Articles | Volume 27, issue 13
https://doi.org/10.5194/hess-27-2479-2023
https://doi.org/10.5194/hess-27-2479-2023
Review article
 | 
10 Jul 2023
Review article |  | 10 Jul 2023

Floods and droughts: a multivariate perspective

Manuela Irene Brunner

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Cited articles

Abatan, A. A., Gutowski, W. J., Ammann, C. M., Kaatz, L., Brown, B. G., Buja, L., Bullock, R., Fowler, T., Gilleland, E., and Gotway, J. H.: Multiyear droughts and pluvials over the upper Colorado River basin and associated circulations, J. Hydrometeorol., 18, 799–818, https://doi.org/10.1175/JHM-D-16-0125.1, 2017. a
Alvarez-Garreton, C., Pablo Boisier, J., Garreaud, R., Seibert, J., and Vis, M.: Progressive water deficits during multiyear droughts in basins with long hydrological memory in Chile, Hydrol. Earth Syst. Sci., 25, 429–446, https://doi.org/10.5194/hess-25-429-2021, 2021. a
Andreadis, K. M., Clark, E. A., Wood, A. W., Hamlet, A. F., and Lettenmaier, D. P.: Twentieth-Century drought in the conterminous United States, J. Hydrometeorol., 6, 985–1001, 2005. a
Ansari, R. and Grossi, G.: Spatio-temporal evolution of wet–dry event features and their transition across the Upper Jhelum Basin (UJB) in South Asia, Nat. Hazards Earth Syst. Sci., 22, 287–302, https://doi.org/10.5194/nhess-22-287-2022, 2022. a
Bales, R. C., Goulden, M. L., Hunsaker, C. T., Conklin, M. H., Hartsough, P. C., O'Geen, A. T., Hopmans, J. W., and Safeeq, M.: Mechanisms controlling the impact of multi-year drought on mountain hydrology, Sci. Rep., 8, 1–8, https://doi.org/10.1038/s41598-017-19007-0, 2018. a
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Short summary
I discuss different types of multivariate hydrological extremes and their dependencies, including regional extremes affecting multiple locations, such as spatially connected flood events; consecutive extremes occurring in close temporal succession, such as successive droughts; extremes characterized by multiple characteristics, such as floods with jointly high peak discharge and flood volume; and transitions between different types of extremes, such as drought-to-flood transitions.