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Agriculture drought hazard risk assessment in China

机译:中国农业干旱灾害风险评估

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摘要

It is unusual inadequate precipitation that is the main factor leading to agriculture drought. The degree of precipitation deficit, the occurrence frequency and the duration are the main aspects for the quantitative calculation of drought hazard. China is a vast country with the complex and various types of landforms, and is affected by the significant monsoon climate, as result the farming activities are significant different over the country. In order to find out the comprehensively spatial differentiation of agricultural drought in a large area, this paper established a three-dimensional assessment model “I-P-L” for agriculture drought risk, where I,P,L means drought intensity, frequency, and length of duration respectively and drought is defined as the negative precipitation anomaly. daily data (from 1960 to 2009)of 535 meteorological stations in the recent 50 years was chosen for the drought risk calculation according to the water demand during the crop growing season, and the GIS technology was introduced into the risk mapping. The results showed that the Northwest, most of Inner Mongolia and Huang-Huai-Hai regions were of the high drought risk, while Tibet plateau and Sichuan Basin was lower. The agriculture hazard pattern has better tally with the drought centers got by many scholars, and can reflect the spatial differentiation of drought hazard. This paper can provide a scientific approach for the comprehensive hazards risk assessment and visual expression. This also can offer scientific proof to carry out risk evaluation and spatial, temporal pattern analysis on agricultural drought.
机译:罕见的降水不足是导致农业干旱的主要因素。降水亏缺程度,发生频率和持续时间是干旱灾害定量计算的主要方面。中国是一个幅员辽阔,地貌复杂多样的大国,受季风气候的影响,农业活动在全国范围内差异很大。为了找出大面积农业干旱的综合空间分异,本文建立了农业干旱风险的三维评估模型“ IPL”,其中I,P,L表示干旱强度,频率和持续时间。干旱被定义为负降水异常。根据作物生长期的需水量,选取近50年来535个气象台站的每日数据(1960年至2009年)进行干旱风险计算,并将GIS技术引入风险地图。结果表明,西北,内蒙古大部分地区和黄淮海地区干旱风险较高,而西藏高原和四川盆地的干旱风险较低。农业灾害模式与许多学者建立的干旱中心具有较好的一致性,可以反映干旱灾害的空间分异。本文可以为综合危害风险评估和视觉表达提供科学的方法。这也可以为开展农业干旱风险评估和时空格局分析提供科学依据。

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