Comparison of the calculated frost event return period based on copula models under climate change: a case study of Chadegan region in Isfahan province- Iran

IF 2.8 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
Elham Mazaheri, Jahangir Abedi Koupai, Manouchehr Heidarpour, Mohammad Javad Zareian, Alireza Gohari
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Abstract

Spring frost, is one of the important phenomena that damage agricultural production in cold areas. Predicting the occurrence of frost events can be valuable for managing and mitigating frost risk in orchards. In this study, copula models were applied to calculate the joint bivariate return period of frost event in both historical (1984–2014) and future (2023–2053) periods in Chadegan’s almond orchard. For the future period, a combination of 10 general circulation models (GCMs) from Coupled Model Intercomparison Project phase 6 (CMIP6) under three Shared Socioeconomic Pathway scenarios (SSPs) SSP1-2.6, SSP2-4.5 and SSP5-8.8 was employed using a weighting approach. The results indicated that the Generalized Pareto (GP) and Inverse Gaussian were the best marginal distribution functions of the severity (S) and duration (D), respectively. The Frank copula best explained the relationship between severity and duration of frost event. According to the joint bivariate return period of frost event, the extreme frost occurred more frequently in the future period under three SSPs compared to the historical period. In both historical and future periods, in “AND” mode, the frost event with S ≥ 6 ̊C and D ≥ 4 ̊C days, would be more likely to return in 64.71 years and about 14 years, respectively. In "OR" mode, the joint bivariate return period of mentioned frost event increase slightly in future period (3 years for SSPs) compared to the historical (1.54 years). This probabilistic assessment was pointed as a strong toll for predicting the return period of frost event in Chadegan.

Abstract Image

基于共轭模型计算的气候变化下霜冻事件重现期的比较:伊朗伊斯法罕省 Chadegan 地区的案例研究
春季霜冻是损害寒冷地区农业生产的重要现象之一。预测霜冻事件的发生对于管理和降低果园霜冻风险具有重要价值。本研究采用 copula 模型计算了 Chadegan 杏仁园历史时期(1984-2014 年)和未来时期(2023-2053 年)霜冻事件的联合双变量回归期。对于未来时期,采用加权法将耦合模式相互比较项目第 6 阶段(CMIP6)中的 10 个大气环流模式(GCMs)在三种共享社会经济路径(SSPs)SSP1-2.6、SSP2-4.5 和 SSP5-8.8 情景下进行组合。结果表明,广义帕累托(GP)和反高斯分别是严重程度(S)和持续时间(D)的最佳边际分布函数。弗兰克协方差最能解释霜冻事件的严重程度和持续时间之间的关系。根据霜冻事件的联合双变量回归期,与历史时期相比,三种 SSP 条件下未来时期极端霜冻发生的频率更高。无论是历史时期还是未来时期,在 "和 "模式下,S ≥ 6 ̊C 和 D ≥ 4 ̊C 天的霜冻事件分别在 64.71 年和 14 年左右更有可能再次发生。在 "OR "模式下,所述霜冻事件的联合双变量回归期在未来时期(SSPs 为 3 年)比历史时期(1.54 年)略有增加。这种概率评估被认为是预测 Chadegan 霜冻事件重现期的有力工具。
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来源期刊
Theoretical and Applied Climatology
Theoretical and Applied Climatology 地学-气象与大气科学
CiteScore
6.00
自引率
11.80%
发文量
376
审稿时长
4.3 months
期刊介绍: Theoretical and Applied Climatology covers the following topics: - climate modeling, climatic changes and climate forecasting, micro- to mesoclimate, applied meteorology as in agro- and forestmeteorology, biometeorology, building meteorology and atmospheric radiation problems as they relate to the biosphere - effects of anthropogenic and natural aerosols or gaseous trace constituents - hardware and software elements of meteorological measurements, including techniques of remote sensing
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