Articles | Volume 11, issue 4
https://doi.org/10.5194/esurf-11-547-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-11-547-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
06 Jul 2023
Research article |
| 06 Jul 2023
| 06 Jul 2023
Synoptic-scale to mesoscale atmospheric circulation connects fluvial and coastal gravel conveyors and directional deposition of coastal landforms in the Dead Sea basin
The Freddy & Nadin Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, The Edmond J. Safra Campus, Givat Ram, Jerusalem, 91904, Israel
Geological Survey of Israel, 32 Yesha'yahu Leibowitz, Jerusalem,
9371234, Israel
Moshe Armon
The Freddy & Nadin Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, The Edmond J. Safra Campus, Givat Ram, Jerusalem, 91904, Israel
Institute for Atmospheric and Climate Science, ETH Zurich, 8092, Zurich, Switzerland
Yehouda Enzel
The Freddy & Nadin Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, The Edmond J. Safra Campus, Givat Ram, Jerusalem, 91904, Israel
Geological Survey of Israel, 32 Yesha'yahu Leibowitz, Jerusalem,
9371234, Israel
The Freddy & Nadin Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, The Edmond J. Safra Campus, Givat Ram, Jerusalem, 91904, Israel
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Ellina Agayar, Franziska Aemisegger, Moshe Armon, Alexander Scherrmann, and Heini Wernli
Nat. Hazards Earth Syst. Sci., 24, 2441–2459, https://doi.org/10.5194/nhess-24-2441-2024, https://doi.org/10.5194/nhess-24-2441-2024, 2024
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This study presents the results of a climatological investigation of extreme precipitation events (EPEs) in Ukraine for the period 1979–2019. During all seasons EPEs are associated with pronounced upper-level potential vorticity (PV) anomalies. In addition, we find distinct seasonal and regional differences in moisture sources. Several extreme precipitation cases demonstrate the importance of these processes, complemented by a detailed synoptic analysis.
Shai Abir, Hamish A. McGowan, Yonatan Shaked, Hezi Gildor, Efrat Morin, and Nadav G. Lensky
Atmos. Chem. Phys., 24, 6177–6195, https://doi.org/10.5194/acp-24-6177-2024, https://doi.org/10.5194/acp-24-6177-2024, 2024
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Understanding air–sea heat exchange is vital for studying ocean dynamics. Eddy covariance measurements over the Gulf of Eilat revealed a 3.22 m yr-1 evaporation rate, which is inconsistent with bulk formulae estimations in stable atmospheric conditions, requiring bulk formulae to be revisited in these environments. The surface fluxes have a net cooling effect on the gulf water on an annual mean (-79 W m-2), balanced by a strong exchange flux between the Red Sea and the Gulf of Eilat.
Joëlle C. Rieder, Franziska Aemisegger, Elad Dente, and Moshe Armon
EGUsphere, https://doi.org/10.5194/egusphere-2024-539, https://doi.org/10.5194/egusphere-2024-539, 2024
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The Sahara was wetter in the past and may become wetter in the future. Lake remnants are evidence of the desert’s wetter past. If the Sahara gets wetter in the future, these lakes may serve as a water resource. However, it is unclear how these lakes get filled and how moisture is carried into the desert and converted into rain in the first place. Therefore, we examine processes currently leading to the filling of a dry lake in the Sahara, which can help in assessing future water availability.
Francesco Marra, Moshe Armon, and Efrat Morin
Hydrol. Earth Syst. Sci., 26, 1439–1458, https://doi.org/10.5194/hess-26-1439-2022, https://doi.org/10.5194/hess-26-1439-2022, 2022
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We present a new method for quantifying the probability of occurrence of extreme rainfall using radar data, and we use it to examine coastal and orographic effects on extremes. We identify three regimes, directly related to precipitation physical processes, which respond differently to these forcings. The methods and results are of interest for researchers and practitioners using radar for the analysis of extremes, risk managers, water resources managers, and climate change impact studies.
Yoav Ben Dor, Francesco Marra, Moshe Armon, Yehouda Enzel, Achim Brauer, Markus Julius Schwab, and Efrat Morin
Clim. Past, 17, 2653–2677, https://doi.org/10.5194/cp-17-2653-2021, https://doi.org/10.5194/cp-17-2653-2021, 2021
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Laminated sediments from the deepest part of the Dead Sea unravel the hydrological response of the eastern Mediterranean to past climate changes. This study demonstrates the importance of geological archives in complementing modern hydrological measurements that do not fully capture natural hydroclimatic variability, which is crucial to configure for understanding the impact of climate change on the hydrological cycle in subtropical regions.
Yair Rinat, Francesco Marra, Moshe Armon, Asher Metzger, Yoav Levi, Pavel Khain, Elyakom Vadislavsky, Marcelo Rosensaft, and Efrat Morin
Nat. Hazards Earth Syst. Sci., 21, 917–939, https://doi.org/10.5194/nhess-21-917-2021, https://doi.org/10.5194/nhess-21-917-2021, 2021
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Flash floods are among the most devastating and lethal natural hazards worldwide. The study of such events is important as flash floods are poorly understood and documented processes, especially in deserts. A small portion of the studied basin (1 %–20 %) experienced extreme rainfall intensities resulting in local flash floods of high magnitudes. Flash floods started and reached their peak within tens of minutes. Forecasts poorly predicted the flash floods mostly due to location inaccuracy.
Moshe Armon, Francesco Marra, Yehouda Enzel, Dorita Rostkier-Edelstein, and Efrat Morin
Hydrol. Earth Syst. Sci., 24, 1227–1249, https://doi.org/10.5194/hess-24-1227-2020, https://doi.org/10.5194/hess-24-1227-2020, 2020
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Heavy precipitation events (HPEs), occurring around the globe, lead to natural hazards as well as to water resource recharge. Rainfall patterns during HPEs vary from one case to another and govern their effect. Thus, correct prediction of these patterns is crucial for coping with HPEs. However, the ability of weather models to generate such patterns is unclear. Here, we characterise rainfall patterns during HPEs based on weather radar data and evaluate weather model simulations of these events.
Davide Zoccatelli, Francesco Marra, Moshe Armon, Yair Rinat, James A. Smith, and Efrat Morin
Hydrol. Earth Syst. Sci., 23, 2665–2678, https://doi.org/10.5194/hess-23-2665-2019, https://doi.org/10.5194/hess-23-2665-2019, 2019
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This study presents a comparison of flood properties over multiple Mediterranean and desert catchments. While in Mediterranean areas floods are related to rainfall amount, in deserts we observed a strong connection with the characteristics of the more intense part of storms. Because of the different mechanisms involved, despite having significantly shorter and more localized storms, deserts are able to produce floods with a magnitude comparable to Mediterranean areas.
Elad Levintal, Nadav G. Lensky, Amit Mushkin, and Noam Weisbrod
Earth Syst. Dynam., 9, 1141–1153, https://doi.org/10.5194/esd-9-1141-2018, https://doi.org/10.5194/esd-9-1141-2018, 2018
I. Neugebauer, M. J. Schwab, N. D. Waldmann, R. Tjallingii, U. Frank, E. Hadzhiivanova, R. Naumann, N. Taha, A. Agnon, Y. Enzel, and A. Brauer
Clim. Past, 12, 75–90, https://doi.org/10.5194/cp-12-75-2016, https://doi.org/10.5194/cp-12-75-2016, 2016
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Micro-facies changes and elemental variations in deep Dead Sea sediments are used to reconstruct relative lake level changes for the early last glacial period. The results indicate a close link of hydroclimatic variability in the Levant to North Atlantic-Mediterranean climates during the time of the build-up of Northern Hemisphere ice shields. First petrographic analyses of gravels in the deep core question the recent hypothesis of a Dead Sea dry-down at the end of the last interglacial.
E. Shamir, L. Ben-Moshe, A. Ronen, T. Grodek, Y. Enzel, K. P. Georgakakos, and E. Morin
Hydrol. Earth Syst. Sci., 17, 1021–1034, https://doi.org/10.5194/hess-17-1021-2013, https://doi.org/10.5194/hess-17-1021-2013, 2013
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Physical: Geomorphology (including all aspects of fluvial, coastal, aeolian, hillslope and glacial geomorphology)
Post-fire evolution of ravel transport regimes in the Diablo Range, CA
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The Aare main overdeepening on the northern margin of the European Alps: basins, riegels, and slot canyons
A simple model for faceted topographies at normal faults based on an extended stream-power law
Testing floc settling velocity models in rivers and freshwater wetlands
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A landslide runout model for sediment transport, landscape evolution, and hazard assessment applications
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Hayden L. Jacobson, Danica L. Roth, Gabriel Walton, Margaret Zimmer, and Kerri Johnson
Earth Surf. Dynam., 12, 1415–1446, https://doi.org/10.5194/esurf-12-1415-2024, https://doi.org/10.5194/esurf-12-1415-2024, 2024
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Loose grains travel farther after a fire because no vegetation is left to stop them. This matters since loose grains at the base of a slope can turn into a debris flow if it rains. To find if grass growing back after a fire had different impacts on grains of different sizes on slopes of different steepness, we dropped thousands of natural grains and measured how far they went. Large grains went farther 7 months after the fire than 11 months after, and small grain movement didn’t change much.
Elizabeth N. Orr, Taylor F. Schildgen, Stefanie Tofelde, Hella Wittmann, and Ricardo N. Alonso
Earth Surf. Dynam., 12, 1391–1413, https://doi.org/10.5194/esurf-12-1391-2024, https://doi.org/10.5194/esurf-12-1391-2024, 2024
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Fluvial terraces and alluvial fans in the Toro Basin, NW Argentina, record river evolution and global climate cycles over time. Landform dating reveals lower-frequency climate cycles (100 kyr) preserved downstream and higher-frequency cycles (21/40 kyr) upstream, supporting theoretical predications that longer rivers filter out higher-frequency climate signals. This finding improves our understanding of the spatial distribution of sedimentary paleoclimate records within landscapes.
Fritz Schlunegger, Edi Kissling, Dimitri Tibo Bandou, Guilhem Amin Douillet, David Mair, Urs Marti, Regina Reber, Patrick Schläfli, and Michael Alfred Schwenk
Earth Surf. Dynam., 12, 1371–1389, https://doi.org/10.5194/esurf-12-1371-2024, https://doi.org/10.5194/esurf-12-1371-2024, 2024
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Overdeepenings are bedrock depressions filled with sediment. We combine the results of a gravity survey with drilling data to explore the morphology of such a depression beneath the city of Bern. We find that the target overdeepening comprises two basins >200 m deep. They are separated by a bedrock riegel that itself is cut by narrow canyons up to 150 m deep. We postulate that these structures formed underneath a glacier, where erosion by subglacial meltwater caused the formation of the canyons.
Stefan Hergarten
Earth Surf. Dynam., 12, 1315–1327, https://doi.org/10.5194/esurf-12-1315-2024, https://doi.org/10.5194/esurf-12-1315-2024, 2024
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Faceted topographies are impressive footprints of active tectonics in geomorphology. This paper investigates the evolution of faceted topographies at normal faults and their interaction with a river network theoretically and numerically. As a main result beyond several relations for the geometry of facets, the horizontal displacement associated with normal faults is crucial for the dissection of initially polygonal facets into triangular facets bounded by almost parallel rivers.
Justin A. Nghiem, Gen K. Li, Joshua P. Harringmeyer, Gerard Salter, Cédric G. Fichot, Luca Cortese, and Michael P. Lamb
Earth Surf. Dynam., 12, 1267–1294, https://doi.org/10.5194/esurf-12-1267-2024, https://doi.org/10.5194/esurf-12-1267-2024, 2024
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Fine sediment grains in freshwater can cohere into faster-settling particles called flocs, but floc settling velocity theory has not been fully validated. Combining three data sources in novel ways in the Wax Lake Delta, we verified a semi-empirical model relying on turbulence and geochemical factors. For a physics-based model, we showed that the representative grain diameter within flocs relies on floc structure and that heterogeneous flow paths inside flocs increase floc settling velocity.
Jessica Marggraf, Guillaume Dramais, Jérôme Le Coz, Blaise Calmel, Benoît Camenen, David J. Topping, William Santini, Gilles Pierrefeu, and François Lauters
Earth Surf. Dynam., 12, 1243–1266, https://doi.org/10.5194/esurf-12-1243-2024, https://doi.org/10.5194/esurf-12-1243-2024, 2024
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Suspended-sand fluxes in rivers vary with time and space, complicating their measurement. The proposed method captures the vertical and lateral variations of suspended-sand concentration throughout a river cross-section. It merges water samples taken at various positions throughout the cross-section with high-resolution acoustic velocity measurements. This is the first method that includes a fully applicable uncertainty estimation; it can easily be applied to any other study sites.
Dominic T. Robson and Andreas C. W. Baas
Earth Surf. Dynam., 12, 1205–1226, https://doi.org/10.5194/esurf-12-1205-2024, https://doi.org/10.5194/esurf-12-1205-2024, 2024
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Barchans are fast-moving sand dunes which form large populations (swarms) on Earth and Mars. We show that a small range of model parameters produces swarms in which dune size does not vary downwind – something that is observed in nature but not when using earlier models. We also show how the shape of dunes and the spatial patterns they form are affected by wind direction. This work furthers our understanding of the interplay between environmental drivers, dune interactions, and swarm properties.
Jeffrey Keck, Erkan Istanbulluoglu, Benjamin Campforts, Gregory Tucker, and Alexander Horner-Devine
Earth Surf. Dynam., 12, 1165–1191, https://doi.org/10.5194/esurf-12-1165-2024, https://doi.org/10.5194/esurf-12-1165-2024, 2024
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MassWastingRunout (MWR) is a new landslide runout model designed for sediment transport, landscape evolution, and hazard assessment applications. MWR is written in Python and includes a calibration utility that automatically determines best-fit parameters for a site and empirical probability density functions of each parameter for probabilistic model implementation. MWR and Jupyter Notebook tutorials are available as part of the Landlab package at https://github.com/landlab/landlab.
Ariane Mueting and Bodo Bookhagen
Earth Surf. Dynam., 12, 1121–1143, https://doi.org/10.5194/esurf-12-1121-2024, https://doi.org/10.5194/esurf-12-1121-2024, 2024
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This study investigates the use of optical PlanetScope data for offset tracking of the Earth's surface movement. We found that co-registration accuracy is locally degraded when outdated elevation models are used for orthorectification. To mitigate this bias, we propose to only correlate scenes acquired from common perspectives or base orthorectification on more up-to-date elevation models generated from PlanetScope data alone. This enables a more detailed analysis of landslide dynamics.
Cho-Hee Lee, Yeong Bae Seong, John Weber, Sangmin Ha, Dong-Eun Kim, and Byung Yong Yu
Earth Surf. Dynam., 12, 1091–1120, https://doi.org/10.5194/esurf-12-1091-2024, https://doi.org/10.5194/esurf-12-1091-2024, 2024
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Topographic metrics were used to understand changes due to tectonic activity. We evaluated the relative tectonic activity along the Ulsan Fault Zone (UFZ), one of the most active fault zones in South Korea. We divided the UFZ into five segments, based on the spatial variation in activity. We modeled the landscape evolution of the study area and interpreted tectono-geomorphic history during which the northern part of the UFZ experienced asymmetric uplift, while the southern part did not.
Juditha Aga, Livia Piermattei, Luc Girod, Kristoffer Aalstad, Trond Eiken, Andreas Kääb, and Sebastian Westermann
Earth Surf. Dynam., 12, 1049–1070, https://doi.org/10.5194/esurf-12-1049-2024, https://doi.org/10.5194/esurf-12-1049-2024, 2024
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Coastal rock cliffs on Svalbard are considered to be fairly stable; however, long-term trends in coastal-retreat rates remain unknown. This study examines changes in the coastline position along Brøggerhalvøya, Svalbard, using aerial images from 1970, 1990, 2010, and 2021. Our analysis shows that coastal-retreat rates accelerate during the period 2010–2021, which coincides with increasing storminess and retreating sea ice.
Aaron T. Steelquist, Gustav B. Seixas, Mary L. Gillam, Sourav Saha, Seulgi Moon, and George E. Hilley
Earth Surf. Dynam., 12, 1071–1089, https://doi.org/10.5194/esurf-12-1071-2024, https://doi.org/10.5194/esurf-12-1071-2024, 2024
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The rates at which rivers erode their bed can be used to interpret the geologic history of a region. However, these rates depend significantly on the time window over which you measure. We use multiple dating methods to determine an incision rate for the San Juan River and compare it to regional rates with longer timescales. We demonstrate how specific geologic events, such as cutoffs of bedrock meander bends, are likely to preserve material we can date but also bias the rates we measure.
Johannes Leinauer, Michael Dietze, Sibylle Knapp, Riccardo Scandroglio, Maximilian Jokel, and Michael Krautblatter
Earth Surf. Dynam., 12, 1027–1048, https://doi.org/10.5194/esurf-12-1027-2024, https://doi.org/10.5194/esurf-12-1027-2024, 2024
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Massive rock slope failures are a significant alpine hazard and change the Earth's surface. Therefore, we must understand what controls the preparation of such events. By correlating 4 years of slope displacements with meteorological and seismic data, we found that water from rain and snowmelt is the most important driver. Our approach is applicable to similar sites and indicates where future climatic changes, e.g. in rain intensity and frequency, may alter the preparation of slope failure.
Julien Coatléven and Benoit Chauveau
Earth Surf. Dynam., 12, 995–1026, https://doi.org/10.5194/esurf-12-995-2024, https://doi.org/10.5194/esurf-12-995-2024, 2024
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The aim of this paper is to explain how to incorporate classical water flow routines into landscape evolution models while keeping numerical errors under control. The key idea is to adapt filtering strategies to eliminate anomalous numerical errors and mesh dependencies, as confirmed by convergence tests with analytic solutions. The emergence of complex geomorphic structures is now driven exclusively by nonlinear heterogeneous physical processes rather than by random numerical artifacts.
Jingjuan Li, John D. Jansen, Xuanmei Fan, Zhiyong Ding, Shugang Kang, and Marco Lovati
Earth Surf. Dynam., 12, 953–971, https://doi.org/10.5194/esurf-12-953-2024, https://doi.org/10.5194/esurf-12-953-2024, 2024
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In this study, we investigated the geomorphology, sedimentology, and chronology of Tuanjie (seven terraces) and Taiping (three terraces) terraces in Diexi, eastern Tibetan Plateau. Results highlight that two damming and three outburst events occurred in the area during the late Pleistocene, and the outburst floods have been a major factor in the formation of tectonically active mountainous river terraces. Tectonic activity and climatic changes play a minor role.
Jens Martin Turowski, Fergus McNab, Aaron Bufe, and Stefanie Tofelde
EGUsphere, https://doi.org/10.5194/egusphere-2024-2342, https://doi.org/10.5194/egusphere-2024-2342, 2024
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Channel belts comprise the area that is affected by a river due to lateral migration and floods. As a landform, they affect local water resources, flood hazard, and often host unique ecological communities. Here, we develop a model describing the evolution of channel belt area over time. The model connects the behaviour of the river to the evolution of the channel belt over a timescale of centuries. A comparison to selected data from experiments and real river systems is favourable.
Andrew Hollyday, Maureen E. Raymo, Jacqueline Austermann, Fred Richards, Mark Hoggard, and Alessio Rovere
Earth Surf. Dynam., 12, 883–905, https://doi.org/10.5194/esurf-12-883-2024, https://doi.org/10.5194/esurf-12-883-2024, 2024
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Sea level was significantly higher during the Pliocene epoch, around 3 million years ago. The present-day elevations of shorelines that formed in the past provide a data constraint on the extent of ice sheet melt and the global sea level response under warm Pliocene conditions. In this study, we identify 10 escarpments that formed from wave-cut erosion during Pliocene times and compare their elevations with model predictions of solid Earth deformation processes to estimate past sea level.
Gregory A. Ruetenik, Ken L. Ferrier, and Odin Marc
Earth Surf. Dynam., 12, 863–881, https://doi.org/10.5194/esurf-12-863-2024, https://doi.org/10.5194/esurf-12-863-2024, 2024
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Fluvial sediment fluxes increased dramatically in Taiwan during Typhoon Morakot in 2009, which produced some of the heaviest landsliding on record. We analyzed fluvial discharge and suspended sediment concentration data at 87 gauging stations across Taiwan to quantify fluvial sediment responses since Morakot. In basins heavily impacted by landsliding, rating curve coefficients sharply increased during Morakot and then declined exponentially with a characteristic decay time of <10 years.
Nil Carrion-Bertran, Albert Falqués, Francesca Ribas, Daniel Calvete, Rinse de Swart, Ruth Durán, Candela Marco-Peretó, Marta Marcos, Angel Amores, Tim Toomey, Àngels Fernández-Mora, and Jorge Guillén
Earth Surf. Dynam., 12, 819–839, https://doi.org/10.5194/esurf-12-819-2024, https://doi.org/10.5194/esurf-12-819-2024, 2024
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The sensitivity to the wave and sea-level forcing sources in predicting a 6-month embayed beach evolution is assessed using two different morphodynamic models. After a successful model calibration using in situ data, other sources are applied. The wave source choice is critical: hindcast data provide wrong results due to an angle bias, whilst the correct dynamics are recovered with the wave conditions from an offshore buoy. The use of different sea-level sources gives no significant differences.
Jean Vérité, Clément Narteau, Olivier Rozier, Jeanne Alkalla, Laurie Barrier, and Sylvain Courrech du Pont
EGUsphere, https://doi.org/10.5194/egusphere-2024-1634, https://doi.org/10.5194/egusphere-2024-1634, 2024
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Using a numerical model in 2D, we study how two identical dunes interact with each other when exposed to reversing winds. Depending on the distance between the dunes, they either repel or attract each other until they reach an equilibrium distance, which is controlled by the wind strength, wind reversal frequency and dune size. This process is controlled by the modification of wind flow over dunes of various shape, influencing the sediment transport downstream.
Abhishek Kashyap, Kristen Cook, and Mukunda Dev Behera
EGUsphere, https://doi.org/10.5194/egusphere-2024-1618, https://doi.org/10.5194/egusphere-2024-1618, 2024
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High-mountain floods exhibit a significant geomorphic hazard, often triggered by rapid snowmelt, extreme precipitation, glacial lake outbursts, and natural failures of dams. Such high-magnitude floods can have catastrophic impacts on downstream communities, ecosystems, and infrastructure. These floods demonstrate the significance of understanding the complex interaction of climatic, hydrological, and geological forces in high mountain regions.
Thomas J. Barnes, Thomas V. Schuler, Simon Filhol, and Karianne S. Lilleøren
Earth Surf. Dynam., 12, 801–818, https://doi.org/10.5194/esurf-12-801-2024, https://doi.org/10.5194/esurf-12-801-2024, 2024
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In this paper, we use machine learning to automatically outline landforms based on their characteristics. We test several methods to identify the most accurate and then proceed to develop the most accurate to improve its accuracy further. We manage to outline landforms with 65 %–75 % accuracy, at a resolution of 10 m, thanks to high-quality/high-resolution elevation data. We find that it is possible to run this method at a country scale to quickly produce landform inventories for future studies.
Eric Petersen, Regine Hock, and Michael G. Loso
Earth Surf. Dynam., 12, 727–745, https://doi.org/10.5194/esurf-12-727-2024, https://doi.org/10.5194/esurf-12-727-2024, 2024
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Ice cliffs are melt hot spots that increase melt rates on debris-covered glaciers which otherwise see a reduction in melt rates. In this study, we show how surface runoff streams contribute to the generation, evolution, and survival of ice cliffs by carving into the glacier and transporting rocky debris. On Kennicott Glacier, Alaska, 33 % of ice cliffs are actively influenced by streams, while nearly half are within 10 m of streams.
Daniel O'Hara, Liran Goren, Roos M. J. van Wees, Benjamin Campforts, Pablo Grosse, Pierre Lahitte, Gabor Kereszturi, and Matthieu Kervyn
Earth Surf. Dynam., 12, 709–726, https://doi.org/10.5194/esurf-12-709-2024, https://doi.org/10.5194/esurf-12-709-2024, 2024
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Understanding how volcanic edifices develop drainage basins remains unexplored in landscape evolution. Using digital evolution models of volcanoes with varying ages, we quantify the geometries of their edifices and associated drainage basins through time. We find that these metrics correlate with edifice age and are thus useful indicators of a volcano’s history. We then develop a generalized model for how volcano basins develop and compare our results to basin evolution in other settings.
Brayden Noh, Omar Wani, Kieran B. J. Dunne, and Michael P. Lamb
Earth Surf. Dynam., 12, 691–708, https://doi.org/10.5194/esurf-12-691-2024, https://doi.org/10.5194/esurf-12-691-2024, 2024
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In this paper, we propose a framework for generating risk maps that provide the probabilities of erosion due to river migration. This framework uses concepts from probability theory to learn the river migration model's parameter values from satellite data while taking into account parameter uncertainty. Our analysis shows that such geomorphic risk estimation is more reliable than models that do not explicitly consider various sources of variability and uncertainty.
Steven Y. J. Lai, David Amblas, Aaron Micallef, and Hervé Capart
Earth Surf. Dynam., 12, 621–640, https://doi.org/10.5194/esurf-12-621-2024, https://doi.org/10.5194/esurf-12-621-2024, 2024
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This study explores the creation of submarine canyons and hanging-wall fans on active faults, which can be defined by gravity-dominated breaching and underflow-dominated diffusion processes. The study reveals the self-similarity in canyon–fan long profiles, uncovers Hack’s scaling relationship and proposes a formula to estimate fan volume using canyon length. This is validated by global data from source-to-sink systems, providing insights into deep-water sedimentary processes.
Anuska Narayanan, Sagy Cohen, and John R. Gardner
Earth Surf. Dynam., 12, 581–599, https://doi.org/10.5194/esurf-12-581-2024, https://doi.org/10.5194/esurf-12-581-2024, 2024
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This study investigates the profound impact of deforestation in the Amazon on sediment dynamics. Novel remote sensing data and statistical analyses reveal significant changes, especially in heavily deforested regions, with rapid effects within a year. In less disturbed areas, a 1- to 2-year lag occurs, influenced by natural sediment shifts and human activities. These findings highlight the need to understand the consequences of human activity for our planet's future.
Jacob Hardt, Tim P. Dooley, and Michael R. Hudec
Earth Surf. Dynam., 12, 559–579, https://doi.org/10.5194/esurf-12-559-2024, https://doi.org/10.5194/esurf-12-559-2024, 2024
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We investigate the reaction of salt structures on ice sheet transgressions. We used a series of sandbox models that enabled us to experiment with scaled-down versions of salt bodies from northern Germany. The strongest reactions occurred when large salt pillows were partly covered by the ice load. Subsurface salt structures may play an important role in the energy transition, e.g., as energy storage. Thus, it is important to understand all processes that affect their stability.
Jon D. Pelletier, Robert G. Hayes, Olivia Hoch, Brendan Fenerty, and Luke A. McGuire
EGUsphere, https://doi.org/10.5194/egusphere-2024-1153, https://doi.org/10.5194/egusphere-2024-1153, 2024
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On the gently sloping landscapes next to mountain fronts, junction angles tend to be lower (more acute), while in bedrock landscapes where the initial landscape or tectonic forcing is likely more spatially variable, junction angles tend to be larger (more obtuse). We demonstrate this using an analysis of ~20 million junction angles for the U.S.A., augmented by analyses of the Loess Plateau, China, and synthetic landscapes.
Julius Reich and Axel Winterscheid
EGUsphere, https://doi.org/10.5194/egusphere-2024-579, https://doi.org/10.5194/egusphere-2024-579, 2024
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Analysing the geometry and the dynamics of riverine bedforms (so-called dunetracking) is important for various fields of application and contributes to a sound and efficient river and sediment management. We developed a new tool, which enables a robust estimation of bedform characteristics and with which comprehensive sensitivity analyses can be carried out. Using a test dataset, we show that the selection of input parameters of dunetracking tools can have a significant impact on the results.
Alexander B. Prescott, Jon D. Pelletier, Satya Chataut, and Sriram Ananthanarayan
EGUsphere, https://doi.org/10.5194/egusphere-2024-1138, https://doi.org/10.5194/egusphere-2024-1138, 2024
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Many Earth surface processes are controlled by the spatial pattern of surface water flow. We review commonly used methods for predicting such spatial patterns in digital landform models and document the pros and cons of commonly used methods. We propose a new method that is designed to minimize those limitations and show that it works well in a variety of test cases.
Prakash Pokhrel, Mikael Attal, Hugh D. Sinclair, Simon M. Mudd, and Mark Naylor
Earth Surf. Dynam., 12, 515–536, https://doi.org/10.5194/esurf-12-515-2024, https://doi.org/10.5194/esurf-12-515-2024, 2024
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Pebbles become increasingly rounded during downstream transport in rivers due to abrasion. This study quantifies pebble roundness along the length of two Himalayan rivers. We demonstrate that roundness increases with downstream distance and that the rates are dependent on rock type. We apply this to reconstructing travel distances and hence the size of ancient Himalaya. Results show that the ancient river network was larger than the modern one, indicating that there has been river capture.
Janbert Aarnink, Tom Beucler, Marceline Vuaridel, and Virginia Ruiz-Villanueva
EGUsphere, https://doi.org/10.5194/egusphere-2024-792, https://doi.org/10.5194/egusphere-2024-792, 2024
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This study presents a novel CNN approach for detecting instream large wood in rivers, addressing the need for flexible monitoring methods that can be used on a variety of data sources. Leveraging a database of 15,228 fully labeled images, our model achieved a 67 % weighted mean average precision. Fine-tuning parameters and sampling techniques offer potential for further performance enhancement of more than 10 % in certain cases, promising valuable insights for ecosystem management.
Orie Cecil, Nicholas Cohn, Matthew Farthing, Sourav Dutta, and Andrew Trautz
EGUsphere, https://doi.org/10.5194/egusphere-2024-855, https://doi.org/10.5194/egusphere-2024-855, 2024
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Using computational fluid dynamics, we analyze the error trends of an analytical shear stress distribution model used to drive aeolian transport for coastal dunes which are an important line of defense against storm related flooding hazards. We find that compared to numerical simulations, the analytical model results in a net overprediction of the landward migration rate. Additionally, two data-driven approaches are proposed for reducing the error while maintaining computational efficiency.
Jens Martin Turowski, Aaron Bufe, and Stefanie Tofelde
Earth Surf. Dynam., 12, 493–514, https://doi.org/10.5194/esurf-12-493-2024, https://doi.org/10.5194/esurf-12-493-2024, 2024
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Fluvial valleys are ubiquitous landforms, and understanding their formation and evolution affects a wide range of disciplines from archaeology and geology to fish biology. Here, we develop a model to predict the width of fluvial valleys for a wide range of geographic conditions. In the model, fluvial valley width is controlled by the two competing factors of lateral channel mobility and uplift. The model complies with available data and yields a broad range of quantitative predictions.
Daniel J. Ciarletta, Jennifer L. Miselis, Julie C. Bernier, and Arnell S. Forde
Earth Surf. Dynam., 12, 449–475, https://doi.org/10.5194/esurf-12-449-2024, https://doi.org/10.5194/esurf-12-449-2024, 2024
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We reconstructed the evolution of Fire Island, a barrier island in New York, USA, to identify drivers of landscape change. Results reveal Fire Island was once divided into multiple inlet-separated islands with distinct features. Later, inlets closed, and Fire Island’s landscape became more uniform as human activities intensified. The island is now less mobile and less likely to resist and recover from storm impacts and sea level rise. This vulnerability may exist for other stabilized barriers.
Chao Zhou, Xibin Tan, Yiduo Liu, and Feng Shi
Earth Surf. Dynam., 12, 433–448, https://doi.org/10.5194/esurf-12-433-2024, https://doi.org/10.5194/esurf-12-433-2024, 2024
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The drainage-divide stability provides new insights into both the river network evolution and the tectonic and/or climatic changes. Several methods have been proposed to determine the direction of drainage-divide migration. However, how to quantify the migration rate of drainage divides remains challenging. In this paper, we propose a new method to calculate the migration rate of drainage divides from high-resolution topographic data.
Moritz Altmann, Madlene Pfeiffer, Florian Haas, Jakob Rom, Fabian Fleischer, Tobias Heckmann, Livia Piermattei, Michael Wimmer, Lukas Braun, Manuel Stark, Sarah Betz-Nutz, and Michael Becht
Earth Surf. Dynam., 12, 399–431, https://doi.org/10.5194/esurf-12-399-2024, https://doi.org/10.5194/esurf-12-399-2024, 2024
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We show a long-term erosion monitoring of several sections on Little Ice Age lateral moraines with derived sediment yield from historical and current digital elevation modelling (DEM)-based differences. The first study period shows a clearly higher range of variability of sediment yield within the sites than the later periods. In most cases, a decreasing trend of geomorphic activity was observed.
Paul A. Carling
Earth Surf. Dynam., 12, 381–397, https://doi.org/10.5194/esurf-12-381-2024, https://doi.org/10.5194/esurf-12-381-2024, 2024
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Edge rounding in Shap granite glacial erratics is an irregular function of distance from the source outcrop in northern England, UK. Block shape is conservative, evolving according to block fracture mechanics – stochastic and silver ratio models – towards either of two attractor states. Progressive reduction in size occurs for blocks transported at the sole of the ice mass where the blocks are subject to compressive and tensile forces of the ice acting against a bedrock or till surface.
Gary Parker, Chenge An, Michael P. Lamb, Marcelo H. Garcia, Elizabeth H. Dingle, and Jeremy G. Venditti
Earth Surf. Dynam., 12, 367–380, https://doi.org/10.5194/esurf-12-367-2024, https://doi.org/10.5194/esurf-12-367-2024, 2024
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River morphology has traditionally been divided by the size 2 mm. We use dimensionless arguments to show that particles in the 1–5 mm range (i) are the finest range not easily suspended by alluvial flood flows, (ii) are transported preferentially over coarser gravel, and (iii), within limits, are also transported preferentially over sand. We show how fluid viscosity mediates the special status of sediment in this range.
Lindsay Marie Capito, Enrico Pandrin, Walter Bertoldi, Nicola Surian, and Simone Bizzi
Earth Surf. Dynam., 12, 321–345, https://doi.org/10.5194/esurf-12-321-2024, https://doi.org/10.5194/esurf-12-321-2024, 2024
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We propose that the pattern of erosion and deposition from repeat topographic surveys can be a proxy for path length in gravel-bed rivers. With laboratory and field data, we applied tools from signal processing to quantify this periodicity and used these path length estimates to calculate sediment transport using the morphological method. Our results highlight the potential to expand the use of the morphological method using only remotely sensed data as well as its limitations.
Caroline Fenske, Jean Braun, François Guillocheau, and Cécile Robin
EGUsphere, https://doi.org/10.5194/egusphere-2024-160, https://doi.org/10.5194/egusphere-2024-160, 2024
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We have developed a new numerical model to represent the formation of ferricretes which are iron-rich, hard layers found in soils and at the surface of the Earth. We assume that the formation mechanism implies variations in the height of the water table and that the hardening rate is proportional to precipitation. The model allows us to quantify the potential feedbacks they generate on the surface topography and the thickness of the regolith/soil layer.
Xuxu Wu, Jonathan Malarkey, Roberto Fernández, Jaco H. Baas, Ellen Pollard, and Daniel R. Parsons
Earth Surf. Dynam., 12, 231–247, https://doi.org/10.5194/esurf-12-231-2024, https://doi.org/10.5194/esurf-12-231-2024, 2024
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The seabed changes from flat to rippled in response to the frictional influence of waves and currents. This experimental study has shown that the speed of this change, the size of ripples that result and even whether ripples appear also depend on the amount of sticky mud present. This new classification on the basis of initial mud content should lead to improvements in models of seabed change in present environments by engineers and the interpretation of past environments by geologists.
Andrea D'Alpaos, Davide Tognin, Laura Tommasini, Luigi D'Alpaos, Andrea Rinaldo, and Luca Carniello
Earth Surf. Dynam., 12, 181–199, https://doi.org/10.5194/esurf-12-181-2024, https://doi.org/10.5194/esurf-12-181-2024, 2024
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Sediment erosion induced by wind waves is one of the main drivers of the morphological evolution of shallow tidal environments. However, a reliable description of erosion events for the long-term morphodynamic modelling of tidal systems is still lacking. By statistically characterizing sediment erosion dynamics in the Venice Lagoon over the last 4 centuries, we set up a novel framework for a synthetic, yet reliable, description of erosion events in tidal systems.
Davide Tognin, Andrea D'Alpaos, Luigi D'Alpaos, Andrea Rinaldo, and Luca Carniello
Earth Surf. Dynam., 12, 201–218, https://doi.org/10.5194/esurf-12-201-2024, https://doi.org/10.5194/esurf-12-201-2024, 2024
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Reliable quantification of sediment transport processes is necessary to understand the fate of shallow tidal environments. Here we present a framework for the description of suspended sediment dynamics to quantify deposition in the long-term modelling of shallow tidal systems. This characterization, together with that of erosion events, allows one to set up synthetic, yet reliable, models for the long-term evolution of tidal landscapes.
Emma L. S. Graf, Hugh D. Sinclair, Mikaël Attal, Boris Gailleton, Basanta Raj Adhikari, and Bishnu Raj Baral
Earth Surf. Dynam., 12, 135–161, https://doi.org/10.5194/esurf-12-135-2024, https://doi.org/10.5194/esurf-12-135-2024, 2024
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Using satellite images, we show that, unlike other examples of earthquake-affected rivers, the rivers of central Nepal experienced little increase in sedimentation following the 2015 Gorkha earthquake. Instead, a catastrophic flood occurred in 2021 that buried towns and agricultural land under up to 10 m of sediment. We show that intense storms remobilised glacial sediment from high elevations causing much a greater impact than flushing of earthquake-induced landslides.
Mohamad Nasr, Adele Johannot, Thomas Geay, Sebastien Zanker, Jules Le Guern, and Alain Recking
Earth Surf. Dynam., 12, 117–134, https://doi.org/10.5194/esurf-12-117-2024, https://doi.org/10.5194/esurf-12-117-2024, 2024
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Hydrophones are used to monitor sediment transport in the river by listening to the acoustic noise generated by particle impacts on the riverbed. However, this acoustic noise is modified by the river flow and can cause misleading information about sediment transport. This article proposes a model that corrects the measured acoustic signal. Testing the model showed that the corrected signal is better correlated with bedload flux in the river.
Byungho Kang, Rusty A. Feagin, Thomas Huff, and Orencio Durán Vinent
Earth Surf. Dynam., 12, 105–115, https://doi.org/10.5194/esurf-12-105-2024, https://doi.org/10.5194/esurf-12-105-2024, 2024
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We provide a detailed characterization of the frequency, intensity and duration of flooding events at a site along the Texas coast. Our analysis demonstrates the suitability of relatively simple wave run-up models to estimate the frequency and intensity of coastal flooding. Our results validate and expand a probabilistic model of coastal flooding driven by wave run-up that can then be used in coastal risk management in response to sea level rise.
Shunsuke Oya, Fumitoshi Imaizumi, and Shoki Takayama
Earth Surf. Dynam., 12, 67–86, https://doi.org/10.5194/esurf-12-67-2024, https://doi.org/10.5194/esurf-12-67-2024, 2024
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The monitoring of pore water pressure in fully and partly saturated debris flows was performed at Ohya landslide scar, central Japan. The pore water pressure in some partly saturated flows greatly exceeded the hydrostatic pressure. The depth gradient of the pore water pressure in the lower part of the flow was generally higher than the upper part of the flow. We conclude that excess pore water pressure is present in many debris flow surges and is an important mechanism in debris flow behavior.
Gabriele Barile, Marco Redolfi, and Marco Tubino
Earth Surf. Dynam., 12, 87–103, https://doi.org/10.5194/esurf-12-87-2024, https://doi.org/10.5194/esurf-12-87-2024, 2024
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River bifurcations often show the closure of one branch (avulsion), whose causes are still poorly understood. Our model shows that when one branch stops transporting sediments, the other considerably erodes and captures much more flow, resulting in a self-sustaining process. This phenomenon intensifies when increasing the length of the branches, eventually leading to branch closure. This work may help to understand when avulsions occur and thus to design sustainable river restoration projects.
Cited articles
Abu Ghazleh, S. and Kempe, S.: Geomorphology of Lake Lisan terraces along
the eastern coast of the Dead Sea, Jordan, Geomorphology, 108, 246–263,
https://doi.org/10.1016/j.geomorph.2009.02.015, 2009.
Ahlborn, M., Armon, M., Ben Dor, Y., Neugebauer, I., Schwab, M. J., Tjallingii, R., Shoqeir, J. H., Morin, E., Enzel, Y., and Brauer, A.: Increased frequency of torrential rainstorms during a regional late Holocene
eastern Mediterranean drought, Quatern. Res., 89, 425–431,
https://doi.org/10.1017/qua.2018.9, 2018.
Alpert, P. and Shay-El, Y.: The moisture source for the winter cyclones in
the EM, Isr. Meteorol. Res. Pap., 5, 20–27, 1994.
Alpert, P. and Ziv, B.: The Sharav Cyclone: Observations and some theoretical considerations, J. Geophys. Res., 94, 18495, https://doi.org/10.1029/JD094iD15p18495, 1989.
Alpert, P., Neeman, B. U., and Shay-El, Y.: Climatological analysis of
Mediterranean cyclones using ECMWF data, Tellus A, 42, 65–77, https://doi.org/10.3402/tellusa.v42i1.11860, 1990a.
Alpert, P., Abramsky, R., and Neeman, B. U.: The prevailing summer synoptic
system in Israel – subtropical high, not Persian trough, Isr. J. Earth Sci.,
39, 93–102, 1990b.
Alpert, P., Shafir, H., and Issahary, D.: Recent changes in the climate at
the Dead Sea – a preliminary study, Climatic Change, 37, 513–537,
https://doi.org/10.1023/A:1005330908974, 1997.
Alpert, P., Osetinsky, I., Ziv, B., and Shafir, H.: A new seasons definition
based on classified daily synoptic systems: an example for the eastern
Mediterranean, Int. J. Climatol., 24, 1013–1021, https://doi.org/10.1002/joc.1037, 2004a.
Alpert, P., Osetinsky, I., Ziv, B., and Shafir, H.: Semi-objective classification for daily synoptic systems: application to the eastern
Mediterranean climate change, Int. J. Climatol., 24, 1001–1011,
https://doi.org/10.1002/joc.1036, 2004b.
Amit, R. and Gerson, R.: The evolution of holocene reg (gravelly) soils in
deserts: An example from the dead sea region, Catena, 13, 59–79,
https://doi.org/10.1016/S0341-8162(86)80005-4, 1986.
Anderson, J. B., Wallace, D. J., Simms, A. R., Rodriguez, A. B., Weight, R.
W. R., and Taha, Z. P.: Recycling sediments between source and sink during a
eustatic cycle: Systems of late Quaternary northwestern Gulf of Mexico Basin, Earth-Sci. Rev., 153, 111–138, https://doi.org/10.1016/j.earscirev.2015.10.014, 2016.
Arbel, S., Getker, M., Arazi, A., Yosi, B., Moshe, G., Efraim, F., and Alon,
M.: Data of rain and floods of exceptional events in the hydrological year
2006–2007, special report M-84, Ministry of Agriculture and Rural Development, Israel, https://www.gov.il/BlobFolder/dynamiccollectorresultitem/sers-2009-1-m-84/he/water-and-soil_Hydrological-book_sers_2009_1_M-84.pdf (last access: 2 July 2023), 2009.
Armon, M., Dente, E., Smith, J. A., Enzel, Y., and Morin, E.: Synoptic-Scale
Control over Modern Rainfall and Flood Patterns in the Levant Drylands with
Implications for Past Climates, J. Hydrometeorol., 19, 1077–1096,
https://doi.org/10.1175/JHM-D-18-0013.1, 2018.
Armon, M., Morin, E., and Enzel, Y.: Overview of modern atmospheric patterns
controlling rainfall and floods into the Dead Sea: Implications for the lake's sedimentology and paleohydrology, Quaternary Sci. Rev., 216, 58–73,
https://doi.org/10.1016/j.quascirev.2019.06.005, 2019.
Armon, M., Marra, F., Enzel, Y., Rostkier-Edelstein, D., and Morin, E.:
Radar-based characterisation of heavy precipitation in the eastern Mediterranean and its representation in a convection-permitting model,
Hydrol. Earth Syst. Sci., 24, 1227–1249, https://doi.org/10.5194/hess-24-1227-2020, 2020.
Armon, M., Marra, F., Enzel, Y., Rostkier-Edelstein, D., Garfinkel, C. I.,
Adam, O., Dayan, U., and Morin, E.: Reduced Rainfall in Future Heavy Precipitation Events Related to Contracted Rain Area Despite Increased Rain
Rate, Earth's Future, 10, e2021EF002397, https://doi.org/10.1029/2021EF002397, 2022.
Ashton, A. D. and Giosan, L.: Wave-angle control of delta evolution, Geophys. Res. Lett., 38, L13405, https://doi.org/10.1029/2011GL047630, 2011.
Ashton, A. D., Hutton, E. W. H., Kettner, A. J., Xing, F., Kallumadikal, J.,
Nienhuis, J., and Giosan, L.: Progress in coupling models of coastline and
fluvial dynamics, Comput. Geosci., 53, 21–29, https://doi.org/10.1016/j.cageo.2012.04.004, 2013.
Bárdossy, A. and Filiz, F.: Identification of flood producing atmospheric circulation patterns, J. Hydrol., 313, 48–57, https://doi.org/10.1016/j.jhydrol.2005.02.006, 2005.
Bartov, Y., Stein, M., Enzel, Y., Agnon, A., and Reches, Z.: Lake Levels and
Sequence Stratigraphy of Lake Lisan, the Late Pleistocene Precursor of the
Dead Sea, Quatern. Res., 57, 9–21, https://doi.org/10.1006/qres.2001.2284, 2002.
Bartov, Y., Goldstein, S. L., Stein, M., and Enzel, Y.: Catastrophic arid
episodes in the Eastern Mediterranean linked with the North Atlantic Heinrich events, Geology, 31, 439, https://doi.org/10.1130/0091-7613(2003)031<0439:CAEITE>2.0.CO;2, 2003.
Bartov, Y., Bookman, R., and Enzel, Y.: Current depositional environments at
the Dead Sea margins as indicators of past lake levels, in: New Frontiers in
Dead Sea Paleoenvironmental Research, vol. 401, Geological Society of
America, 127–140, https://doi.org/10.1130/2006.2401(08), 2006.
Bartov, Y., Enzel, Y., Porat, N., and Stein, M.: Evolution of the Late
Pleistocene Holocene Dead Sea Basin from Sequence Statigraphy of Fan Deltas
and Lake-Level Reconstruction, J. Sediment. Res., 77, 680–692,
https://doi.org/10.2110/jsr.2007.070, 2007.
Belachsen, I., Marra, F., Peleg, N., and Morin, E.: Convective rainfall in a
dry climate: relations with synoptic systems and flash-flood generation in
the Dead Sea region, Hydrol. Earth Syst. Sci., 21, 5165–5180,
https://doi.org/10.5194/hess-21-5165-2017, 2017.
Ben Dor, Y., Armon, M., Ahlborn, M., Morin, E., Erel, Y., Brauer, A., Schwab, M. J., Tjallingii, R., and Enzel, Y.: Changing flood frequencies under opposing late Pleistocene eastern Mediterranean climates, Sci. Rep., 8, 8445, https://doi.org/10.1038/s41598-018-25969-6, 2018.
Benelli, G., Pozzebon, A., Bertoni, D., and Sarti, G.: An RFID-Based Toolbox
for the Study of Under- and Outside-Water Movement of Pebbles on
Coarse-Grained Beaches, IEEE J. Select. Top. Appl. Earth Obs. Remote Sens., 5, 1474–1482, https://doi.org/10.1109/JSTARS.2012.2196499, 2012.
Ben Moshe, L., Haviv, I., Enzel, Y., Zilberman, E., and Matmon, A.: Incision
of alluvial channels in response to a continuous base level fall: Field
characterization, modeling, and validation along the Dead Sea, Geomorphology, 93, 524–536, https://doi.org/10.1016/j.geomorph.2007.03.014, 2008.
Bitan, A.: The wind regime in the north-west section of the Dead-Sea, Arch.
für Meteorol. Geophys. und Bioklimatologie Ser. B, 22, 313–335,
https://doi.org/10.1007/BF02246585, 1974.
Bitan, A.: The influence of the special shape of the dead-sea and its environment on the local wind system, Arch. für Meteorol. Geophys. und
Bioklimatologie Ser. B, 24, 283–301, https://doi.org/10.1007/BF02263460, 1976.
Blum, M. D. and Hattier-Womack, J.: Climate Change, Sea-Level Change, and
Fluvial Sediment Supply to Deepwater Depositional Systems, in: External Controls of Deep-Water Depositional Systems, SEPM – Society for Sedimentary
Geology, 15–39, https://doi.org/10.2110/sepmsp.092.015, 2009.
Blum, M. D., Martin, J., Milliken, K., and Garvin, M.: Paleovalley systems:
Insights from Quaternary analogs and experiments, Earth-Sci. Rev., 116, 128–169, https://doi.org/10.1016/j.earscirev.2012.09.003, 2013.
Bookman, R., Enzel, Y., Agnon, A., and Stein, M.: Late Holocene lake levels of the Dead Sea, Geol. Soc. Am. Bull., 116, 555–571, https://doi.org/10.1130/B25286.1, 2004.
Bookman, R., Bartov, Y., Enzel, Y., and Stein, M.: Quaternary lake levels in
the Dead Sea basin: two centuries of research, Geol. Soc. Am. Spacial Pap.,
401, 155–170, https://doi.org/10.1130/2006.2401(10), 2006.
Borga, M., Comiti, F., Ruin, I., and Marra, F.: Forensic analysis of flash
flood response, WIREs Water, 6, e1338, https://doi.org/10.1002/wat2.1338, 2019.
Bowman, D.: Geomorphology of the shore terraces of the late pleistocene Lisan lake (Israel), Palaeogeogr. Palaeoclimatol. Palaeoecol., 9, 183–209,
https://doi.org/10.1016/0031-0182(71)90031-9, 1971.
Bowman, D.: The Regional Approach: Alluvial Fans along the Dead Sea-Arava
Rift Valley, in: Principles of Alluvial Fan Morphology, Springer Netherlands, Dordrecht, 135–151, https://doi.org/10.1007/978-94-024-1558-2_19, 2019.
Bowman, D. and Gross, T.: The highest stand of Lake Lisan: ∼150 meter
below MSL, Isr. J. Earth Sci., 41, 233–237, 1992.
Bowman, D., Banet-Davidovich, D., Bruins, H. J., and Van der Plicht, J.:
Dead Sea shoreline facies with seismically-induced soft-sediment deformation
structures, Israel, Isr. J. Earth Sci., 49, 197–214,
https://doi.org/10.1560/GXHT-AK5W-46EF-VTR8, 2000.
Bowman, D., Svoray, T., Devora, S., Shapira, I., and Laronne, J. B.: Geomorphology Extreme rates of channel incision and shape evolution in
response to a continuous, rapid base-level fall, the Dead Sea, Israel,
Geomorphology, 114, 227–237, https://doi.org/10.1016/j.geomorph.2009.07.004, 2010.
Bridge, J. S.: The interaction between channel geometry, water flow, sediment transport and deposition in braided rivers, Geol. Soc. Lond. Spec. Publ., 75, 13–71, https://doi.org/10.1144/GSL.SP.1993.075.01.02, 1993.
Burgess, P. M. and Hovius, N.: Rates of delta progradation during highstands: consequences for timing of deposition in deep-marine systems, J. Geol. Soc. Lond., 155, 217–222, https://doi.org/10.1144/gsjgs.155.2.0217, 1998.
CDS: https://cds.climate.copernicus.eu (last access: 1 October 2022), 2022.
Coleman, J. M. and Prior, D. B.: Deltaic environments of deposition, in: M 31: Sandstone Depositional Environments, AAPG Special Volumes, 139–178,
1982.
David-Novak, H. B., Morin, E., and Enzel, Y.: Modern extreme storms and the rainfall thresholds for initiating debris flows on the hyperarid western
escarpment of the Dead Sea, Israel, Geol. Soc. Am. Bull., 116, 718–728, https://doi.org/10.1130/B25403.2, 2004.
Dayan, U. and Morin, E.: Flash flood-producing rainstorms over the Dead Sea: A review, in: New Frontiers in Dead Sea Paleoenvironmental Research, vol. 401, Geological Society of America, 53–62, https://doi.org/10.1130/2006.2401(04), 2006.
Dayan, U., Ricaud, P., Zbinden, R., and Dulac, F.: Atmospheric pollution over the eastern Mediterranean during summer – a review, Atmos. Chem. Phys., 17, 13233–13263, https://doi.org/10.5194/acp-17-13233-2017, 2017.
Dayan, U., Lensky, I. M., Ziv, B., and Khain, P.: Atmospheric conditions leading to an exceptional fatal flash flood in the Negev Desert, Israel, Nat. Hazards Earth Syst. Sci., 21, 1583–1597, https://doi.org/10.5194/nhess-21-1583-2021, 2021.
Dente, E., Lensky, N. G., Morin, E., Grodek, T., Sheffer, N. A., and Enzel, Y.: Geomorphic Response of a Low-Gradient Channel to Modern, Progressive
Base-Level Lowering: Nahal HaArava, the Dead Sea, J. Geophys. Res.-Earth, 122, 2468–2487, https://doi.org/10.1002/2016JF004081, 2017.
Dente, E., Lensky, N. G., Morin, E., Dunne, T., and Enzel, Y.: Sinuosity
evolution along an incising channel: New insights from the Jordan River response to the Dead Sea level fall, Earth Surf. Proc. Land., 44, 781–795, https://doi.org/10.1002/esp.4530, 2018.
Dente, E., Lensky, N. G., Morin, E., and Enzel, Y.: From straight to deeply
incised meandering channels: Slope impact on sinuosity of confined streams,
Earth Surf. Process. Land., 46, 1041–1054, https://doi.org/10.1002/esp.5085, 2021.
Desert Floods Research Center: https://floods.org.il/english/ (last access: 1 October 2022), 2022.
de Vries, A. J., Tyrlis, E., Edry, D., Krichak, S. O., Steil, B., and Lelieveld, J.: Extreme precipitation events in the Middle East: Dynamics of
the Active Red Sea Trough, J. Geophys. Res.-Atmos., 118, 7087–7108,
https://doi.org/10.1002/jgrd.50569, 2013.
Elliot, T.: Deltas, edited by: Reading, H., Oxford, 113–154, http://geoweb.uwyo.edu/geol2100/Deltas.pdf (last access: 2 July 2023), 1986.
Enzel, Y. and Bar-Yosef, O. (Eds.): Quaternary of the Levant, Cambridge University Press, https://doi.org/10.1017/9781316106754, 2017.
Enzel, Y., Bookman, R., Sharon, D., Gvirtzman, H., Dayan, U., Ziv, B., and
Stein, M.: Late Holocene climates of the Near East deduced from Dead Sea level variations and modern regional winter rainfall, Quatern. Res., 60,
263–273, https://doi.org/10.1016/j.yqres.2003.07.011, 2003.
Enzel, Y., Agnon, A., and Stein, M.: New Frontiers in Dead Sea Paleoenvironmental Research, Geological Society of America, https://doi.org/10.1130/SPE401, 2006.
Enzel, Y., Amit, R., Dayan, U., Crouvi, O., Kahana, R., Ziv, B., and Sharon,
D.: The climatic and physiographic controls of the eastern Mediterranean over the late Pleistocene climates in the southern Levant and its neighboring deserts, Global Planet. Change, 60, 165–192, https://doi.org/10.1016/j.gloplacha.2007.02.003, 2008.
Enzel, Y., Mushkin, A., Groisman, M., Calvo, R., Eyal, H., and Lensky, N.:
The modern wave-induced coastal staircase morphology along the western shores of the Dead Sea, Geomorphology, 408, 108237, https://doi.org/10.1016/j.geomorph.2022.108237, 2022.
Eyal, H.: Nahal Og beach – the 25.12.2019 largest storm wave, TIB-AV-Portal [video supplement], https://doi.org/10.5446/59268, 2023a.
Eyal, H.: Nahal Og – the 28.2.2019 flash flood, TIB-AV-Portal [video supplement], https://doi.org/10.5446/59269, 2023b.
Eyal, H.: Air flow circulation over the Dead Sea under Mediterranean cyclones indicated by the movement of clouds, TIB-AV-Portal [video supplement], https://doi.org/10.5446/59267, 2023c.
Eyal, H., Dente, E., Haviv, I., Enzel, Y., Dunne, T., and Lensky, N. G.: Fluvial incision and coarse gravel redistribution across the modern Dead Sea
shelf as a result of base-level fall, Earth Surf. Process. Land., 44, 2170–2185, https://doi.org/10.1002/esp.4640, 2019.
Eyal, H., Enzel, Y., Meiburg, E., Vowinckel, B., and Lensky, N. G.: How Does
Coastal Gravel Get Sorted Under Stormy Longshore Transport?, Geophys. Res.
Lett., 48, e2021GL095082, https://doi.org/10.1029/2021GL095082, 2021.
Eyal, H., Armon, M., Enzel, Y., and Lensky, N. G.: Synoptic- to meso-scale
circulation connects fluvial and coastal gravel conveyors and directional
deposition of coastal landforms in the Dead Sea basin, V1, Mendeley Data [data set], https://doi.org/10.17632/65bhpwftrh.1, 2022.
Fagherazzi, S., Howard, A. D., and Wiberg, P. L.: Modeling fluvial erosion and deposition on continental shelves during sea level cycles, J. Geophys. Res., 109, F03010, https://doi.org/10.1029/2003JF000091, 2004.
Frostick, L. E. and Reid, I. A. N.: Climatic versus tectonic controls of fan
sequences: lessons from the Dead Sea, Israel, J. Geol. Soc. Lond., 146,
527–538, https://doi.org/10.1144/gsjgs.146.3.0527, 1989.
Galloway, W. E.: Process framework for describing the morphologic and stratigraphic evolution of deltaic depositional systems, 87–98, https://archives.datapages.com/data/hgssp/data/022/022001/87_hgs0220087.htm
(last access: 2 July 2023), 1975.
Garfunkel, Z. and Ben-Avraham, Z.: The structure of the Dead Sea basin,
Tectonophysics, 266, 155–176, https://doi.org/10.1016/S0040-1951(96)00188-6, 1996.
Gertman, I. and Hecht, A.: The Dead Sea hydrography from 1992 to 2000, J.
Mar. Syst., 35, 169–181, https://doi.org/10.1016/S0924-7963(02)00079-9, 2002.
Goldreich, Y.: The spatial distribution of annual rainfall in Israel? a review, Theor. Appl. Climatol., 50, 45–59, https://doi.org/10.1007/BF00864902, 1994.
Goldreich, Y.: The Climate of Israel, Springer US, Boston, MA,
https://doi.org/10.1007/978-1-4615-0697-3, 2003.
Goldreich, Y., Mozes, H., and Rosenfeld, D.: Radar analysis of cloud systems
and their rainfall yield in Israel, Isr. J. Earth Sci., 53, 63–76, 2004.
Goodwin, I. D., Mortlock, T. R., and Browning, S.: Tropical and extratropical-origin storm wave types and their influence on the East Australian longshore sand transport system under a changing climate, J.
Geophys. Res.-Oceans, 121, 4833–4853, https://doi.org/10.1002/2016JC011769, 2016.
Graf, M., Sprenger, M., Lohmann, U., Seibt, C., and Hofmann, H.: Evaluating
the suitability of the SWAN/COSMO-2 model system to simulate short-crested
surface waves for a narrow lake with complex bathymetry, Meteorol. Z., 22, 257–272, https://doi.org/10.1127/0941-2948/2013/0442, 2013.
Grosse, G., Schirrmeister, L., Kunitsky, V. V., and Hubberten, H.: The use of
CORONA images in remote sensing of periglacial geomorphology: an illustration from the NE Siberian coast, Permafrost. Periglac. Process., 16, 163–172, https://doi.org/10.1002/ppp.509, 2005.
Grottoli, E., Bertoni, D., Ciavola, P., and Pozzebon, A.: Short term displacements of marked pebbles in the swash zone: Focus on particle shape
and size, Mar. Geol., 367, 143–158, https://doi.org/10.1016/j.margeo.2015.06.006, 2015.
Hamdani, I., Assouline, S., Tanny, J., Lensky, I. M., Gertman, I., Mor, Z.,
and Lensky, N. G.: Seasonal and diurnal evaporation from a deep hypersaline
lake: The Dead Sea as a case study, J. Hydrol., 562, 155–167,
https://doi.org/10.1016/j.jhydrol.2018.04.057, 2018.
Hansford, M. R. and Plink-Björklund, P.: River discharge variability as
the link between climate and fluvial fan formation, Geology, 48, 952–956,
https://doi.org/10.1130/G47471.1, 2020.
Haviv, I.: Mechanics, morphology and evolution of vertical knickpoints
(waterfalls) along the bedrock channels of the Dead Sea western tectonic
escarpment, PhD thesis, The Hebrew University of Jerusalem, https://huji.primo.exlibrisgroup.com/permalink/972HUJI_INST/10ptda2/alma990014406120203701
(last access: 2 July 2023), 2007.
Hersbach, H., Bell, B., Berrisford, P., Hirahara, S., Horányi, A.,
Muñoz-Sabater, J., Nicolas, J., Peubey, C., Radu, R., Schepers, D.,
Simmons, A., Soci, C., Abdalla, S., Abellan, X., Balsamo, G., Bechtold, P.,
Biavati, G., Bidlot, J., Bonavita, M., Chiara, G., Dahlgren, P., Dee, D.,
Diamantakis, M., Dragani, R., Flemming, J., Forbes, R., Fuentes, M., Geer,
A., Haimberger, L., Healy, S., Hogan, R. J., Hólm, E., Janisková,
M., Keeley, S., Laloyaux, P., Lopez, P., Lupu, C., Radnoti, G., Rosnay, P.,
Rozum, I., Vamborg, F., Villaume, S., and Thépaut, J.: The ERA5 global
reanalysis, Q. J. Roy. Meteorol. Soc., 146, 1999–2049, https://doi.org/10.1002/qj.3803, 2020.
Hochman, A., Mercogliano, P., Alpert, P., Saaroni, H., and Bucchignani, E.:
High-resolution projection of climate change and extremity over Israel using
COSMO-CLM, Int. J. Climatol., 38, 5095–5106, https://doi.org/10.1002/joc.5714, 2018.
Huntington, E.: Palestine and its Transformation, Houghton, Mifflin and Company, Boston, https://www.loc.gov/item/unk82080191/ (last access: 2 July 2023), 1911.
IMS – Israel Meteorological Service: http://www.ims.gov.il (last access: 1 October 2022), 2022.
Kahana, R., Ziv, B., Enzel, Y., and Dayan, U.: Synoptic climatology of major
floods in the Negev Desert, Israel, Int. J. Climatol., 22, 867–882,
https://doi.org/10.1002/joc.766, 2002.
Karimpour, A. and Chen, Q.: Wind wave analysis in depth limited water using
OCEANLYZ, A MATLAB toolbox, Comput. Geosci., 106, 181–189,
https://doi.org/10.1016/j.cageo.2017.06.010, 2017.
Kiro, Y., Goldstein, S. L., Garcia-Veigas, J., Levy, E., Kushnir, Y., Stein,
M., and Lazar, B.: Relationships between lake-level changes and water and
salt budgets in the Dead Sea during extreme aridities in the Eastern Mediterranean, Earth Planet. Sc. Lett., 464, 211–226,
https://doi.org/10.1016/j.epsl.2017.01.043, 2017.
Kunin, P., Alpert, P., and Rostkier-Edelstein, D.: Investigation of sea-breeze/foehn in the Dead Sea valley employing high resolution WRF and
observations, Atmos. Res., 229, 240–254, https://doi.org/10.1016/j.atmosres.2019.06.012, 2019.
Kushnir, Y., Dayan, U., Ziv, B., Morin, E., and Enzel, Y.: Climate of the
Levant, in: Quaternary of the Levant, Cambridge University Press, 31–44,
https://doi.org/10.1017/9781316106754.004, 2017.
Lekach, J. and Enzel, Y.: Flood-duration-integrated stream power and
frequency magnitude of >50-year-long sediment discharge out of a hyperarid watershed, Earth Surf. Process. Land., 46, 1348–1362, https://doi.org/10.1002/esp.5104, 2021.
Lensky, I. M. and Dayan, U.: Continuous detection and characterization of
the Sea Breeze in clear sky conditions using Meteosat Second Generation, Atmos. Chem. Phys., 12, 6505–6513, https://doi.org/10.5194/acp-12-6505-2012, 2012.
Lensky, I. M. and Dayan, U.: Satellite observations of land surface temperature patterns induced by synoptic circulation, Int. J. Climatol., 35,
189–195, https://doi.org/10.1002/joc.3971, 2015.
Lensky, N. G., Dvorkin, Y., Lyakhovsky, V., Gertman, I., and Gavrieli, I.:
Water, salt, and energy balances of the Dead Sea, Water Resour. Res., 41,
1–13, https://doi.org/10.1029/2005WR004084, 2005.
Lensky, N. G., Lensky, I. M., Peretz, A., Gertman, I., Tanny, J., and Assouline, S.: Diurnal Course of Evaporation From the Dead Sea in Summer: A
Distinct Double Peak Induced by Solar Radiation and Night Sea Breeze, Water
Resour. Res., 54, 150–160, https://doi.org/10.1002/2017WR021536, 2018.
Longuet-Higgins, M. S.: Longshore currents generated by obliquely incident
sea waves: 1, J. Geophys. Res., 75, 6778–6789, 1970.
Manspeizer, W.: The Dead Sea Rift: Impact of climate and tectonism on Pleistocene and Holocene sedimentation, SEPM, https://archives.datapages.com/data/sepm_sp/SP37/The_Dead_Sea_Rift.htm
(last access: 2 July 2023), 1985.
Marra, F. and Morin, E.: Autocorrelation structure of convective rainfall in
semiarid-arid climate derived from high-resolution X-Band radar estimates,
Atmos. Res., 200, 126–138, https://doi.org/10.1016/j.atmosres.2017.09.020, 2018.
Marra, F., Borga, M., and Morin, E.: A Unified Framework for Extreme Subdaily Precipitation Frequency Analyses Based on Ordinary Events, Geophys. Res. Lett., 47, e2020GL090209, https://doi.org/10.1029/2020GL090209, 2020.
Marra, F., Armon, M., Adam, O., Zoccatelli, D., Gazal, O., Garfinkel, C. I.,
Rostkier-Edelstein, D., Dayan, U., Enzel, Y., and Morin, E.: Toward Narrowing Uncertainty in Future Projections of Local Extreme Precipitation, Geophys. Res. Lett., 48, e2020GL091823, https://doi.org/10.1029/2020GL091823, 2021.
Marra, F., Armon, M., and Morin, E.: Coastal and orographic effects on extreme precipitation revealed by weather radar observations, Hydrol. Earth
Syst. Sci., 26, 1439–1458, https://doi.org/10.5194/hess-26-1439-2022, 2022.
Masselink, G., Scott, T., Poate, T., Stokes, C., Wiggins, M., Valiente, N.,
and Konstantinou, A.: Tale of two beaches: correlation between decadal beach
dynamics and climate indices, in: Coastal Sediments 2023: The Proceedings of
the Coastal Sediments 2023, World Scientific, 337–350,
https://doi.org/10.1142/9789811275135_0031, 2023.
Meadows, G. A., Meadows, L. A., Wood, W. L., Hubertz, J. M., and Perlin, M.:
The Relationship between Great Lakes Water Levels, Wave Energies, and
Shoreline Damage, B. Am. Meteorol. Soc., 78, 675–682,
https://doi.org/10.1175/1520-0477(1997)078<0675:TRBGLW>2.0.CO;2, 1997.
Merz, B., Blöschl, G., Vorogushyn, S., Dottori, F., Aerts, J. C. J. H.,
Bates, P., Bertola, M., Kemter, M., Kreibich, H., Lall, U., and Macdonald,
E.: Causes, impacts and patterns of disastrous river floods, Nat. Rev. Earth
Environ., 2, 592–609, https://doi.org/10.1038/s43017-021-00195-3, 2021.
Meyer-Peter, E. and Müller, R.: Formulas for bed-load transport, in:
appendix 2, IAHSR 2nd meeting, 7 June 1948, Stockholm, http://resolver.tudelft.nl/uuid:4fda9b61-be28-4703-ab06-43cdc2a21bd7 (last access: 2 July 2023), 1948.
Molina, R., Manno, G., Lo Re, C., Anfuso, G., and Ciraolo, G.: Storm Energy
Flux Characterization along the Mediterranean Coast of Andalusia (Spain),
Water, 11, 509, https://doi.org/10.3390/w11030509, 2019.
Montgomery, D. R. and Buffington, J. M.: Channel-reach morphology in mountain drainage basins, Bull. Geol. Soc. Am., 109, 596–611,
https://doi.org/10.1130/0016-7606(1997)109<0596:CRMIMD>2.3.CO;2, 1997.
Morin, E., Jacoby, Y., Navon, S., and Bet-Halachmi, E.: Towards flash-flood
prediction in the dry Dead Sea region utilizing radar rainfall information,
Adv. Water Resour., 32, 1066–1076, https://doi.org/10.1016/j.advwatres.2008.11.011, 2009.
Mulder, T. and Syvitski, J. P. M.: Climatic and Morphologic Relationships of
Rivers: Implications of Sea-Level Fluctuations on River Loads, J. Geol., 104, 509–523, https://doi.org/10.1086/629849, 1996.
Naor, R., Potchter, O., Shafir, H., and Alpert, P.: An observational study
of the summer Mediterranean Sea breeze front penetration into the complex
topography of the Jordan Rift Valley, Theor. Appl. Climatol., 127, 275–284,
https://doi.org/10.1007/s00704-015-1635-3, 2017.
Neev, D. and Emery, K. O.: The Dead Sea: depositional processes and environments of evaporites, Israel Geological Survey Bulletin, 41, p. 147, 1967.
Neugebauer, I., Schwab, M. J., Waldmann, N. D., Tjallingii, R., Frank, U.,
Hadzhiivanova, E., Naumann, R., Taha, N., Agnon, A., Enzel, Y., and Brauer, A.: Hydroclimatic variability in the Levant during the early last glacial
(∼117–75 ka) derived from micro-facies analyses of deep Dead Sea
sediments, Clim. Past, 12, 75–90, https://doi.org/10.5194/cp-12-75-2016, 2016.
Nienhuis, J. H., Ashton, A. D., and Giosan, L.: What makes a delta wave-dominated?, Geology, 43, 511–514, https://doi.org/10.1130/G36518.1, 2015.
Nienhuis, J. H., Ashton, A. D., and Giosan, L.: Littoral steering of deltaic
channels, Earth Planet. Sc. Lett., 453, 204–214, https://doi.org/10.1016/j.epsl.2016.08.018, 2016.
Palchan, D., Neugebauer, I., Amitai, Y., Waldmann, N. D., Schwab, M. J., Dulski, P., Brauer, A., Stein, M., Erel, Y., and Enzel, Y.: North Atlantic
controlled depositional cycles in MIS 5e layered sediments from the deep Dead Sea basin, Quatern. Res., 87, 168–179, https://doi.org/10.1017/qua.2016.10, 2017.
Postma, G.: An analysis of the variation in delta architecture, Terra Nova,
2, 124–130, https://doi.org/10.1111/j.1365-3121.1990.tb00052.x, 1990.
Postma, G.: Sea-level-related architectural trends in coarse-grained delta
complexes, Sediment. Geol., 98, 3–12, https://doi.org/10.1016/0037-0738(95)00024-3, 1995.
Pringle, J. and Stretch, D. D.: On a new statistical wave generator based on
atmospheric circulation patterns and its applications to coastal shoreline
evolution, Comput. Geosci., 149, 104707, https://doi.org/10.1016/j.cageo.2021.104707, 2021.
Pringle, J., Stretch, D. D., and Bárdossy, A.: Automated classification
of the atmospheric circulation patterns that drive regional wave climates,
Nat. Hazards Earth Syst. Sci., 14, 2145–2155, https://doi.org/10.5194/nhess-14-2145-2014, 2014.
Pringle, J., Stretch, D. D., and Bárdossy, A.: On linking atmospheric
circulation patterns to extreme wave events for coastal vulnerability assessments, Nat. Hazards, 79, 45–59, https://doi.org/10.1007/s11069-015-1825-4, 2015.
Reid, I., Frostick, L. E., and Layman, J. T.: The incidence and nature of
bedload transport during flood flows in coarse-grained alluvial channels,
Earth Surf. Process. Land., 10, 33–44, https://doi.org/10.1002/esp.3290100107, 1985.
Rinat, Y., Marra, F., Armon, M., Metzger, A., Levi, Y., Khain, P., Vadislavsky, E., Rosensaft, M., and Morin, E.: Hydrometeorological analysis
and forecasting of a 3 d flash-flood-triggering desert rainstorm, Nat.
Hazards Earth Syst. Sci., 21, 917–939, https://doi.org/10.5194/nhess-21-917-2021, 2021.
Rodwell, M. J. and Hoskins, B. J.: Monsoons and the dynamics of deserts, Q.
J. Roy. Meteorol. Soc., 122, 1385–1404, https://doi.org/10.1002/qj.49712253408, 1996.
Saaroni, H., Ziv, B., Bitan, A., and Alpert, P.: Easterly Wind Storms over
Israel, Theor. Appl. Climatol., 59, 61–77, https://doi.org/10.1007/s007040050013, 1998.
Saaroni, H., Halfon, N., Ziv, B., Alpert, P., and Kutiel, H.: Links between
the rainfall regime in Israel and location and intensity of Cyprus lows, Int. J. Climatol., 30, 1014–1025, https://doi.org/10.1002/joc.1912, 2010.
Segal, M., Mahrer, Y., and Pielke, R. A.: A study of meteorological patterns
associated with a lake confined by mountains – the Dead Sea case, Q. J. Roy.
Meteorol. Soc., 109, 549–564, 1983.
Sharon, D.: The spottiness of rainfall in a desert area, J. Hydrol., 17,
161–175, https://doi.org/10.1016/0022-1694(72)90002-9, 1972.
Sharon, D. and Kutiel, H.: The distribution of rainfall intensity in Israel,
its regional and seasonal variations and its climatological evaluation, J.
Climatol., 6, 277–291, https://doi.org/10.1002/joc.3370060304, 1986.
Shentsis, I., Laronne, J. B., and Alpert, P.: Red Sea Trough flood events in
the Negev, Israel (1964–2007), Hydrolog. Sci. J., 57, 42–51, https://doi.org/10.1080/02626667.2011.636922, 2012.
Shohami, D., Dayan, U., and Morin, E.: Warming and drying of the eastern
Mediterranean: Additional evidence from trend analysis, J. Geophys. Res.-Atmos., 116, D22101, https://doi.org/10.1029/2011JD016004, 2011.
Sirota, I., Enzel, Y., Mor, Z., Ben Moshe, L., Eyal, H., Lowenstein, T. K.,
and Lensky, N. G.: Sedimentology and stratigraphy of a modern halite sequence formed under Dead Sea level fall, Sedimentology, 68, 1069–1090,
https://doi.org/10.1111/sed.12814, 2021.
Solari, S. and Alonso, R.: A New Methodology for Extreme Waves Analysis
Based on Weather-Patterns Classification Methods, Coast. Eng. Proc., 35, 23, https://doi.org/10.9753/icce.v35.waves.23, 2017.
Steirou, E., Gerlitz, L., Apel, H., and Merz, B.: Links between large-scale
circulation patterns and streamflow in Central Europe: A review, J. Hydrol.,
549, 484–500, 2017.
Syvitski, J. P. M. and Milliman, J. D.: Geology, Geography, and Humans Battle for Dominance over the Delivery of Fluvial Sediment to the Coastal Ocean, J. Geol., 115, 1–19, https://doi.org/10.1086/509246, 2007.
Syvitski, J. P. M., Kettner, A. J., Overeem, I., Hutton, E. W. H., Hannon,
M. T., Brakenridge, G. R., Day, J., Vörösmarty, C., Saito, Y., Giosan, L., and Nicholls, R. J.: Sinking deltas due to human activities, Nat. Geosci., 2, 681–686, https://doi.org/10.1038/ngeo629, 2009.
Torfstein, A. and Enzel, Y.: Dead Sea lake level changes and Levant palaeoclimate, Quat. Levant, 115–126, https://doi.org/10.1017/9781316106754.013, 2017.
Torfstein, A., Goldstein, S. L., Stein, M., and Enzel, Y.: Impacts of abrupt
climate changes in the Levant from Last Glacial Dead Sea levels, Quaternary Sci. Rev., 69, 1–7, https://doi.org/10.1016/j.quascirev.2013.02.015, 2013.
Torfstein, A., Goldstein, S. L., Kushnir, Y., Enzel, Y., Haug, G., and Stein, M.: Dead Sea drawdown and monsoonal impacts in the Levant during the last interglacial, Earth Planet. Sc. Lett., 412, 235–244, https://doi.org/10.1016/j.epsl.2014.12.013, 2015.
Tsvieli, Y. and Zangvil, A.: Synoptic climatological analysis of Red Sea Trough and non-Red Sea Trough rain situations over Israel, Adv. Geosci., 12,
137–143, https://doi.org/10.5194/adgeo-12-137-2007, 2007.
Tyrlis, E. and Lelieveld, J.: Climatology and Dynamics of the Summer Etesian
Winds over the Eastern Mediterranean, J. Atmos. Sci., 70, 3374–3396,
https://doi.org/10.1175/JAS-D-13-035.1, 2013.
Van Hijum, E. and Pilarczyk, K. W.: Gravel beaches: equilibrium profile and
longshore transport of coarse material under regular and irregular wave
attack, Publication no. 274, Delft Hydraulics Laboratory, the Netherlands, 1982.
Vüllers, J., Mayr, G. J., Corsmeier, U., and Kottmeier, C.: Characteristics and evolution of diurnal foehn events in the Dead Sea
valley, Atmos. Chem. Phys., 18, 18169–18186, https://doi.org/10.5194/acp-18-18169-2018, 2018.
Wang, C., Zheng, S., Wang, P., and Hou, J.: Interactions between vegetation,
water flow and sediment transport: A review, J. Hydrodynam., 27, 24–37,
https://doi.org/10.1016/S1001-6058(15)60453-X, 2015.
Weisbrod, N., Yechieli, Y., Shandalov, S., and Lensky, N.: On the viscosity
of natural hyper-saline solutions and its importance: The Dead Sea brines, J. Hydrol., 532, 46–51, https://doi.org/10.1016/j.jhydrol.2015.11.036, 2016.
Wright, L. D.: Sediment transport and deposition at river mouths: A synthesis, Geol. Soc. Am. Bull., 88, 857, https://doi.org/10.1130/0016-7606(1977)88<857:STADAR>2.0.CO;2, 1977.
Zak, I.: The geology of Mt. Sedom, PhD thesis, The Hebrew University, Jerusalem, 208 pp., https://huji.primo.exlibrisgroup.com/permalink/972HUJI_INST/u1osdb/alma990014863530203701
(last acccess: 2 July 2023), 1967.
Zappa, G., Hoskins, B. J., and Shepherd, T. G.: The dependence of wintertime
Mediterranean precipitation on the atmospheric circulation response to climate change, Environ. Res. Lett., 10, 104012, https://doi.org/10.1088/1748-9326/10/10/104012, 2015.
Zittis, G., Almazroui, M., Alpert, P., Ciais, P., Cramer, W., Dahdal, Y.,
Fnais, M., Francis, D., Hadjinicolaou, P., Howari, F., Jrrar, A., Kaskaoutis, D. G., Kulmala, M., Lazoglou, G., Mihalopoulos, N., Lin, X., Rudich, Y., Sciare, J., Stenchikov, G., Xoplaki, E., and Lelieveld, J.: Climate Change and Weather Extremes in the Eastern Mediterranean and Middle East, Rev. Geophys., 60, e2021RG000762, https://doi.org/10.1029/2021RG000762, 2022.
Ziv, B., Saaroni, H., and Alpert, P.: The factors governing the summer regime of the eastern Mediterranean, Int. J. Climatol., 24, 1859–1871, https://doi.org/10.1002/joc.1113, 2004.
Ziv, B., Harpaz, T., Saaroni, H., and Blender, R.: A new methodology for
identifying daughter cyclogenesis: application for the Mediterranean Basin,
Int. J. Climatol., 35, 3847–3861, https://doi.org/10.1002/joc.4250, 2015.
Ziv, B., Saaroni, H., Etkin, A., Harpaz, T., and Shendrik, L.: Formation of
cyclones over the East Mediterranean within Red-Sea Troughs, Int. J. Climatol., 42, 577–596, https://doi.org/10.1002/joc.7261, 2022.
Zoccatelli, D., Marra, F., Armon, M., Rinat, Y., Smith, J. A., and Morin, E.: Contrasting rainfall-runoff characteristics of floods in desert and Mediterranean basins, Hydrol. Earth Syst. Sci., 23, 2665–2678,
https://doi.org/10.5194/hess-23-2665-2019, 2019.
Short summary
Extracting paleoenvironmets from sedimentologic and geomorphic records is a main goal in Earth sciences. We study a chain of processes connecting causative Mediterranean cyclones, coeval floods, storm waves generated by mesoscale funneled wind, and coastal gravel transport. This causes northward dispersion of gravel along the modern Dead Sea coast, which has also persisted since the late Pleistocene, resulting in beach berms and fan deltas always being deposited north of channel mouths.
Extracting paleoenvironmets from sedimentologic and geomorphic records is a main goal in Earth...
