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松花江流域生长季旱涝急转特征

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分析1950-2023年作物生长季松花江流域旱涝急转特征和旱涝急转风险指数的时空变化,结果表明:松花江流域生长季旱转涝的发生频次和影响范围普遍高于涝转旱,二者强度相当.5月和6月是旱涝急转多发期.1990年后旱涝急转频次、强度及风险指数变率较大.旱转涝频次在黑河、嫩江以及吉林东南部较高,强度在松嫩平原东部和大兴安岭较大.1950-2023年松花江流域旱转涝风险指数呈增加趋势,5月和6月贡献较大,尤其是5月北部和东北部及6月中部,7月贡献小.涝转旱频次在三江平原和吉林东南部较高,强度在松嫩平原中部较大.1950-2023年涝转旱风险指数有所上升,但趋势不显著.2000年后旱转涝频次和风险指数的年际变率大,1970年前后以及1995-2010年涝转旱变率大.7月涝转旱风险指数贡献大,5月北部和西部贡献大,6月、7月和9月东部贡献大.降水变率是导致旱涝急转风险指数变化的直接原因.
Characteristics of Drought-flood Abrupt Events During Growing Season in the Songhua River Basin
Drought-flood abrupt event refers to the extreme climatic event in which a region rapidly transitions from a drought to a flood state(or vice versa)within a relatively short period.As a typical compound event,its impact is far greater than that of droughts or floods occurring independently.Such events can significantly impact agricultural production,water resource management,ecological environments,and socio-economic conditions.Characteristics of drought-flood abrupt during crop growing season in the Song-hua River Basin from 1950 to 2023 are investigated,and spatiotemporal changes in the risk index of these transitions are also analyzed,providing a scientific basis for climate change research,water resource plan-ning,and enhancing the ability to cope with extreme climate events.It's found that the frequency and im-pact range of drought-to-flood transitions during the growth season in the Songhua River Basin are general-ly higher than those of flood-to-drought transitions,with the intensity of both being roughly equivalent.May and June are high incidence periods for abrupt droughts and floods.Since 1990,the frequency,inten-sity,and variability of the drought-flood risk index have been significant.The frequency of transitions from drought to flood is relatively high in Heihe,Nenjiang,and southeastern part of Jilin.In contrast,the intensity of these events is greater in the eastern part of the Songnen Plain and the Daxing'anling region.From 1950 to 2023,the risk index of drought-to-flood transitions in the Basin has shown an increasing trend;contributions of the risk index for drought-to-flood transitions in May and June are relatively large,especially in the northern and northeastern part in May and the central region in June;the contribution in July is relatively small.The frequency of transitions from flood to drought is relatively high in the Sanjiang Plain and the southeastern part of Jilin,with greater intensity observed in the central area of the Songnen Plain.From 1950 to 2023,the risk index for transitions from flood to drought has increased;however,this trend is not statistically significant.In the past 20 years,the interannual variability of the frequency and risk index of drought-to-flood transitions has been significant,and they are also significant around 1970 and from 1995 to 2010.The risk index contribution of flood-to-drought transitions in July across the Basin is substantial,with notable contributions in May for the northern and western parts,and in June,July,and September for the eastern part.Changes in precipitation variability may directly influence the ab-rupt risk index of drought and flood in the Songhua River Basin.

drought-flood abruptthe Songhua River Basinspatiotemporal changesrisk index

刘玉莲、康恒元、李秀芬

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黑龙江省气候中心,哈尔滨 150030

五营国家气候观象台,伊春 153000

哈尔滨市气象局,哈尔滨 150028

黑龙江省气象科学研究所,哈尔滨 150030

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旱涝急转 松花江流域 时空变化 风险指数

2025

应用气象学报
中国气象科学研究院 国家气象中心 国家卫星气象中心 国家气候中心 国家气象信息中心 中国气象局气象探测中心

应用气象学报

北大核心
影响因子:1.459
ISSN:1001-7313
年,卷(期):2025.36(2)