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Global hydrology 2015: State, trends, and directions [PDF]

, 2015
Global hydrology has come a long way since the first introduction of the primitive land surface model of Manabe (1969) and the declaration of the “Emergence of Global Hydrology” by Eagleson (1986).
Landscape functioning, Geocomputation and Hydrology, Marc F. P. Bierkens, Hydrologie, Bierkens, Marc F. P.   +3 more
core   +2 more sources

Acknowledgment to Reviewers of Hydrology in 2020

, 2021
Peer review is the driving force of journal development, and reviewers are gatekeepers who ensure that Hydrology maintains its standards for the high quality of its published papers [...
Hydrology Editorial Office Hydrology Editorial Office
core   +1 more source

Coupling Waterlogging Hazard Assessment Based on SWMM–LISFLOOD Simulation in Chaoyang River Basin of Nanning, China

Journal of Flood Risk Management, Volume 19, Issue 2, June 2026.
ABSTRACT Urban stormwater waterlogging poses significant threats to public safety and property, making scientific and effective risk management a crucial element in China's whole‐area sponge city construction. This study evaluates waterlogging hazards in Nanning's Chaoyang River Basin using a SWMM–LISFLOOD coupled model to simulate 11 design storm ...
Yang Yun‐chuan, Tang Ya‐qian, Fu Hao, Liao Li‐ping, Feng Min‐hui, Mo Chong‐xun, Li Xun‐gui, Sun Gui‐kai   +7 more
wiley   +1 more source

Hydrological reconstruction and climatic background of the Holocene extreme paleoflood event in the Danjiang River, central China

Open Geosciences
The Danjiang River Basin, situated in central China, serves as the water source for the Middle Route of the South-to-North Water Diversion Project. The occurrence of catastrophic rainstorm-induced floods within this basin constitutes a significant hazard
Li Xiaogang, Lei Shaohua, Zhang Yuzhu, Pang Jiangli   +3 more
doaj   +1 more source

Sedimentary records of palaeohydrological variability during the Late Holocene in the Lower Narmada Basin, western India

The Depositional Record, Volume 12, Issue 1, February 2026.
Late Holocene palaeohydrological changes in the lower Narmada Basin, India, revealed using multiproxy analyses of the Orsang River terrace sediments. Distinct depositional phases corresponding to global climatic events were recorded. High‐magnitude floods in the Narmada River during the MWP, and within the tributary Orsang River during DACP and LIA ...
Alpa Sridhar, Pooja Tiwari, Biswajit Thakur, Deependra Singh, Vineet Goswami, Sanjit Kumar Jena, Ravi Bhushan, Saremulhaq Parwej Mosarraf Shaikh, Deepak Maurya, Laxman Singh Chamyal   +9 more
wiley   +1 more source

Lower Meuse Paleoflood Record Reveals NAO‐Driven Decadal to Multi‐Centennial Variability

Geophysical Research Letters, Volume 52, Issue 18, 28 September 2025.
Abstract A central challenge in assessing climate‐driven flood regimes is constructing long‐term paleoflood records with sufficient temporal resolution to identify both short‐ and long‐term variability. To address this, we performed grain‐size and X‐ray fluorescence scanning analyses on two cores from paleochannels in the Lower Meuse (the Netherlands).
Fei Peng, Willem Toonen, Xueqin Yang, Rick Hennekam, Nina van Leeuwen, Sanne Rip, Cornelis Kasse   +6 more
wiley   +1 more source

Land-use change as a major driver for mid-20th-century flood intensity reduction in the Southeastern US

Environmental Research Letters
Land-use changes affect hydrologic processes, but their impact on flooding remains obscure amid increasingly heavy precipitation. Instrumental records are short relative to land-use change history and inadequate for flood attribution studies.
Zhixiong Shen, Nicholas Conway, Shaowu Bao, Samuel Muñoz, Andreas Lang   +4 more
doaj   +1 more source

Fluviomorphic trajectories for dryland ephemeral stream channels following extreme flash floods

Earth Surface Processes and Landforms, Volume 49, Issue 9, Page 2628-2650, July 2024.
Aerial photographs enable evolutionary trajectory analyses of ephemeral streams. The geometric braiding index reaches the pre‐flood state the fastest, that is, in circa 15–24 years. Junction‐node density and stream‐link area recover in 25 years after extraordinary floods, but the spatial distribution of the channel forms takes 30–35 years to recover ...
Eliisa Lotsari, P. Kyle House, Petteri Alho, Victor R. Baker   +3 more
wiley   +1 more source

Bank erosion and erosion processes from dendrogeomorphology in southern U.S. prairie streams

River Research and Applications, Volume 40, Issue 5, Page 747-760, June 2024.
Abstract Streambank erosion processes influence the amount of soil material contributed to rivers and sedimentation rates in receiving reservoirs. However, the amount of data on bank erosion rates is limited both in range and extent affecting planning for mitigation and watershed management.
Joseph D. White, Peter M. Allen, Stephen G. Norair II, Samuel T. Barber, John Dunbar, Jungang Gao   +5 more
wiley   +1 more source

Challenges in the attribution of river flood events

WIREs Climate Change, Volume 15, Issue 3, May/June 2024.
Drivers of river floods change through time. Global warming, and associated changes in temperature and precipitation, often overlap with changes in the hydrology, such as land‐cover change, construction of levees and large‐scale irrigation. This poses a special challenge to the attribution of flood events.
Paolo Scussolini, Linh Nhat Luu, Sjoukje Philip, Wouter R. Berghuijs, Dirk Eilander, Jeroen C. J. H. Aerts, Sarah F. Kew, Geert Jan van Oldenborgh, Willem H. J. Toonen, Jan Volkholz, Dim Coumou   +10 more
wiley   +1 more source