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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Kharif foodgrain yield and daily summer monsoon precipitation over India
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Kharif foodgrain yield and daily summer monsoon precipitation over India

机译:印度哈里夫的粮食产量和夏季夏季季风降水

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摘要

Foodgrain yield over India during kharif (summer) season is directly affected by day to day variations in summer monsoon precipitation (June through September). An increase (decrease) in foodgrain yield is generally associated with an increase (decrease) in rainfall. However, the reduction of rainfall or occurrence of heavy rainfall activity may cause adverse effect on the crop growth. This study is therefore aimed at understanding the impact of all possible values of daily precipitation from lowest to highest rainfall during summer monsoon on kharif foodgrain yield over India for the period 1966-2003. The study also includes an impact of intense rainfall events (1 and 5 days maximum precipitation) on foodgrain yield. Analysis covers frequency of rainy days based on all fixed thresholds (1 mm and above) at the interval of 1 mm as well as percentile thresholds (1st percentile to 99th percentile) at the interval of 1 percentile. The study reveals that the kharif foodgrain yield increases with increase in all-India summer monsoon precipitation and rainy days. Strong positive relationship (statistically significant at 1% level) is observed for lower range of threshold values from 1 to 50 mm (1st percentile to 90th percentile), and the magnitudes of correlation decreases with increase in threshold values. The negative impact of the heavy rainfall activity is more pronounced over the heavy rainfall regions of northeast India. It is found that the prolonged occurrence of intense rainfall activity increases their impact on the foodgrain yield. Normal (moderate) range of precipitation indices is seen to be associated with both positive and negative anomalies of foodgrain yield, which point towards the influence of other climatic factors in determining the better yield of kharif foodgrain.
机译:印度在卡里夫(夏季)季节的粮食产量直接受到夏季季风降水(6月至9月)每天变化的影响。粮食产量的增加(减少)通常与降雨的增加(减少)有关。但是,降雨减少或出现强降雨活动可能会对作物生长造成不利影响。因此,本研究旨在了解夏季季风期间从最低降水到最高降水的每日降水的所有可能值对1966-2003年印度哈里夫粮食产量的影响。该研究还包括强降雨事件(最大降雨1天和5天)对粮食产量的影响。分析基于所有固定阈值(1毫米及以上)(间隔为1毫米)和百分比阈值(第1个百分点至第99个百分点)(间隔为1个百分点)来确定雨天的频率。研究表明,随着全印度夏季季风降水和雨天的增加,哈里夫的粮食产量增加。在1到50 mm的较低阈值范围(从1%到90%)中观察到强正相关关系(在1%的水平上具有统计显着性),并且相关强度随阈值的增加而减小。在印度东北部的强降雨地区,强降雨活动的负面影响更为明显。发现长时间的强降雨活动增加了它们对粮食产量的影响。降水指数的正常(中等)范围被认为与粮食产量的正反相关,这表明其他气候因素对确定更好的哈里夫粮食产量的影响。

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