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- W4286639920 abstract "Abstract The intensity, duration, and frequency (IDF) of low streamflow events are often considered stationary in time. Given droughts are likely to become more frequent and extreme, here those IDFs are analyzed for their non‐stationarity in relation to three climate drivers, namely, the El Niño‐Southern Oscillation, the Indian Ocean Dipole, and the Southern Annular Mode. For this, low flow events were identified for 161 unregulated catchments in Victoria, Australia. The relationship between the climate drivers and the IDFs were developed using covariate‐based non‐stationary statistical models. We found that several of these catchments exhibit strong non‐stationary influences from the climate modes. Such catchments have a higher probability of experiencing more intense, prolonged, and/or frequent low flows when a dry phase of these climate drivers occurs. We found that catchments having strong evidence of non‐stationary frequency ( n = 77) were more compared to those having non‐stationary intensity ( n = 19) or duration ( n = 34). Further, we derived projected indices of these climate drivers from CMIP5 models for the RCP8.5 scenario. These indicate an intensification in the dry phase of the climate drivers. Using information of the projected indices in the IDF models, we found that future dry phases of these climate drivers are likely to further increase the probability of experiencing higher magnitudes of low flow IDFs in catchments non‐stationary in these characteristics in relation to one or more of these climate drivers. Frequency shows greater response to future dry phases of these drivers than intensity or duration of low flows." @default.
- W4286639920 created "2022-07-23" @default.
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- W4286639920 date "2022-07-01" @default.
- W4286639920 modified "2023-10-01" @default.
- W4286639920 title "Non‐Stationary Influences of Large‐Scale Climate Drivers on Low Flow Extremes in Southeast Australia" @default.
- W4286639920 cites W128533561 @default.
- W4286639920 cites W129305155 @default.
- W4286639920 cites W1500657154 @default.
- W4286639920 cites W1556090316 @default.
- W4286639920 cites W1595159159 @default.
- W4286639920 cites W1609585737 @default.
- W4286639920 cites W1665401944 @default.
- W4286639920 cites W1665721417 @default.
- W4286639920 cites W1964513767 @default.
- W4286639920 cites W1967863463 @default.
- W4286639920 cites W1984231257 @default.
- W4286639920 cites W1985661264 @default.
- W4286639920 cites W1986263898 @default.
- W4286639920 cites W1990000849 @default.
- W4286639920 cites W1992109129 @default.
- W4286639920 cites W1995743207 @default.
- W4286639920 cites W2013909639 @default.
- W4286639920 cites W2022787571 @default.
- W4286639920 cites W2031346902 @default.
- W4286639920 cites W2032866640 @default.
- W4286639920 cites W2037797393 @default.
- W4286639920 cites W2044035070 @default.
- W4286639920 cites W2044987862 @default.
- W4286639920 cites W2055340620 @default.
- W4286639920 cites W2058328641 @default.
- W4286639920 cites W2061991767 @default.
- W4286639920 cites W2079377422 @default.
- W4286639920 cites W2080192596 @default.
- W4286639920 cites W2080739280 @default.
- W4286639920 cites W2082001988 @default.
- W4286639920 cites W2086535886 @default.
- W4286639920 cites W2088266147 @default.
- W4286639920 cites W2097403132 @default.
- W4286639920 cites W2101108516 @default.
- W4286639920 cites W2102588958 @default.
- W4286639920 cites W2107489669 @default.
- W4286639920 cites W2109465218 @default.
- W4286639920 cites W2115489405 @default.
- W4286639920 cites W2120004639 @default.
- W4286639920 cites W2124076118 @default.
- W4286639920 cites W2130091784 @default.
- W4286639920 cites W2131086800 @default.
- W4286639920 cites W2135725459 @default.
- W4286639920 cites W2142635246 @default.
- W4286639920 cites W2158952405 @default.
- W4286639920 cites W2159689047 @default.
- W4286639920 cites W2164072970 @default.
- W4286639920 cites W2165301409 @default.
- W4286639920 cites W2167106264 @default.
- W4286639920 cites W2168396386 @default.
- W4286639920 cites W2248796894 @default.
- W4286639920 cites W230693944 @default.
- W4286639920 cites W2318480145 @default.
- W4286639920 cites W2409349911 @default.
- W4286639920 cites W2468503799 @default.
- W4286639920 cites W2491513442 @default.
- W4286639920 cites W2516934950 @default.
- W4286639920 cites W2582969025 @default.
- W4286639920 cites W2612052242 @default.
- W4286639920 cites W2730028507 @default.
- W4286639920 cites W2770679673 @default.
- W4286639920 cites W2792010339 @default.
- W4286639920 cites W2792444893 @default.
- W4286639920 cites W2800324450 @default.
- W4286639920 cites W2887679048 @default.
- W4286639920 cites W2903352811 @default.
- W4286639920 cites W2904109594 @default.
- W4286639920 cites W2904535766 @default.
- W4286639920 cites W2905334383 @default.
- W4286639920 cites W2921898421 @default.
- W4286639920 cites W2949210087 @default.
- W4286639920 cites W3003367883 @default.
- W4286639920 cites W3007882649 @default.
- W4286639920 cites W3019650895 @default.
- W4286639920 cites W3039446713 @default.
- W4286639920 cites W3084447037 @default.
- W4286639920 cites W3118148064 @default.
- W4286639920 cites W3161201474 @default.
- W4286639920 cites W3175806815 @default.
- W4286639920 cites W4235730371 @default.
- W4286639920 cites W4288625073 @default.
- W4286639920 cites W4379510236 @default.
- W4286639920 doi "https://doi.org/10.1029/2021wr031508" @default.
- W4286639920 hasPublicationYear "2022" @default.
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