| 基于条件分布模型的气象水文干旱传递分析 |
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| 引用本文： | 李 敏,张铭锋,朱黎明,黄金柏.基于条件分布模型的气象水文干旱传递分析[J].水文,2023,43(4):39-44. |
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| 作者姓名： | 李 敏 张铭锋 朱黎明 黄金柏 |
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| 作者单位： | 扬州大学水利科学与工程学院,扬州大学水利科学与工程学院,扬州大学水利科学与工程学院,扬州大学水利科学与工程学院 |
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| 基金项目： | 江苏省“双创博士项目”项目(JSSCBS20211029)；江苏省博士后科研资助计划(2020Z223)) |
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| 摘 要： | 气象干旱发展到一定程度可以传递为水文干旱。以潘家口水库流域1961—2010年逐月平均降水数据和潘家口水库的入库径流序列为基础数据，分别计算了1、3、6、12个月时间尺度的标准化降水指数（SPI）和标准化径流指数（SRI），以表征研究区域的气象干旱和水文干旱。基于条件分布模型，分析了不同时间尺度的气象干旱传递到未来的不同等级和不同的预测期（或滞后期）的水文干旱的概率。结果表明，当SPI时间尺度较短或预测期（滞后期）较短时，其对应的SRI水文干旱等级越倾向于维持与SPI相同的干旱等级；随着SPI时间尺度的增长或预测期（滞后期）延长，其对应的SRI水文干旱等级略低于气象干旱或恢复到正常状态。
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| 关 键 词： | 气象干旱 水文干旱 条件分布模型 转换概率 |
| 收稿时间： | 2022/1/31 0:00:00 |
| 修稿时间： | 2022/1/31 0:00:00 |
Analysis of Meteorological and Hydrological Drought Transfer Based on Conditional Distribution Model |
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| LI Min,ZHANG Mingfeng,ZHU LiMing and HUANG Jinbai.Analysis of Meteorological and Hydrological Drought Transfer Based on Conditional Distribution Model[J].Hydrology,2023,43(4):39-44. |
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| Authors: | LI Min ZHANG Mingfeng ZHU LiMing and HUANG Jinbai |
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| Institution: | Yangzhou University,Yangzhou University,Yangzhou University,Yangzhou University |
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| Abstract: | Meteorological drought can be converted to hydrological drought to a certain extent. In this paper, based on the monthly average precipitation data of Panjiakou Reservoir Basin from 1961 to 2010 and the inflow runoff series of Panjiakou Reservoir, the standardized precipitation index ( SPI ) and standardized runoff index ( SRI ) at the time scales of 1,3,6 and 12 months are calculated to characterize the meteorological drought and hydrological drought in the study area. Based on the conditional distribution model, the probability of meteorological drought in different time scales and different prediction periods ( or lag periods ) passing to different levels of hydrological drought in the future is analyzed. The results showed that when the SPI time scale was small or the prediction period ( lag period ) was short, the drought level of the converted SRI was more inclined to maintain the same drought level as that of SPI. With the increase of SPI time scale or the extension of prediction period ( lag period ), the drought level of the converted SRI was slightly lower than that of meteorological drought or returned to normal state. |
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| Keywords: | Meteorological drought Hydrological drought Conditional distribution model Transition probability |
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