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Analysis and Application of Drought Characteristics Based on Theory of Runs and Copulas in Yunnan Southwest China

机译:基于游动和Copulas理论的云南干旱特征分析与应用

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摘要

Drought is a complex natural disaster phenomenon. It is of great significance to analyze the occurrence and development of drought events for drought prevention. In this study, two drought characteristic variables (the drought duration and severity) were extracted by using the Theory of Runs based on four drought indexes (i.e., the percentage of precipitation anomaly, the standardized precipitation index, the standardized precipitation evapotranspiration index and the improved comprehensive meteorological drought index). The joint distribution model of drought characteristic variables was built based on four types of Archimedean copulas. The joint cumulative probability and the joint return period of drought events were analyzed and the relationship between the drought characteristics and the actual crop drought reduction area was also studied. The results showed that: (1) The area of the slight drought and the extreme drought were both the zonal increasing distribution from northeast to southwest in Yunnan Province from 1960 to 2015. The area of the high frequency middle drought was mainly distributed in Huize and Zhanyi in Northeast Yunnan, Kunming in Central Yunnan and some areas of Southwest Yunnan, whereas the severe drought was mainly occurred in Deqin, Gongshan and Zhongdian in Northwest Yunnan; (2) The drought duration and severity were fitted the Weibull and Gamma distribution, respectively and the Frank copula function was the optimal joint distribution function. The Drought events were mostly short duration and high severity, long duration and low severity and short duration and low severity. The joint cumulative probability and joint return period were increased with the increase of drought duration and severity; (3) The error range between the theoretical return period and the actual was 0.1–0.4 a. The year of the agricultural disaster can be accurately reflected by the combined return period in Yunnan Province. The research can provide guidelines for the agricultural management in the drought area.
机译:干旱是一种复杂的自然灾害现象。分析干旱事件的发生和发展对预防干旱具有重要意义。在这项研究中,使用运行理论基于四个干旱指数(降水异常百分比,标准化降水指数,标准化降水蒸散指数和改进的干旱指数)提取了两个干旱特征变量(干旱持续时间和严重程度)综合气象干旱指数)。基于四种阿基米德系系建立了干旱特征变量联合分布模型。分析了干旱事件的联合累积概率和联合回归期,研究了干旱特征与作物实际减旱面积之间的关系。结果表明:(1)1960-2015年云南省从东北向西南呈轻度干旱和极度干旱的区域性递增分布。高频中部干旱主要分布在会泽和云南东北的沾益,云南中部的昆明和云南西南的一些地区,而严重的干旱主要发生在云南的德钦,贡山和中甸。 (2)干旱持续时间和严重程度分别符合Weibull和Gamma分布,Frank copula函数是最佳的联合分布函数。干旱事件主要是持续时间短和严重程度高,持续时间长和严重程度低以及持续时间短和严重程度低。联合累积概率和联合回归期随干旱持续时间和严重程度的增加而增加; (3)理论返回期与实际返回值之间的误差范围为0.1–0.4 a。农业灾害年份可以通过云南省的综合归还期准确反映。该研究可为干旱地区的农业管理提供指导。

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