The natural elements include the atmosphere, geosphere, hydrosphere, and biosphere, while the human factors include land and resource uses. Changes in any of these factors can cause local, regional, or even global changes in the climate. In this paper, climate variability in Cuddalore district has been assessed through trend analysis of selected meteorological parameters. Statistical techniques have been used to detect and assess the climate variability in terms of rainfall and temperature. Cuddalore district is located between 11°11′ N to 12°35′ N latitude and 78°38′E to 80°00′ E longitude. Representative meteorological parameters have been statistically analysed over the Cuddalore district for 102 years (1901 to 2002) to detect temporal shift. The analysis shows mild increasing trend in rainfall and steep increasing trend in temperature in Cuddalore district. This may be attributed to emission of gasses, industrialization, urbanization and land use.
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泰米尔纳德邦Cuddalore地区某些气象参数的变率研究
地球气候通常被定义为在很长一段时间内的平均天气。一个地方或地区的气候是由自然和人为因素共同决定的。自然因素包括大气、地圈、水圈和生物圈,人为因素包括土地和资源利用。这些因素中的任何一个的变化都可能导致局部、区域甚至全球气候的变化。本文通过对选定气象参数的趋势分析,对Cuddalore地区的气候变率进行了评价。统计技术已被用于探测和评估降雨和温度方面的气候变率。Cuddalore地区位于北纬11°11′至12°35′,东经78°38′至80°00′之间。对Cuddalore地区102年(1901 - 2002)的代表性气象参数进行了统计分析,以探测时间变化。分析表明,库达洛尔地区降水呈温和增加趋势,气温呈急剧上升趋势。这可能归因于气体排放、工业化、城市化和土地利用。
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