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Analyzing Precipitation Using Concentration Indices for North Gujarat Agro Climatic Zone, India

机译:用北古杰拉特农业气候区使用浓度指数分析降水

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The climate of India defies easy generalisation, comprising a wide range of weather conditions across a large geographic extent and varied topography. India's unique geography and geology strongly influence its climate; this is particularly true of the Himalayas in the north and the Thar Desert in the northwest. As in much of the tropics, monsoonal and other weather conditions in India are unstable: major droughts, floods, cyclones and other natural disasters are sporadic, but have killed or displaced millions. India's long-term climatic stability is further threatened by global warming. Climatic diversity in India makes the analysis of these issues complex. Gujarat is divided into eight agroclimatic zones. For the present study north Gujarat agroclimatic zone is considered. The major objectives of present study are to investigate the climate characteristics in the area. For the present study daily precipitation data from 167 raingauge stations for 48 years (1961-2008). The present study methodologically attempts to determine the structure of the accumulated precipitation amounts contributed by the accumulated number of precipitation days using concentration index, COIN, to represent the distribution and intensity of the precipitation. The COIN values are ranging from 0.54 to 0.66 with an average value of 0.60. It can be concluded that a concentration index, defined on the basis of the exponential curves, enables the evaluation of contrast or concentration of the different daily amounts of the precipitation by regionalizing the study area into lower and higher variability.
机译:印度的气候无视泛化,包括跨越地理范围和各种形貌的各种天气条件。印度独特的地理和地质强烈影响其气候;这尤其如此的喜马拉雅山和西北地区的沙漠。与在热带的大部分地区一样,印度的季风和其他天气条件不稳定:主要的干旱,洪水,旋风和其他自然灾害是零星的,但已经杀死或流离失所数百万。全球变暖,印度的长期气候稳定性进一步威胁。印度的气候多样性使得这些问题复杂的分析。古吉拉特分为八个旧货罩区。对于目前的研究,考虑了北古吉拉特省农石素。目前研究的主要目标是调查该地区的气候特征。对于目前的研究来自167个RaInauge站的每日降水数据48年(1961-2008)。本研究的方法论上讲,确定使用浓度指数,硬币累积沉淀天累积数量的累积沉淀量的结构,以代表沉淀的分布和强度。硬币值的范围为0.54至0.66,平均值为0.60。可以得出结论,在指数曲线的基础上定义的浓度指数使得通过将研究区域纳入较低和更高的可变性来评估不同每日沉淀量的对比度或浓度。

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