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[极值分布理论在中国广东省低温冷害重现期预测中的应用。]

[Application of extreme value distribution theory in the forecast of chilling return periods of Guangdong Province, China.].

作者信息

Tang Li Sheng, Wang Hua, Liu Wei Qin, Liu Ye

机构信息

Guangdong Climate Center, Guangzhou 510080, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2018 Aug;29(8):2667-2674. doi: 10.13287/j.1001-9332.201808.019.

DOI:10.13287/j.1001-9332.201808.019
PMID:30182607
Abstract

Chilling is the third weather disaster following flood and typhoon in Guangdong Province. Prediction of chilling return period is of practical significance for scientific reduction and protection of disaster. Four models, including Gumbel distribution, Weibull distribution, log-normal distribution and Peasron-III distribution, were applied, based on the chilling index, to fit the probability distribution of chilling extreme calculated by chilling accumulation for 86 weather stations of Guangdong Province from 1961 to 2015 (December to the following February). The optimal models were selected to calculate the chilling extreme value of return periods. Results showed that Pearson-III distribution was the optimal model for 77 out of the 86 weather stations. The log-normal distribution was optimal for eight weather stations and Gumbel distribution was optimal for only one station. Weibull distribution was not suitable for modeling extreme value of Guangdong Province. Different return periods of 10-, 25-, 50- and 100-year were predicted by optimal distribution models respectively, with a relative error less than 6%. Chilling extreme for years presented obviously latitude distribution feature, with more in north side and less in south side, which matched the distributions of the lowest temperature, average temperature and temperature dipping scale during chilling period. Our results are useful for guiding the chilling defense for relevant industries in Guangdong Province.

摘要

低温冷害是广东省继洪涝、台风之后的第三大气象灾害。预测低温冷害的重现期对科学减灾防灾具有重要意义。基于低温冷害指数,应用耿贝尔分布、威布尔分布、对数正态分布和皮尔逊Ⅲ型分布4种模型,对广东省86个气象站1961—2015年(12月至次年2月)的低温冷害累积量计算得到的低温冷害极值概率分布进行拟合。选取最优模型计算不同重现期的低温冷害极值。结果表明,86个气象站中有77个站的最优模型为皮尔逊Ⅲ型分布,8个站的最优模型为对数正态分布,仅1个站的最优模型为耿贝尔分布,威布尔分布不适用于拟合广东省低温冷害极值。采用最优分布模型分别预测了10年、25年、50年和100年一遇的低温冷害极值,相对误差均小于6%。多年低温冷害极值呈现明显的纬向分布特征,北多南少,与低温冷害期间的最低气温、平均气温和降温幅度分布一致。研究结果可为广东省相关行业低温冷害防御提供参考。

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