Articles | Volume 24, issue 11
https://doi.org/10.5194/hess-24-5595-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-24-5595-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
New flood frequency estimates for the largest river in Norway based on the combination of short and long time series
The Norwegian Water Resources and Energy Directorate, Oslo, Norway
Anna Aano
The Norwegian Water Resources and Energy Directorate, Oslo, Norway
Department of Geosciences, University of Oslo, Oslo, Norway
Ida Steffensen
Department of Earth Science, University of Bergen, Bergen, Norway
Eivind Støren
Department of Earth Science, University of Bergen, Bergen, Norway
Bjerknes Centre for Climate Research, Bergen, Norway
Øyvind Paasche
Bjerknes Centre for Climate Research, Bergen, Norway
NORCE Climate, Bergen, Norway
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20 citations as recorded by crossref.
- A Hydrological and Hydrochemical Study of the Gudiyalchay River: Understanding Groundwater–River Interactions L. Mammadova et al. 10.3390/w16172480
- Understanding the Contributions of Paleo‐Informed Natural Variability and Climate Changes to Hydroclimate Extremes in the San Joaquin Valley of California R. Gupta et al. 10.1029/2023EF003909
- Influence of warming and atmospheric circulation changes on multidecadal European flood variability S. Brönnimann et al. 10.5194/cp-18-919-2022
- Nordic contributions to stochastic methods in hydrology D. Rosbjerg et al. 10.2166/nh.2022.137
- Flood variability in the upper Yangtze River over the last millennium—Insights from a comparison of climate-hydrological model simulated and reconstruction R. Huo et al. 10.1007/s11430-022-1008-5
- Fluvial palaeohydrology in the 21st century and beyond V. Baker et al. 10.1002/esp.5275
- 长江上游近千年来的洪水变化——比较气候-水文模型模拟数据与重建数据 苒. 霍 et al. 10.1360/N072022-0079
- Changing flood dynamics in Norway since the last millennium and to the end of the 21st century R. Huo et al. 10.1016/j.jhydrol.2022.128331
- Reconstructing Paleoflood Occurrence and Magnitude from Lake Sediments B. Wilhelm et al. 10.3390/quat5010009
- A 7000-year record of extreme flood events reconstructed from a threshold lake in southern Norway J. Hardeng et al. 10.1016/j.quascirev.2024.108659
- Reconstructing the peak flow of historical flood events using a hydraulic model: The city of Bath, United Kingdom I. Stamataki & T. Kjeldsen 10.1111/jfr3.12719
- Lake sediments from southern Norway capture Holocene variations in flood seasonality J. Hardeng et al. 10.1016/j.quascirev.2022.107643
- Timing and maximum flood level of the Early Holocene glacial lake Nedre Glomsjø outburst flood, Norway F. Høgaas et al. 10.1111/bor.12615
- Holocene extreme flood events in the middle reaches of the Lancang‒Mekong River basin recorded by a high-altitude lake in southwestern China S. Shao et al. 10.1016/j.quascirev.2024.108918
- A comprehensive uncertainty framework for historical flood frequency analysis: a 500-year-long case study M. Lucas et al. 10.5194/hess-28-5031-2024
- A Non-Stationarity Analysis of Annual Maximum Floods: A Case Study of Campaspe River Basin, Australia A. Yilmaz et al. 10.3390/w15203683
- Hydrodynamic reconstruction of the paleoflood from the Early Holocene ice-dammed lake Nedre Glomsjø, Norway K. Aurand et al. 10.1016/j.ejrh.2024.101937
- Palynological and sedimentological evidence for early mid-Holocene hydroclimatic variability in the Ningshao Plain, East China S. Yao et al. 10.1016/j.palaeo.2023.111997
- Analysis of the nonstationarity characteristics and future trends of flood extremes in the Dongting Lake Basin Y. Gao et al. 10.1016/j.ejrh.2022.101217
- PDFID: A high-resolution flood inundation dataset with a long time series L. Chen et al. 10.1016/j.ejrh.2024.101715
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Short summary
We combine systematic, historical, and paleo information to obtain flood information from the last 10 300 years for the Glomma River in Norway. We identify periods with increased flood activity (4000–2000 years ago and the recent 1000 years) that correspond broadly to periods with low summer temperatures and glacier growth. The design floods in Glomma were more than 20 % higher during the 18th century than today. We suggest that trends in flood variability are linked to snow in late spring.
We combine systematic, historical, and paleo information to obtain flood information from the...