Articles | Volume 17, issue 6
https://doi.org/10.5194/cp-17-2653-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-2653-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
22 Dec 2021
Research article |
| 22 Dec 2021
| 22 Dec 2021
Hydroclimatic variability of opposing Late Pleistocene climates in the Levant revealed by deep Dead Sea sediments
Yoav Ben Dor
CORRESPONDING AUTHOR
The Fredy and Nadine Herrmann Institute of Earth Sciences, The Hebrew
University of Jerusalem, Jerusalem, 9190401, Israel
Geological Survey of Israel, 32 Yesha'ayahu Leibowitz, Jerusalem,
9692100, Israel
Francesco Marra
Institute of Atmospheric Sciences and Climate, National Research
Council of Italy (CNR-ISAC), Bologna, 40129, Italy
Moshe Armon
The Fredy and Nadine Herrmann Institute of Earth Sciences, The Hebrew
University of Jerusalem, Jerusalem, 9190401, Israel
Yehouda Enzel
The Fredy and Nadine Herrmann Institute of Earth Sciences, The Hebrew
University of Jerusalem, Jerusalem, 9190401, Israel
Achim Brauer
Section Climate Dynamics and Landscape Evolution, GFZ German Research
Centre for Geosciences, Potsdam, Germany
Institute of Geosciences, University of Potsdam,
Karl-Liebknecht-Straße 24–25, 14476 Potsdam, Germany
Markus Julius Schwab
Section Climate Dynamics and Landscape Evolution, GFZ German Research
Centre for Geosciences, Potsdam, Germany
Efrat Morin
The Fredy and Nadine Herrmann Institute of Earth Sciences, The Hebrew
University of Jerusalem, Jerusalem, 9190401, Israel
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Kevin Kenfack, Francesco Marra, Zéphirin Yepdo Djomou, Lucie Angennes Djiotang Tchotchou, Alain Tchio Tamoffo, and Derbetini Appolinaire Vondou
Weather Clim. Dynam., 5, 1457–1472, https://doi.org/10.5194/wcd-5-1457-2024, https://doi.org/10.5194/wcd-5-1457-2024, 2024
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The results of this study show that moisture advection induced by horizontal wind anomalies and vertical moisture advection induced by vertical velocity anomalies were crucial mechanisms behind the anomalous October 2019 exceptional rainfall increase over western central Africa. The information we derive can be used to support risk assessment and management in the region and to improve our resilience to ongoing climate change.
Ido Sirota, Rik Tjallingii, Sylvia Pinkerneil, Birgit Schroeder, Marlen Albert, Rebecca Kearney, Oliver Heiri, Simona Breu, and Achim Brauer
Biogeosciences, 21, 4317–4339, https://doi.org/10.5194/bg-21-4317-2024, https://doi.org/10.5194/bg-21-4317-2024, 2024
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Hypoxia has spread in Tiefer See (NE Germany) due to increased human activity. The onset of hypoxia indicated by varve preservation is dated to ~1920 at the lake’s depocenter, which responds faster and more severely to the reduction in oxygen level. The spread of hypoxic conditions is a gradual process that has lasted nearly 100 years, and the chemistry of the sediments shows that the depletion of oxygen in the lake started several decades before the onset of varve preservation.
Talia Rosin, Francesco Marra, and Efrat Morin
Hydrol. Earth Syst. Sci., 28, 3549–3566, https://doi.org/10.5194/hess-28-3549-2024, https://doi.org/10.5194/hess-28-3549-2024, 2024
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Knowledge of extreme precipitation probability at various spatial–temporal scales is crucial. We estimate extreme precipitation return levels at multiple scales (10 min–24 h, 0.25–500 km2) in the eastern Mediterranean using radar data. We show our estimates are comparable to those derived from averaged daily rain gauges. We then explore multi-scale extreme precipitation across coastal, mountainous, and desert regions.
Rajani Kumar Pradhan, Yannis Markonis, Francesco Marra, Efthymios I. Nikolopoulos, Simon Michael Papalexiou, and Vincenzo Levizzani
EGUsphere, https://doi.org/10.5194/egusphere-2024-1626, https://doi.org/10.5194/egusphere-2024-1626, 2024
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This study compared global satellite and one reanalysis precipitation dataset to assess diurnal variability. We found that all datasets capture key diurnal precipitation patterns, with maximum precipitation in the afternoon over land and early morning over the ocean. However, there are differences in the exact timing and amount of precipitation. This suggests that it is better to use a combination of datasets for potential applications rather than relying on a single dataset.
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.
Marcel Ortler, Achim Brauer, Stefano C. Fabbri, Jean Nicolas Haas, Irka Hajdas, Kerstin Kowarik, Jochem Kueck, Hans Reschreiter, and Michael Strasser
Sci. Dril., 33, 1–19, https://doi.org/10.5194/sd-33-1-2024, https://doi.org/10.5194/sd-33-1-2024, 2024
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The lake drilling project at Lake Hallstatt (Austria) successfully cored 51 m of lake sediments. This was achieved through the novel drilling platform Hipercorig. A core-log seismic correlation was created for the first time of an inner Alpine lake of the Eastern Alps. The sediments cover over 12 000 years before present with 10 (up to 5.1 m thick) instantaneous deposits. Lake Hallstatt is located within an UNESCO World Heritage area which has a rich history of human salt mining.
Francesco Marra, Marika Koukoula, Antonio Canale, and Nadav Peleg
Hydrol. Earth Syst. Sci., 28, 375–389, https://doi.org/10.5194/hess-28-375-2024, https://doi.org/10.5194/hess-28-375-2024, 2024
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We present a new physical-based method for estimating extreme sub-hourly precipitation return levels (i.e., intensity–duration–frequency, IDF, curves), which are critical for the estimation of future floods. The proposed model, named TENAX, incorporates temperature as a covariate in a physically consistent manner. It has only a few parameters and can be easily set for any climate station given sub-hourly precipitation and temperature data are available.
Anna Beckett, Cecile Blanchet, Alexander Brauser, Rebecca Kearney, Celia Martin-Puertas, Ian Matthews, Konstantin Mittelbach, Adrian Palmer, Arne Ramisch, and Achim Brauer
Earth Syst. Sci. Data, 16, 595–604, https://doi.org/10.5194/essd-16-595-2024, https://doi.org/10.5194/essd-16-595-2024, 2024
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This paper focuses on volcanic ash (tephra) in European annually laminated (varve) lake records from the period 25 to 8 ka. Tephra enables the synchronisation of these lake records and their proxy reconstructions to absolute timescales. The data incorporate geochemical data from tephra layers across 19 varve lake records. We highlight the potential for synchronising multiple records using tephra layers across continental scales whilst supporting reproducibility through accessible data.
Paula A. Vignoni, Francisco E. Córdoba, Rik Tjallingii, Carla Santamans, Liliana C. Lupo, and Achim Brauer
Geochronology, 5, 333–344, https://doi.org/10.5194/gchron-5-333-2023, https://doi.org/10.5194/gchron-5-333-2023, 2023
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Radiocarbon dating is a widely used tool to establish chronologies for sediment records. We show that modern aquatic plants in the Laguna del Peinado lake system (Altiplano–Puna Plateau) give overestimated ages due to reservoir effects from the input of old groundwater and volcanic CO2. Our results reveal a spatial variability in the modern reservoir effect within the lake basin, which has implications for radiocarbon-based chronologies in paleoclimate studies in this (and similar) regions.
Haggai Eyal, Moshe Armon, Yehouda Enzel, and Nadav G. Lensky
Earth Surf. Dynam., 11, 547–574, https://doi.org/10.5194/esurf-11-547-2023, https://doi.org/10.5194/esurf-11-547-2023, 2023
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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.
Stefan Steger, Mateo Moreno, Alice Crespi, Peter James Zellner, Stefano Luigi Gariano, Maria Teresa Brunetti, Massimo Melillo, Silvia Peruccacci, Francesco Marra, Robin Kohrs, Jason Goetz, Volkmar Mair, and Massimiliano Pittore
Nat. Hazards Earth Syst. Sci., 23, 1483–1506, https://doi.org/10.5194/nhess-23-1483-2023, https://doi.org/10.5194/nhess-23-1483-2023, 2023
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We present a novel data-driven modelling approach to determine season-specific critical precipitation conditions for landslide occurrence. It is shown that the amount of precipitation required to trigger a landslide in South Tyrol varies from season to season. In summer, a higher amount of preparatory precipitation is required to trigger a landslide, probably due to denser vegetation and higher temperatures. We derive dynamic thresholds that directly relate to hit rates and false-alarm rates.
Nadav Peleg, Herminia Torelló-Sentelles, Grégoire Mariéthoz, Lionel Benoit, João P. Leitão, and Francesco Marra
Nat. Hazards Earth Syst. Sci., 23, 1233–1240, https://doi.org/10.5194/nhess-23-1233-2023, https://doi.org/10.5194/nhess-23-1233-2023, 2023
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Floods in urban areas are one of the most common natural hazards. Due to climate change enhancing extreme rainfall and cities becoming larger and denser, the impacts of these events are expected to increase. A fast and reliable flood warning system should thus be implemented in flood-prone cities to warn the public of upcoming floods. The purpose of this brief communication is to discuss the potential implementation of low-cost acoustic rainfall sensors in short-term flood warning systems.
Eleonora Dallan, Francesco Marra, Giorgia Fosser, Marco Marani, Giuseppe Formetta, Christoph Schär, and Marco Borga
Hydrol. Earth Syst. Sci., 27, 1133–1149, https://doi.org/10.5194/hess-27-1133-2023, https://doi.org/10.5194/hess-27-1133-2023, 2023
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Convection-permitting climate models could represent future changes in extreme short-duration precipitation, which is critical for risk management. We use a non-asymptotic statistical method to estimate extremes from 10 years of simulations in an orographically complex area. Despite overall good agreement with rain gauges, the observed decrease of hourly extremes with elevation is not fully represented by the model. Climate model adjustment methods should consider the role of orography.
Shalev Siman-Tov and Francesco Marra
Nat. Hazards Earth Syst. Sci., 23, 1079–1093, https://doi.org/10.5194/nhess-23-1079-2023, https://doi.org/10.5194/nhess-23-1079-2023, 2023
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Debris flows represent a threat to infrastructure and the population. In arid areas, they are observed when heavy rainfall hits steep slopes with sediments. Here, we use digital surface models and radar rainfall data to detect and characterize the triggering and non-triggering rainfall conditions. We find that rainfall intensity alone is insufficient to explain the triggering. We suggest that antecedent rainfall could represent a critical factor for debris flow triggering in arid regions.
Markus Czymzik, Rik Tjallingii, Birgit Plessen, Peter Feldens, Martin Theuerkauf, Matthias Moros, Markus J. Schwab, Carla K. M. Nantke, Silvia Pinkerneil, Achim Brauer, and Helge W. Arz
Clim. Past, 19, 233–248, https://doi.org/10.5194/cp-19-233-2023, https://doi.org/10.5194/cp-19-233-2023, 2023
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Productivity increases in Lake Kälksjön sediments during the last 9600 years are likely driven by the progressive millennial-scale winter warming in northwestern Europe, following the increasing Northern Hemisphere winter insolation and decadal to centennial periods of a more positive NAO polarity. Strengthened productivity variability since ∼5450 cal yr BP is hypothesized to reflect a reinforcement of NAO-like atmospheric circulation.
Bernhard Diekmann, Werner Stackebrandt, Roland Weiße, Margot Böse, Udo Rothe, Boris Biskaborn, and Achim Brauer
DEUQUA Spec. Pub., 4, 5–17, https://doi.org/10.5194/deuquasp-4-5-2022, https://doi.org/10.5194/deuquasp-4-5-2022, 2022
Achim Brauer, Ingo Heinrich, Markus J. Schwab, Birgit Plessen, Brian Brademann, Matthias Köppl, Sylvia Pinkerneil, Daniel Balanzategui, Gerhard Helle, and Theresa Blume
DEUQUA Spec. Pub., 4, 41–58, https://doi.org/10.5194/deuquasp-4-41-2022, https://doi.org/10.5194/deuquasp-4-41-2022, 2022
Achim Brauer and Markus J. Schwab
DEUQUA Spec. Pub., 4, 1–3, https://doi.org/10.5194/deuquasp-4-1-2022, https://doi.org/10.5194/deuquasp-4-1-2022, 2022
Sella Nevo, Efrat Morin, Adi Gerzi Rosenthal, Asher Metzger, Chen Barshai, Dana Weitzner, Dafi Voloshin, Frederik Kratzert, Gal Elidan, Gideon Dror, Gregory Begelman, Grey Nearing, Guy Shalev, Hila Noga, Ira Shavitt, Liora Yuklea, Moriah Royz, Niv Giladi, Nofar Peled Levi, Ofir Reich, Oren Gilon, Ronnie Maor, Shahar Timnat, Tal Shechter, Vladimir Anisimov, Yotam Gigi, Yuval Levin, Zach Moshe, Zvika Ben-Haim, Avinatan Hassidim, and Yossi Matias
Hydrol. Earth Syst. Sci., 26, 4013–4032, https://doi.org/10.5194/hess-26-4013-2022, https://doi.org/10.5194/hess-26-4013-2022, 2022
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Early flood warnings are one of the most effective tools to save lives and goods. Machine learning (ML) models can improve flood prediction accuracy but their use in operational frameworks is limited. The paper presents a flood warning system, operational in India and Bangladesh, that uses ML models for forecasting river stage and flood inundation maps and discusses the models' performances. In 2021, more than 100 million flood alerts were sent to people near rivers over an area of 470 000 km2.
Assaf Hochman, Francesco Marra, Gabriele Messori, Joaquim G. Pinto, Shira Raveh-Rubin, Yizhak Yosef, and Georgios Zittis
Earth Syst. Dynam., 13, 749–777, https://doi.org/10.5194/esd-13-749-2022, https://doi.org/10.5194/esd-13-749-2022, 2022
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Gaining a complete understanding of extreme weather, from its physical drivers to its impacts on society, is important in supporting future risk reduction and adaptation measures. Here, we provide a review of the available scientific literature, knowledge gaps and key open questions in the study of extreme weather events over the vulnerable eastern Mediterranean region.
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.
Cécile L. Blanchet, Rik Tjallingii, Anja M. Schleicher, Stefan Schouten, Martin Frank, and Achim Brauer
Clim. Past, 17, 1025–1050, https://doi.org/10.5194/cp-17-1025-2021, https://doi.org/10.5194/cp-17-1025-2021, 2021
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The Mediterranean Sea turned repeatedly into an oxygen-deprived basin during the geological past, as evidenced by distinct sediment layers called sapropels. We use here records of the last sapropel S1 retrieved in front of the Nile River to explore the relationships between riverine input and seawater oxygenation. We decipher the seasonal cycle of fluvial input and seawater chemistry as well as the decisive influence of primary productivity on deoxygenation at millennial timescales.
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.
Arne Ramisch, Alexander Brauser, Mario Dorn, Cecile Blanchet, Brian Brademann, Matthias Köppl, Jens Mingram, Ina Neugebauer, Norbert Nowaczyk, Florian Ott, Sylvia Pinkerneil, Birgit Plessen, Markus J. Schwab, Rik Tjallingii, and Achim Brauer
Earth Syst. Sci. Data, 12, 2311–2332, https://doi.org/10.5194/essd-12-2311-2020, https://doi.org/10.5194/essd-12-2311-2020, 2020
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Annually laminated lake sediments (varves) record past climate change at seasonal resolution. The VARved sediments DAtabase (VARDA) is created to utilize the full potential of varves for climate reconstructions. VARDA offers free access to a compilation and synchronization of standardized climate-proxy data, with applications ranging from reconstructing regional patterns of past climate change to validating simulations of climate models. VARDA is freely accessible at https://varve.gfz-potsdam.de
Florian Mekhaldi, Markus Czymzik, Florian Adolphi, Jesper Sjolte, Svante Björck, Ala Aldahan, Achim Brauer, Celia Martin-Puertas, Göran Possnert, and Raimund Muscheler
Clim. Past, 16, 1145–1157, https://doi.org/10.5194/cp-16-1145-2020, https://doi.org/10.5194/cp-16-1145-2020, 2020
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Due to chronology uncertainties within paleoclimate archives, it is unclear how climate oscillations from different records relate to one another. By using radionuclides to synchronize Greenland ice cores and a German lake record over 11 000 years, we show that two oscillations observed in these records were not synchronous but terminated and began with the onset of a grand solar minimum. Both this and changes in ocean circulation could have played a role in the two climate oscillations.
Julia Kalanke, Jens Mingram, Stefan Lauterbach, Ryskul Usubaliev, Rik Tjallingii, and Achim Brauer
Geochronology, 2, 133–154, https://doi.org/10.5194/gchron-2-133-2020, https://doi.org/10.5194/gchron-2-133-2020, 2020
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Our study presents the first seasonally laminated (varved) sediment record covering almost the entire Holocene in high mountainous arid Central Asia. The established floating varve chronology is confirmed by two terrestrial radiocarbon dates, whereby aquatic radiocarbon dates reveal decreasing reservoir ages up core. Changes in seasonal deposition characteristics are attributed to changes in runoff and precipitation and/or to evaporative summer conditions.
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.
Achim Brauer, Markus J. Schwab, Brian Brademann, Sylvia Pinkerneil, and Martin Theuerkauf
DEUQUA Spec. Pub., 2, 89–93, https://doi.org/10.5194/deuquasp-2-89-2019, https://doi.org/10.5194/deuquasp-2-89-2019, 2019
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.
Bernhard Aichner, Florian Ott, Michał Słowiński, Agnieszka M. Noryśkiewicz, Achim Brauer, and Dirk Sachse
Clim. Past, 14, 1607–1624, https://doi.org/10.5194/cp-14-1607-2018, https://doi.org/10.5194/cp-14-1607-2018, 2018
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Abundances of plant biomarkers are compared with pollen data in a 3000-year climate archive covering the Late Glacial to Holocene transition in northern Poland. Both parameters synchronously show the rapid onset (12680–12600 yr BP) and termination
(11580–11490 yr BP) of the Younger Dryas cold interval in the study area. This demonstrates the suitability of such proxies to record pronounced changes in vegetation cover without significant delay.
William Amponsah, Pierre-Alain Ayral, Brice Boudevillain, Christophe Bouvier, Isabelle Braud, Pascal Brunet, Guy Delrieu, Jean-François Didon-Lescot, Eric Gaume, Laurent Lebouc, Lorenzo Marchi, Francesco Marra, Efrat Morin, Guillaume Nord, Olivier Payrastre, Davide Zoccatelli, and Marco Borga
Earth Syst. Sci. Data, 10, 1783–1794, https://doi.org/10.5194/essd-10-1783-2018, https://doi.org/10.5194/essd-10-1783-2018, 2018
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The EuroMedeFF database comprises 49 events that occurred in France, Israel, Germany, Slovenia, Romania, and Italy. The dataset may be of help to hydrologists as well as other scientific communities because it offers benchmark data for the verification of flash flood hydrological models and for hydro-meteorological forecast systems. It provides, moreover, a sample of rainfall and flood discharge extremes in different climates.
Markus Czymzik, Raimund Muscheler, Florian Adolphi, Florian Mekhaldi, Nadine Dräger, Florian Ott, Michał Słowinski, Mirosław Błaszkiewicz, Ala Aldahan, Göran Possnert, and Achim Brauer
Clim. Past, 14, 687–696, https://doi.org/10.5194/cp-14-687-2018, https://doi.org/10.5194/cp-14-687-2018, 2018
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Our results provide a proof of concept for facilitating 10Be in varved lake sediments as a novel synchronization tool required for investigating leads and lags of proxy responses to climate variability. They also point to some limitations of 10Be in these archives mainly connected to in-lake sediment resuspension processes.
Norel Rimbu, Monica Ionita, Markus Czymzik, Achim Brauer, and Gerrit Lohmann
Clim. Past Discuss., https://doi.org/10.5194/cp-2017-137, https://doi.org/10.5194/cp-2017-137, 2017
Manuscript not accepted for further review
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Multi-decadal to millennial flood frequency variations in the Mid- to Late Holocene in a flood layer record from Lake Ammersee is strongly related to the occurrence of extreme precipitation and temperatures in the northeastern Europe.
Annette Witt, Bruce D. Malamud, Clara Mangili, and Achim Brauer
Hydrol. Earth Syst. Sci., 21, 5547–5581, https://doi.org/10.5194/hess-21-5547-2017, https://doi.org/10.5194/hess-21-5547-2017, 2017
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Here we present a unique 9.5 m palaeo-lacustrine record of 771 palaeofloods which occurred over a period of 10 000 years in the Piànico–Sèllere basin (southern Alps) during an interglacial period in the Pleistocene (sometime between 400 000 and 800 000 years ago). We analyse the palaeoflood series correlation, clustering, and cyclicity properties, finding a long-range cyclicity with a period of about 2030 years superimposed onto a fractional noise.
Idit Belachsen, Francesco Marra, Nadav Peleg, and Efrat Morin
Hydrol. Earth Syst. Sci., 21, 5165–5180, https://doi.org/10.5194/hess-21-5165-2017, https://doi.org/10.5194/hess-21-5165-2017, 2017
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Spatiotemporal rainfall patterns in arid environments are not well-known. We derived properties of convective rain cells over the arid Dead Sea region from a long-term radar archive. We found differences in cell properties between synoptic systems and between flash-flood and non-flash-flood events. Large flash floods are associated with slow rain cells, directed downstream with the main catchment axis. Results from this work can be used for hydrological models and stochastic storm simulations.
Francesco Marra, Elisa Destro, Efthymios I. Nikolopoulos, Davide Zoccatelli, Jean Dominique Creutin, Fausto Guzzetti, and Marco Borga
Hydrol. Earth Syst. Sci., 21, 4525–4532, https://doi.org/10.5194/hess-21-4525-2017, https://doi.org/10.5194/hess-21-4525-2017, 2017
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Previous studies have reported a systematic underestimation of debris flow occurrence thresholds, due to the use of sparse networks in non-stationary rain fields. We analysed high-resolution radar data to show that spatially aggregated estimates (e.g. satellite data) largely reduce this issue, in light of a reduced estimation variance. Our findings are transferable to other situations in which lower envelope curves are used to predict point-like events in the presence of non-stationary fields.
Oliver Rach, Ansgar Kahmen, Achim Brauer, and Dirk Sachse
Clim. Past, 13, 741–757, https://doi.org/10.5194/cp-13-741-2017, https://doi.org/10.5194/cp-13-741-2017, 2017
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Currently, reconstructions of past changes in the hydrological cycle are usually qualitative, which is a major drawback for testing the accuracy of models in predicting future responses. Here we present a proof of concept of a novel approach to deriving quantitative paleohydrological data, i.e. changes in relative humidity, from lacustrine sediment archives, employing a combination of organic geochemical methods and plant physiological modeling.
Francesco Marra, Efrat Morin, Nadav Peleg, Yiwen Mei, and Emmanouil N. Anagnostou
Hydrol. Earth Syst. Sci., 21, 2389–2404, https://doi.org/10.5194/hess-21-2389-2017, https://doi.org/10.5194/hess-21-2389-2017, 2017
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Rainfall frequency analyses from radar and satellite estimates over the eastern Mediterranean are compared examining different climatic conditions. Correlation between radar and satellite results is high for frequent events and decreases with return period. The uncertainty related to record length is larger for drier climates. The agreement between different sensors instills confidence on their use for rainfall frequency analysis in ungauged areas of the Earth.
Markus Czymzik, Raimund Muscheler, and Achim Brauer
Clim. Past, 12, 799–805, https://doi.org/10.5194/cp-12-799-2016, https://doi.org/10.5194/cp-12-799-2016, 2016
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Integrating discharge data of the River Ammer back to 1926 and a 5500-year flood layer record from an annually laminated sediment core of the downstream Ammersee allowed investigating changes in the frequency of major floods in Central Europe on interannual to multi-centennial timescales. Significant correlations between flood frequency variations in both archives and changes in the activity of the Sun suggest a solar influence on the frequency of these hydrometeorological extremes.
Norel Rimbu, Markus Czymzik, Monica Ionita, Gerrit Lohmann, and Achim Brauer
Clim. Past, 12, 377–385, https://doi.org/10.5194/cp-12-377-2016, https://doi.org/10.5194/cp-12-377-2016, 2016
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
Short summary
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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.
N. Peleg, E. Shamir, K. P. Georgakakos, and E. Morin
Hydrol. Earth Syst. Sci., 19, 567–581, https://doi.org/10.5194/hess-19-567-2015, https://doi.org/10.5194/hess-19-567-2015, 2015
C. Martin-Puertas, A. Brauer, S. Wulf, F. Ott, S. Lauterbach, and P. Dulski
Clim. Past, 10, 2099–2114, https://doi.org/10.5194/cp-10-2099-2014, https://doi.org/10.5194/cp-10-2099-2014, 2014
B. Merz, J. Aerts, K. Arnbjerg-Nielsen, M. Baldi, A. Becker, A. Bichet, G. Blöschl, L. M. Bouwer, A. Brauer, F. Cioffi, J. M. Delgado, M. Gocht, F. Guzzetti, S. Harrigan, K. Hirschboeck, C. Kilsby, W. Kron, H.-H. Kwon, U. Lall, R. Merz, K. Nissen, P. Salvatti, T. Swierczynski, U. Ulbrich, A. Viglione, P. J. Ward, M. Weiler, B. Wilhelm, and M. Nied
Nat. Hazards Earth Syst. Sci., 14, 1921–1942, https://doi.org/10.5194/nhess-14-1921-2014, https://doi.org/10.5194/nhess-14-1921-2014, 2014
T. Swierczynski, S. Lauterbach, P. Dulski, and A. Brauer
Clim. Past, 9, 1601–1612, https://doi.org/10.5194/cp-9-1601-2013, https://doi.org/10.5194/cp-9-1601-2013, 2013
N. Peleg, M. Ben-Asher, and E. Morin
Hydrol. Earth Syst. Sci., 17, 2195–2208, https://doi.org/10.5194/hess-17-2195-2013, https://doi.org/10.5194/hess-17-2195-2013, 2013
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
Related subject area
Subject: Proxy Use-Development-Validation | Archive: Terrestrial Archives | Timescale: Pleistocene
The Indo–Pacific Pollen Database – a Neotoma constituent database
Can machine-learning algorithms improve upon classical palaeoenvironmental reconstruction models?
Distinguishing the combined vegetation and soil component of δ13C variation in speleothem records from subsequent degassing and prior calcite precipitation effects
Multi-proxy speleothem-based reconstruction of mid-MIS 3 climate in South Africa
Biomarker proxy records of Arctic climate change during the Mid-Pleistocene transition from Lake El'gygytgyn (Far East Russia)
Different facets of dry–wet patterns in south-western China over the past 27 000 years
The triple oxygen isotope composition of phytoliths, a new proxy of atmospheric relative humidity: controls of soil water isotope composition, temperature, CO2 concentration and relative humidity
The speleothem oxygen record as a proxy for thermal or moisture changes: a case study of multiproxy records from MIS 5–MIS 6 speleothems from the Demänová Cave system
A new multivariable benchmark for Last Glacial Maximum climate simulations
The Last Glacial Maximum in the central North Island, New Zealand: palaeoclimate inferences from glacier modelling
Late-glacial to late-Holocene shifts in global precipitation δ18O
Climate history of the Southern Hemisphere Westerlies belt during the last glacial–interglacial transition revealed from lake water oxygen isotope reconstruction of Laguna Potrok Aike (52° S, Argentina)
New online method for water isotope analysis of speleothem fluid inclusions using laser absorption spectroscopy (WS-CRDS)
Inorganic geochemistry data from Lake El'gygytgyn sediments: marine isotope stages 6–11
A 350 ka record of climate change from Lake El'gygytgyn, Far East Russian Arctic: refining the pattern of climate modes by means of cluster analysis
Dynamic diatom response to changing climate 0–1.2 Ma at Lake El'gygytgyn, Far East Russian Arctic
Amplified bioproductivity during Transition IV (332 000–342 000 yr ago): evidence from the geochemical record of Lake El'gygytgyn
Potential and limits of OSL, TT-OSL, IRSL and pIRIR290 dating methods applied on a Middle Pleistocene sediment record of Lake El'gygytgyn, Russia
Rock magnetic properties, magnetic susceptibility, and organic geochemistry comparison in core LZ1029-7 Lake El'gygytgyn, Russia Far East
High-temperature thermomagnetic properties of vivianite nodules, Lake El'gygytgyn, Northeast Russia
Reconstruction of drip-water δ18O based on calcite oxygen and clumped isotopes of speleothems from Bunker Cave (Germany)
A biomarker record of Lake El'gygytgyn, Far East Russian Arctic: investigating sources of organic matter and carbon cycling during marine isotope stages 1–3
Climate warming and vegetation response after Heinrich event 1 (16 700–16 000 cal yr BP) in Europe south of the Alps
A 250 ka oxygen isotope record from diatoms at Lake El'gygytgyn, far east Russian Arctic
The oxygen isotopic composition of phytolith assemblages from tropical rainforest soil tops (Queensland, Australia): validation of a new paleoenvironmental tool
Terrestrial mollusc records from Xifeng and Luochuan L9 loess strata and their implications for paleoclimatic evolution in the Chinese Loess Plateau during marine Oxygen Isotope Stages 24-22
Annika V. Herbert, Simon G. Haberle, Suzette G. A. Flantua, Ondrej Mottl, Jessica L. Blois, John W. Williams, Adrian George, and Geoff S. Hope
Clim. Past, 20, 2473–2485, https://doi.org/10.5194/cp-20-2473-2024, https://doi.org/10.5194/cp-20-2473-2024, 2024
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The Indo-Pacific Pollen Database is a large collection of pollen samples from across the Indo-Pacific region, with most samples coming from Australia. This is a valuable collection that can be used to analyse vegetation dynamics going back thousands of years. It is now being fully shared via Neotoma for the first time, opening up many exciting new avenues of research. This paper presents key aspects of this database, including geographical distribution, age control and deposition times.
Peng Sun, Philip B. Holden, and H. John B. Birks
Clim. Past, 20, 2373–2398, https://doi.org/10.5194/cp-20-2373-2024, https://doi.org/10.5194/cp-20-2373-2024, 2024
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We develop the Multi Ensemble Machine Learning Model (MEMLM) for reconstructing palaeoenvironments from microfossil assemblages. The machine-learning approaches, which include random tree and natural language processing techniques, substantially outperform classical approaches under cross-validation, but they can fail when applied to reconstruct past environments. Statistical significance testing is found sufficient to identify these unreliable reconstructions.
Heather M. Stoll, Chris Day, Franziska Lechleitner, Oliver Kost, Laura Endres, Jakub Sliwinski, Carlos Pérez-Mejías, Hai Cheng, and Denis Scholz
Clim. Past, 19, 2423–2444, https://doi.org/10.5194/cp-19-2423-2023, https://doi.org/10.5194/cp-19-2423-2023, 2023
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Stalagmites formed in caves provide valuable information about past changes in climate and vegetation conditions. In this contribution, we present a new method to better estimate past changes in soil and vegetation productivity using carbon isotopes and trace elements measured in stalagmites. Applying this method to other stalagmites should provide a better indication of past vegetation feedbacks to climate change.
Jenny Maccali, Anna Nele Meckler, Stein-Erik Lauritzen, Torill Brekken, Helen Aase Rokkan, Alvaro Fernandez, Yves Krüger, Jane Adigun, Stéphane Affolter, and Markus Leuenberger
Clim. Past, 19, 1847–1862, https://doi.org/10.5194/cp-19-1847-2023, https://doi.org/10.5194/cp-19-1847-2023, 2023
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The southern coast of South Africa hosts some key archeological sites for the study of early human evolution. Here we present a short but high-resolution record of past changes in the hydroclimate and temperature on the southern coast of South Africa based on the study of a speleothem collected from Bloukrantz Cave. Overall, the paleoclimate indicators suggest stable temperature from 48.3 to 45.2 ka, whereas precipitation was variable, with marked short drier episodes.
Kurt R. Lindberg, William C. Daniels, Isla S. Castañeda, and Julie Brigham-Grette
Clim. Past, 18, 559–577, https://doi.org/10.5194/cp-18-559-2022, https://doi.org/10.5194/cp-18-559-2022, 2022
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Earth experiences regular ice ages resulting in shifts between cooler and warmer climates. Around 1 million years ago, the ice age cycles grew longer and stronger. We used bacterial and plant lipids preserved in an Arctic lake to reconstruct temperature and vegetation during this climate transition. We find that Arctic land temperatures did not cool much compared to ocean records from this period, and that vegetation shifts correspond with a long-term drying previously reported in the region.
Mengna Liao, Kai Li, Weiwei Sun, and Jian Ni
Clim. Past, 17, 2291–2303, https://doi.org/10.5194/cp-17-2291-2021, https://doi.org/10.5194/cp-17-2291-2021, 2021
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The long-term trajectories of precipitation, hydrological balance and soil moisture are not completely consistent in southwest China. Hydrological balance was more sensitive to temperature change on a millennial scale. For soil moisture, plant processes also played a big role in addition to precipitation and temperature. Under future climate warming, surface water shortage in southwest China can be even more serious and efforts at reforestation may bring some relief to the soil moisture deficit.
Clément Outrequin, Anne Alexandre, Christine Vallet-Coulomb, Clément Piel, Sébastien Devidal, Amaelle Landais, Martine Couapel, Jean-Charles Mazur, Christophe Peugeot, Monique Pierre, Frédéric Prié, Jacques Roy, Corinne Sonzogni, and Claudia Voigt
Clim. Past, 17, 1881–1902, https://doi.org/10.5194/cp-17-1881-2021, https://doi.org/10.5194/cp-17-1881-2021, 2021
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Continental atmospheric humidity is a key climate parameter poorly captured by global climate models. Model–data comparison approaches that are applicable beyond the instrumental period are essential to progress on this issue but face a lack of quantitative relative humidity proxies. Here, we calibrate the triple oxygen isotope composition of phytoliths as a new quantitative proxy of continental relative humidity suitable for past climate reconstructions.
Jacek Pawlak
Clim. Past, 17, 1051–1064, https://doi.org/10.5194/cp-17-1051-2021, https://doi.org/10.5194/cp-17-1051-2021, 2021
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Presently, central Europe is under the influence of two types of climate, transitional and continental. The 60 ka long multiproxy speleothem dataset from Slovakia records the climate of the Last Interglacial cycle and its transition to the Last Glacial. The interpretation of stable isotopic composition and trace element content proxies helps to distinguish which factor had the strongest influence on the δ18O record shape: the local temperature, the humidity or the source effect.
Sean F. Cleator, Sandy P. Harrison, Nancy K. Nichols, I. Colin Prentice, and Ian Roulstone
Clim. Past, 16, 699–712, https://doi.org/10.5194/cp-16-699-2020, https://doi.org/10.5194/cp-16-699-2020, 2020
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We present geographically explicit reconstructions of seasonal temperature and annual moisture variables at the Last Glacial Maximum (LGM), 21 000 years ago. The reconstructions use existing site-based estimates of climate, interpolated in space and time in a physically consistent way using climate model simulations. The reconstructions give a much better picture of the LGM climate and will provide a robust evaluation of how well state-of-the-art climate models simulate large climate changes.
Shaun R. Eaves, Andrew N. Mackintosh, Brian M. Anderson, Alice M. Doughty, Dougal B. Townsend, Chris E. Conway, Gisela Winckler, Joerg M. Schaefer, Graham S. Leonard, and Andrew T. Calvert
Clim. Past, 12, 943–960, https://doi.org/10.5194/cp-12-943-2016, https://doi.org/10.5194/cp-12-943-2016, 2016
Short summary
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Geological evidence for past changes in glacier length provides a useful source of information about pre-historic climate change. We have used glacier modelling to show that air temperature reductions of −5 to −7 °C, relative to present, are required to simulate the glacial extent in the North Island, New Zealand, during the last ice age (approx. 20000 years ago). Our results provide data to assess climate model simulations, with the aim of determining the drivers of past natural climate change.
S. Jasechko, A. Lechler, F. S. R. Pausata, P. J. Fawcett, T. Gleeson, D. I. Cendón, J. Galewsky, A. N. LeGrande, C. Risi, Z. D. Sharp, J. M. Welker, M. Werner, and K. Yoshimura
Clim. Past, 11, 1375–1393, https://doi.org/10.5194/cp-11-1375-2015, https://doi.org/10.5194/cp-11-1375-2015, 2015
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In this study we compile global isotope proxy records of climate changes from the last ice age to the late-Holocene preserved in cave calcite, glacial ice and groundwater aquifers. We show that global patterns of late-Pleistocene to late-Holocene precipitation isotope shifts are consistent with stronger-than-modern isotopic distillation of air masses during the last ice age, likely impacted by larger global temperature differences between the tropics and the poles.
J. Zhu, A. Lücke, H. Wissel, C. Mayr, D. Enters, K. Ja Kim, C. Ohlendorf, F. Schäbitz, and B. Zolitschka
Clim. Past, 10, 2153–2169, https://doi.org/10.5194/cp-10-2153-2014, https://doi.org/10.5194/cp-10-2153-2014, 2014
S. Affolter, D. Fleitmann, and M. Leuenberger
Clim. Past, 10, 1291–1304, https://doi.org/10.5194/cp-10-1291-2014, https://doi.org/10.5194/cp-10-1291-2014, 2014
P. S. Minyuk, V. Y. Borkhodoev, and V. Wennrich
Clim. Past, 10, 467–485, https://doi.org/10.5194/cp-10-467-2014, https://doi.org/10.5194/cp-10-467-2014, 2014
U. Frank, N. R. Nowaczyk, P. Minyuk, H. Vogel, P. Rosén, and M. Melles
Clim. Past, 9, 1559–1569, https://doi.org/10.5194/cp-9-1559-2013, https://doi.org/10.5194/cp-9-1559-2013, 2013
J. A. Snyder, M. V. Cherepanova, and A. Bryan
Clim. Past, 9, 1309–1319, https://doi.org/10.5194/cp-9-1309-2013, https://doi.org/10.5194/cp-9-1309-2013, 2013
L. Cunningham, H. Vogel, V. Wennrich, O. Juschus, N. Nowaczyk, and P. Rosén
Clim. Past, 9, 679–686, https://doi.org/10.5194/cp-9-679-2013, https://doi.org/10.5194/cp-9-679-2013, 2013
A. Zander and A. Hilgers
Clim. Past, 9, 719–733, https://doi.org/10.5194/cp-9-719-2013, https://doi.org/10.5194/cp-9-719-2013, 2013
K. J. Murdock, K. Wilkie, and L. L. Brown
Clim. Past, 9, 467–479, https://doi.org/10.5194/cp-9-467-2013, https://doi.org/10.5194/cp-9-467-2013, 2013
P. S. Minyuk, T. V. Subbotnikova, L. L. Brown, and K. J. Murdock
Clim. Past, 9, 433–446, https://doi.org/10.5194/cp-9-433-2013, https://doi.org/10.5194/cp-9-433-2013, 2013
T. Kluge, H. P. Affek, T. Marx, W. Aeschbach-Hertig, D. F. C. Riechelmann, D. Scholz, S. Riechelmann, A. Immenhauser, D. K. Richter, J. Fohlmeister, A. Wackerbarth, A. Mangini, and C. Spötl
Clim. Past, 9, 377–391, https://doi.org/10.5194/cp-9-377-2013, https://doi.org/10.5194/cp-9-377-2013, 2013
A. R. Holland, S. T. Petsch, I. S. Castañeda, K. M. Wilkie, S. J. Burns, and J. Brigham-Grette
Clim. Past, 9, 243–260, https://doi.org/10.5194/cp-9-243-2013, https://doi.org/10.5194/cp-9-243-2013, 2013
S. Samartin, O. Heiri, A. F. Lotter, and W. Tinner
Clim. Past, 8, 1913–1927, https://doi.org/10.5194/cp-8-1913-2012, https://doi.org/10.5194/cp-8-1913-2012, 2012
B. Chapligin, H. Meyer, G. E. A. Swann, C. Meyer-Jacob, and H.-W. Hubberten
Clim. Past, 8, 1621–1636, https://doi.org/10.5194/cp-8-1621-2012, https://doi.org/10.5194/cp-8-1621-2012, 2012
A. Alexandre, J. Crespin, F. Sylvestre, C. Sonzogni, and D. W. Hilbert
Clim. Past, 8, 307–324, https://doi.org/10.5194/cp-8-307-2012, https://doi.org/10.5194/cp-8-307-2012, 2012
B. Wu and N. Q. Wu
Clim. Past, 7, 349–359, https://doi.org/10.5194/cp-7-349-2011, https://doi.org/10.5194/cp-7-349-2011, 2011
Cited articles
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, Quaternary Res., 89, 425–431, https://doi.org/10.1017/qua.2018.9, 2018.
Allen, K., Hope, P., Lam, D., Brown, J., and Wasson, R.: Improving
Australia's flood record for planning purposes – can we do better?,
Australasian Journal of Water Resources, 24, 36–45, 2020.
Alpert, P., Ben-Gai, T., Baharad, A., Benjamini, Y., Yekutieli, D.,
Colacino, M., Diodato, L., Ramis, C., Homar, V., Romero, R., Michaelides,
S., and Manes, A.: The paradoxical increase of Mediterranean extreme daily
rainfall in spite of decrease in total values, Geophys. Res. Lett.,
29, 31-31–31-34, https://doi.org/10.1029/2001GL013554, 2002.
Amit, R., Simhai, O., Ayalon, A., Enzel, Y., Matmon, A., Crouvi, O., Porat,
N., and McDonald, E.: Transition from arid to hyper-arid environment in the
southern Levant deserts as recorded by early Pleistocene cummulic Aridisols,
Quaternary Sci. Rev., 30, 312–323, 2011.
Ansari, A. R. and Bradley, R. A.: Rank-sum tests for dispersions, Ann.
Math. Stat., 31, 1174–1189, 1960.
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, 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.
Avni, S., Joseph-Hai, N., Haviv, I., Matmon, A., Benedetti, L., and Team,
A.: Patterns and rates of 103–105 yr denudation in carbonate terrains under
subhumid to subalpine climatic gradient, Mount Hermon, Israel, GSA Bull.,
131, 899–912, 2018.
Baker, V. R.: Paleoflood hydrology: Origin, progress, prospects,
Geomorphology, 101, 1–13, 2008.
Bar-Matthews, M., Ayalon, A., Kaufman, A., and Wasserburg, G. J.: The
Eastern Mediterranean paleoclimate as a reflection of regional events: Soreq
cave, Israel, Earth Planet. Sc. Lett., 166, 85–95, 1999.
Bar-Matthews, M., Ayalon, A., Gilmour, M., Matthews, A., and Hawkesworth, C.
J.: Sea–land oxygen isotopic relationships from planktonic foraminifera and
speleothems in the Eastern Mediterranean region and their implication for
paleorainfall during interglacial intervals, Geochim. Cosmochim. Ac., 67,
3181–3199, 2003.
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, Quaternary Res., 57, 9–21, 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, 439–442, 2003.
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,
2007.
Begin, Z., Ehrlich, A., and Nathan, Y.: Lake Lisan, the Pleistocene precursor of the Dead Sea. Israel Geological Survey, Bulletin 63, 30 pp., 1974.
Begin, Z. B., Nathan, Y., and Ehrlich, A.: Stratigraphy and facies
distribution in the Lisan Formation – new evidence from the area south of
the Dead Sea, Israel, Israel J. Earth Sci., 29, 182–189, 1980.
Begin, Z. B., Stein, M., Katz, A., Machlus, M., Rosenfeld, A., Buchbinder,
B., and Bartov, Y.: Southward migration of rain tracks during the last
glacial, revealed by salinity gradient in Lake Lisan (Dead Sea rift),
Quaternary Sci. Rev., 23, 1627–1636, https://doi.org/10.1016/j.quascirev.2004.01.002,
2004.
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.
Belmaker, R., Lazar, B., Stein, M., Taha, N., and Bookman, R.: Constraints
on aragonite precipitation in the Dead Sea from geochemical measurements of
flood plumes, Quaternary Sci. Rev., 221, 105876, https://doi.org/10.1016/j.quascirev.2019.105876, 2019.
Ben David-Novak, H., 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, 2004.
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.
Ben Dor, Y., Neugebauer, I., Enzel, Y., Schwab, M. J., Tjallingii, R., Erel,
Y., and Brauer, A.: Varves of the Dead Sea sedimentary record, Quaternary
Sci. Rev., 215, 173–184, 2019.
Ben Dor, Y., Neugebauer, I., Enzel, Y., Schwab, M. J., Tjallingii, R., Erel,
Y., and Brauer, A.: Reply to comment on Ben Dor Y. et al. “Varves of the
Dead Sea sedimentary record”, Quaternary Sci. Rev., 215, 2019
173–184, Quaternary Sci. Rev., 231, 106063, https://doi.org/10.1016/j.quascirev.2019.106063,
2020.
Ben Dor, Y., Flax, T., Levitan, I., Enzel, Y., Brauer, A., and Erel, Y.: The
paleohydrological implications of aragonite precipitation under contrasting
climates in the endorheic Dead Sea and its precursors revealed by
experimental investigations, Chem. Geol., 576, 120261, https://doi.org/10.1016/j.chemgeo.2021.120261, 2021.
Black, E.: The influence of the North Atlantic Oscillation and European
circulation regimes on the daily to interannual variability of winter
precipitation in Israel, Int. J. Climatol., 32,
1654–1664, 2012.
Blackman, R. B. and Tukey, J. W.: The measurement of power spectra from the point of view of communications engineering – Part I, Bell System Technical Journal, 37, 185–282,
https://doi.org/10.1002/j.1538-7305.1958.tb03874.x, 1958.
Bookman, R., Bartov, Y., Enzel, Y., and Stein, M.: Quaternary lake levels in
the Dead Sea basin: two centuries of research, Geol. Soc. Am.
Special Papers, 401, 155–170, 2006.
Brauer, A., Endres, C., and Negendank, J. F.: Lateglacial calendar year
chronology based on annually laminated sediments from Lake Meerfelder Maar,
Germany, Quaternary Int., 61, 17–25, 1999.
Brauer, A., Mangili, C., Moscariello, A., and Witt, A.: Palaeoclimatic
implications from micro-facies data of a 5900 varve time series from the
Piànico interglacial sediment record, southern Alps, Palaeogeogr.
Palaeoclim., 259, 121–135, 2008.
Broomhead, D. S. and King, G. P.: Nonlinear phenomena and chaos, On the
Qualitative Analysis of Experimental Dynamical Systems, Malvern science
series,Adam Hilger ltd., Bristol and Boston
Adam Hilger, Bristol, UK, 113–144, 1986.
Campins, J., Genovés, A., Picornell, M., and Jansà, A.: Climatology
of Mediterranean cyclones using the ERA-40 dataset, Int. J.
Climatol., 31, 1596–1614, 2011.
Coianiz, L., Ben-Avraham, Z., Stein, M., and Lazar, M.: Spatial and temporal
reconstruction of the late Quaternary Dead Sea sedimentary facies from
geophysical properties, J. Appl. Geophys., 160, 15–27, 2019.
Crouvi, O., Amit, R., Ben Israel, M., and Enzel, Y.: Loess in the Negev
desert: sources, loessial soils, palaeosols, and palaeoclimatic
implications, in: Quaternary of the Levant: Environments, Climate Change,
and Humans, edited by: Enzel, Y. and
Bar-Yosef, O., Cambridge University Press, Cambridge, 471–482, 2017.
Dayan, U. and Morin, E.: Flash flood–producing rainstorms over the Dead
Sea: A review, Geol. Soc. Am. Special Papers, 401, 53–62,
2006.
Dean, J. R., Eastwood, W. J., Roberts, N., Jones, M. D., Yiğitbaşıoğlu, H., Allcock, S. L., Woodbridge, J., Metcalfe, S. E., and Leng, M.
J.: Tracking the hydro-climatic signal from lake to sediment: A field study
from central Turkey, J. Hydrol., 529, 608–621, 2015.
Donges, J. F., Donner, R. V., Trauth, M. H., Marwan, N., Schellnhuber,
H.-J., and Kurths, J.: Nonlinear detection of paleoclimate-variability
transitions possibly related to human evolution, P. Natl.
Acad. Sci. USA, 108, 20422–20427, 2011.
Drori, R., Ziv, B., Saaroni, H., Etkin, A., and Sheffer, E.: Recent changes
in the rain regime over the Mediterranean climate region of Israel, Climatic
Change, 167, 1–21, https://doi.org/10.1007/s10584-021-03161-6, 2021.
Eckmann, J. P., Kamphorst, S. O. and Ruelle, D.: Recurrence plots of dynamical systems, World Scientific Series on Nonlinear Science Series A, 16, 441–446, 1995.
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, Quaternary Res.,
60, 263–273, 2003.
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, 2008.
Enzel, Y., Amit, R., Grodek, T., Ayalon, A., Lekach, J., Porat, N., Bierman,
P., Blum, J. D., and Erel, Y.: Late Quaternary weathering, erosion, and
deposition in Nahal Yael, Israel: An “impact of climatic change on an arid
watershed”?, Bulletin, 124, 705–722, 2012.
Feldstein, S. B. and Dayan, U.: Circumglobal teleconnections and wave
packets associated with Israeli winter precipitation, Q. J.
Roy. Meteor. Soc., 134, 455–467, 2008.
Feliks, Y., Ghil, M., and Robertson, A. W.: Oscillatory climate modes in the
Eastern Mediterranean and their synchronization with the North Atlantic
Oscillation, J. Climate, 23, 4060–4079, 2010.
Flocas, H. A., Simmonds, I., Kouroutzoglou, J., Keay, K., Hatzaki, M.,
Bricolas, V., and Asimakopoulos, D.: On cyclonic tracks over the eastern
Mediterranean, J. Climate, 23, 5243–5257, 2010.
Ganor, E. and Foner, H.: The mineralogical and chemical properties and the
behaviour of aeolian Saharan dust over Israel, in: The impact of desert dust
across the Mediterranean, Springer, Kluwer Academic Publishers, Dordrecht, The Netherlands, 163–172, 1996.
Garber, R. A., Levy, Y., and Friedman, G. M.: The sedimentology of the Dead
Sea, Carbonate. Evaporite., 2, 43–57, 1987.
Garfunkel, Z.: Internal structure of the Dead Sea leaky transform (rift) in
relation to plate kinematics, Tectonophysics, 80, 81–108, 1981.
Garfunkel, Z. and Ben-Avraham, Z.: The structure of the Dead Sea basin,
Tectonophysics, 266, 155–176, 1996.
Ghil, M., Allen, M., Dettinger, M., Ide, K., Kondrashov, D., Mann, M.,
Robertson, A. W., Saunders, A., Tian, Y., and Varadi, F.: Advanced spectral
methods for climatic time series, Rev. Geophys., 40, 3-1–3-41,
https://doi.org/10.1029/2000RG000092,
2002.
Goldreich, Y.: Spatial Distribution of Mid-season Rainfall Date in Israel –
a Review, Horizons in Geography, 177–182, 2004.
Goldreich, Y.: The climate of Israel: observation, research and application,
Springer Science & Business Media, Kluwer Academic/Plenum Publishers, New York, USA, ISBN: 978-1-4615-0697-3, 2012.
Goldreich, Y., Mozes, H., and Rosenfeld, D.: Radar analysis of cloud systems
and their rainfall yield in Israel, Israel J. Earth Sci., 53, 63–76, 2004.
Goldsmith, Y., Polissar, P., Ayalon, A., Bar-Matthews, M., and Broecker, W.:
The modern and Last Glacial Maximum hydrological cycles of the Eastern
Mediterranean and the Levant from a water isotope perspective, Earth Planet.
Sc. Lett., 457, 302–312, 2017.
Greenbaum, N., Ben-Zvi, A., Haviv, I., and Enzel, Y.: The hydrology and
paleohydrology of the Dead Sea tributaries, Geol. Soc. Am.
Special Papers, 401, 63–93, 2006.
Greenbaum, N., Schwartz, U., and Bergman, N.: Extreme floods and short-term
hydroclimatological fluctuations in the hyper-arid Dead Sea region, Israel,
Global Planet. Change, 70, 125–137, 2010.
Grinsted, A., Moore, J. C., and Jevrejeva, S.: Application of the cross wavelet transform and wavelet coherence to geophysical time series, Nonlin. Processes Geophys., 11, 561–566, https://doi.org/10.5194/npg-11-561-2004, 2004.
Groth, A: SSA tutorial, University of California, Los Angeles, available at: https://dept.atmos.ucla.edu/tcd/ssa-tutorial-matlab (last access: 27 June 2021), 2016.
Haase-Schramm, A., Goldstein, S. L., and Stein, M.: U-Th dating of Lake
Lisan (late Pleistocene dead sea) aragonite and implications for glacial
east Mediterranean climate change, Geochim. Cosmochim. Ac., 68, 985–1005,
https://doi.org/10.1016/j.gca.2003.07.016, 2004.
Heim, C., Nowaczyk, N. R., Negendank, J. F., Leroy, S. A., and Ben-Avraham,
Z.: Near East desertification: evidence from the Dead Sea,
Naturwissenschaften, 84, 398–401, 1997.
Held, I. M. and Soden, B. J.: Robust responses of the hydrological cycle to
global warming, J. Climate, 19, 5686–5699, 2006.
Hochman, A., Saaroni, H., Abramovich, F., and Alpert, P.: Artificial
Detection of Lower-Frequency Periodicity in Climatic Studies by Wavelet
Analysis Demonstrated on Synthetic Time Series, J. Appl.
Meteorol. Clim., 58, 2077–2086, 2019.
IPCC: Climate Change 2021: The Physical Science
Basis, edited by: Zhai, V. P., Pirani, A. S., Connors, L., Péan, C., Berger, S.,
Caud, N., Chen, Y., Goldfarb, L., Gomis, M. I., Huang, M., Leitzell, K.,
Lonnoy, J. B. E., Matthews, R., Maycock, T. K., Waterfield, T., Yelekçi,
O., Yu, R., and Zhou, B., Cambridge University Press, in press, 2021.
Israel Meteorological Service: Climatic data in Israel (1995–2009), available at https://ims.gov.il/he/ClimateAtlas (last access: 27 June 2021), Israel Meteorological Service
[dataset], 2021.
Kagan, E., Stein, M., and Marco, S.: Integrated Paleoseismic Chronology of
the Last Glacial Lake Lisan: From Lake Margin Seismites to Deep-Lake Mass
Transport Deposits, J. Geophys. Res.-Sol. Ea., 123, 2806–2824, https://doi.org/10.1002/2017JB014117, 2018.
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, 2002.
Kalderon-Asael, B., Erel, Y., Sandler, A., and Dayan, U.: Mineralogical and
chemical characterization of suspended atmospheric particles over the east
Mediterranean based on synoptic-scale circulation patterns, Atmos.
Environ., 43, 3963–3970, 2009.
Katz, A., Kolodny, Y., and Nissenbaum, A.: The geochemical evolution of the
Pleistocene Lake Lisan-Dead Sea system, Geochim. Cosmochim. Ac., 41,
1609–1626, https://doi.org/10.1016/0016-7037(77)90172-7, 1977.
Kaufman, A.: U-Series dating of Dead Sea Basin carbonates, Geochim.
Cosmochim. Ac., 35, 1269–1281,
https://doi.org/10.1016/0016-7037(71)90115-3, 1971.
Keinan, J., Bar-Matthews, M., Ayalon, A., Zilberman, T., Agnon, A., and
Frumkin, A.: Paleoclimatology of the Levant from Zalmon Cave speleothems,
the northern Jordan Valley, Israel, Quaternary Sci. Rev., 220,
142–153, 2019.
Kelley, C., Ting, M., Seager, R., and Kushnir, Y.: Mediterranean
precipitation climatology, seasonal cycle, and trend as simulated by CMIP5,
Geophys. Res. Lett., 39, L21703,
https://doi.org/10.1029/2012GL053416, 2012.
Kennel, M. B., Brown, R., and Abarbanel, H. D.: Determining embedding
dimension for phase-space reconstruction using a geometrical construction,
Phys. Rev. A, 45, 3403, https://doi.org/10.1103/PhysRevA.45.3403, 1992.
Kitagawa, H., Stein, M., Goldstein, S. L., Nakamura, T., and Lazar, B.:
Radiocarbon chronology of the DSDDP core at the deepest floor of the Dead
Sea, Radiocarbon, 59, 383–394, https://doi.org/10.1017/RDC.2016.120, 2017.
Kolodny, Y., Stein, M., and Machlus, M.: Sea-rain-lake relation in the Last
Glacial East Mediterranean revealed by δ18O-δ13C in Lake
Lisan aragonites, Geochim. Cosmochim. Ac., 69, 4045–4060, https://doi.org/10.1016/j.gca.2004.11.022, 2005.
Kondrashov, D. and Ghil, M.: Spatio-temporal filling of missing points in geophysical data sets, Nonlin. Processes Geophys., 13, 151–159, https://doi.org/10.5194/npg-13-151-2006, 2006.
Kottek, M., Grieser, J., Beck, C., Rudolf, B., and Rubel, F.: World map of
the Köppen-Geiger climate classification updated, Meteorol.
Z., 15, 259–263, 2006.
Krichak, S., Kishcha, P., and Alpert, P.: Decadal trends of main Eurasian
oscillations and the Eastern Mediterranean precipitation, Theor.
Appl. Climatol., 72, 209–220, 2002.
Kushnir, Y., Dayan, U., Ziv, B., Morin, E., and Enzel, Y.: Climate of the
Levant, in: Quaternary of the Levant, edited by: Enzel, Y. and Bar-Yosef,
O., Cambridge University Press, Cambridge, 31–44, https://doi.org/10.1017/9781316106754.004,
2017.
Lau, K. and Weng, H.: Climate signal detection using wavelet transform: How
to make a time series sing, B. Am. Meteorol. Soc.,
76, 2391–2402, 1995.
Le Mouël, J. L., Lopes, F., and Courtillot, V.: A Solar Signature in
Many Climate Indices, J. Geophys. Res.-Atmos., 124, 2600–2619,
https://doi.org/10.1029/2018JD028939, 2019.
Levy, Y., Burg, A., Yechieli, Y., and Gvirtzman, H.: Displacement of springs
and changes in groundwater flow regime due to the extreme drop in adjacent
lake levels: The Dead Sea rift, J. Hydrol., 587, 124928, https://doi.org/10.1016/j.jhydrol.2020.124928, 2020.
Lisiecki, L. E. and Raymo, M. E.: A Pliocene-Pleistocene stack of 57
globally distributed benthic δ18O records, Paleoceanography, 20, https://doi.org/10.1029/2004PA001071,
2005.
Luck, M., Landis, M., and Gassert, F.: Aqueduct water stress projections:
decadal projections of water supply and demand using CMIP5 GCMs, Technical
Note, Washington, DC: World Resources Institute, available at:
http://www.wri.org/publication/aqueduct-waterstress-projections (last access: 10 January 2020), 2015.
Luo, T., Young, R., and Reig, P.: Aqueduct Projected Water Stress Country
Rankings, Technical Note, Washington, D.C., World Resources Institute, available at:
http://www.wri.org/publication/aqueduct-projected-water-stresscountry-rankings (last access: 1 August 2021), 2015.
Machlus, M., Enzel, Y., Goldstein, S. L., Marco, S., and Stein, M.:
Reconstructing low levels of Lake Lisan by correlating fan-delta and
lacustrine deposits, Quatern. Int., 73, 137–144, 2000.
Mann, H. B. and Whitney, D. R.: On a test of whether one of two random
variables is stochastically larger than the other, Ann.
Math. Stat., 18, 50–60, 1947.
Marco, S., Stein, M., Agnon, A., and Ron, H.: Long-term earthquake
clustering: A 50,000-year paleoseismic record in the Dead Sea Graben,
J. Geophys. Res.-Sol. Ea., 101, 6179–6191, 1996.
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.
Marwan, N.: How to avoid potential pitfalls in recurrence plot based data
analysis, Int. J. Bifurcat. Chaos, 21, 1003–1017,
2011.
Marwan, N.: Cross Recurrence Plot Toolbox for Matlab [code], available at: https://tocsy.pik-potsdam.de/CRPtoolbox/ (last access: 1 July 2021), 2016.
Marwan, N. and Kurths, J.: Cross recurrence plots and their applications, in: Mathematical physics research at the cutting edge, edited by: Benton, C. V., Nova Science Pub Inc, New York, USA, 101–139, 2004.
Marwan, N., Romano, M. C., Thiel, M., and Kurths, J.: Recurrence plots for
the analysis of complex systems, Phys. Rep., 438, 237–329, 2007.
Marwan, N., Trauth, M. H., Vuille, M., and Kurths, J.: Comparing modern and
Pleistocene ENSO-like influences in NW Argentina using nonlinear time series
analysis methods, Clim. Dynam., 21, 317–326, 2003.
Metzger, A., Marra, F., Smith, J. A., and Morin, E.: Flood frequency
estimation and uncertainty in arid/semi-arid regions, J. Hydrol.,
590, 125254, https://doi.org/10.1016/j.jhydrol.2020.125254, 2020.
Migowski, C., Stein, M., Prasad, S., Negendank, J. F., and Agnon, A.:
Holocene climate variability and cultural evolution in the Near East from
the Dead Sea sedimentary record, Quaternary Res., 66, 421–431, 2006.
Morin, E.: To know what we cannot know: Global mapping of minimal detectable
absolute trends in annual precipitation, Water Resour. Res., 47, https://doi.org/10.1029/2010WR009798, 2011.
Morin, E., Ryb, T., Gavrieli, I., and Enzel, Y.: Mean, variance, and trends
of Levant precipitation over the past 4500 years from reconstructed Dead Sea
levels and stochastic modeling, Quaternary Res., 91, 751–767, 2019.
Neev, D.: Recent precipitation of calcium salts in the Dead Sea, Bull. Res.
Council Israel Sect. G, 11, 153–154, 1963.
Neev, D. and Emery, K. O.: The Dead Sea: depositional processes and
environments of evaporites, Ministry of Commerce and Industry, Geological
Survey of Israel, Jerusalem, 1967.
Nehorai, R., Lensky, I., Hochman, L., Gertman, I., Brenner, S., Muskin, A.,
and Lensky, N.: Satellite observations of turbidity in the Dead Sea, J.
Geophys. Res.-Oceans, 118, 3146–3160, 2013.
Neugebauer, I., Brauer, A., Schwab, M. J., Waldmann, N. D., Enzel, Y.,
Kitagawa, H., Torfstein, A., Frank, U., Dulski, P., and Agnon, A.: Lithology
of the long sediment record recovered by the ICDP Dead Sea Deep Drilling
Project (DSDDP), Quaternary Sci. Rev., 102, 149–165, 2014.
Neugebauer, I., Brauer, A., Schwab, M. J., Dulski, P., Frank, U.,
Hadzhiivanova, E., Kitagawa, H., Litt, T., Schiebel, V., and Taha, N.:
Evidences for centennial dry periods at ∼ 3300
and ∼ 2800 cal. yr BP from micro-facies analyses of the Dead
Sea sediments, Holocene, 25/8, 1358–1371, https://doi.org/10.1177/0959683615584208, 2015.
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.
Nissenbaum, A., Baedecker, M. J., and Kaplan, I. R.: Organic geochemistry of
Dead Sea sediments, Geochim. Cosmochim. Ac., 36, 709–727, 1972.
NOAA Climate Prediction Center: teleconnection patterns, NOAA Climate Prediction Center [data set], available at:
https://www.cpc.ncep.noaa.gov/data/teledoc/telecontents.shtml, last access: 10 February
2020.
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, Quaternary Res., 87, 168–179, 2017.
Peleg, N., Bartov, M., and Morin, E.: CMIP5-predicted climate shifts over
the East Mediterranean: implications for the transition region between
Mediterranean and semi-arid climates, Int. J. Climatol.,
35, 2144–2153, 2015.
Prasad, S., Vos, H., Negendank, J., Waldmann, N., Goldstein, S. L., and
Stein, M.: Evidence from Lake Lisan of solar influence on decadal-to
centennial-scale climate variability during marine oxygen isotope stage 2,
Geology, 32, 581–584, 2004.
Prasad, S., Negendank, J., and Stein, M.: Varve counting reveals high
resolution radiocarbon reservoir age variations in palaeolake Lisan, J. Quaternary Sci.,
24, 690–696, 2009.
Redmond, K. T., Enzel, Y., House, P. K., and Biondi, F.: Climate variability
and flood frequency at decadal to millennial time scales, Water Sci. Appl., 5,
21–45, 2002.
Roeser, P., Dräger, N., Brykała, D., Ott, F., Pinkerneil, S.,
Gierszewski, P., Lindemann, C., Plessen, B., Brademann, B., Kaszubski, M.,
Fojutowski, M., Schwab, M. J., Słowiński, M., Błaszkiewicz, M., and
Brauer, A.: Advances in understanding calcite varve formation: new insights
from a dual lake monitoring approach in the southern Baltic lowlands,
Boreas, 50, 419–440, https://doi.org/10.1111/bor.12506, 2021.
Rohling, E. J.: Quantitative assessment of glacial fluctuations in the level
of Lake Lisan, Dead Sea rift, Quaternary Sci. Rev., 70, 63–72, https://doi.org/10.1016/j.quascirev.2013.03.013, 2013.
Romano, M. C., Thiel, M., Kurths, J., and von Bloh, W.: Multivariate
recurrence plots, Phys. Lett. A, 330, 214–223, 2004.
Ryb, U., Matmon, A., Erel, Y., Haviv, I., Benedetti, L., and Hidy, A.:
Styles and rates of long-term denudation in carbonate terrains under a
Mediterranean to hyper-arid climatic gradient, Earth Planet. Sc. Lett.,
406, 142–152, 2014.
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, 2010.
Safriel, U., Adeel, Z., Niemeijer, D., Puigdefabregas, J., White, R., Lal,
R., Winslow, M., Ziedler, J., Prince, S., and Archer, E.: Dryland systems,
in: Ecosystems and Human Well-being: Current State and Trends: Findings of
the Condition and Trends Working Group, Island Press, Washington, DC, 623–662, 2005.
Schinkel, S., Dimigen, O., and Marwan, N.: Selection of recurrence threshold
for signal detection, Eur. Phys. J.-Spec. Top., 164,
45–53, 2008.
Schulte, J. A.: Cumulative areawise testing in wavelet analysis and its application to geophysical time series, Nonlin. Processes Geophys., 23, 45–57, https://doi.org/10.5194/npg-23-45-2016, 2016.
Schulte, J. A.: Statistical hypothesis testing in wavelet analysis: theoretical developments and applications to Indian rainfall, Nonlin. Processes Geophys., 26, 91–108, https://doi.org/10.5194/npg-26-91-2019, 2019.
Schulte, J. A., Georgas, N., Saba, V., and Howell, P.: North Pacific
influences on Long Island sound temperature variability, J. Climate,
31, 2745–2769, 2018.
Seager, R., Osborn, T. J., Kushnir, Y., Simpson, I. R., Nakamura, J., and
Liu, H.: Climate variability and change of Mediterranean-type climates,
J. Climate, 32, 2887–2915, 2019.
Seager, R., Liu, H., Kushnir, Y., Osborn, T. J., Simpson, I. R., Kelley, C.
R., and Nakamura, J.: Mechanisms of Winter Precipitation Variability in the
European–Mediterranean Region Associated with the North Atlantic
Oscillation, J. Climate, 33, 7179–7196, 2020.
Serinaldi, F., Kilsby, C. G., and Lombardo, F.: Untenable nonstationarity:
An assessment of the fitness for purpose of trend tests in hydrology,
Adv. Water Res., 111, 132–155, 2018.
Sharon, D.: The spottiness of rainfall in a desert area, J.
Hydrol., 17, 161–175, 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, 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,
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, https://doi.org/10.1029/2011JD016004, 2011.
Siebert, C., Rodiger, T., Mallast, U., Grabe, A., Guttman, J., Laronne, J.
B., Storz-Peretz, Y., Greenman, A., Salameh, E., Al-Raggad, M., Vachtman,
D., Zvi, A. B., Ionescu, D., Brenner, A., Merz, R., and Geyer, S.:
Challenges to estimate surface- and groundwater flow in arid regions: the
Dead Sea catchment, Sci. Total Environ., 485–486, 828–841, https://doi.org/10.1016/j.scitotenv.2014.04.010, 2014.
Sirota, I., Enzel, Y., and Lensky, N. G.: Temperature seasonality control on
modern halite layers in the Dead Sea: In situ observations, Geol.
Soc. Am. Bull., 129, 1181–1194,
https://doi.org/10.1130/B31661.1, 2017.
Sirota, I., Enzel, Y., and Lensky, N. G.: Halite focusing and amplification
of salt layer thickness: From the Dead Sea to deep hypersaline basins,
Geology, 46, 851–854,
https://doi.org/10.1130/G45339.1, 2018.
Stein, M., Starinsky, A., Katz, A., Goldstein, S. L., Machlus, M., and
Schramm, A.: Strontium isotopic, chemical, and sedimentological evidence for
the evolution of Lake Lisan and the Dead Sea, Geochim. Cosmochim. Ac., 61,
3975–3992, 1997.
Stöckli, R., Vermote, E., Saleous, N., Simmon, R., and Herring, D.: The
Blue Marble Next Generation-A true color earth dataset including seasonal
dynamics from MODIS, published by the NASA Earth Observatory, available at: https://earthobservatory.nasa.gov/ContentFeature/BlueMarble/bmng.pdf (last access: 15 November 2017), 2005.
Swierczynski, T., Brauer, A., Lauterbach, S., Martín-Puertas, C.,
Dulski, P., von Grafenstein, U., and Rohr, C.: A 1600 yr seasonally resolved
record of decadal-scale flood variability from the Austrian Pre-Alps,
Geology, 40, 1047–1050, 2012.
Tamarin-Brodsky, T. and Kaspi, Y.: Enhanced poleward propagation of storms
under climate change, Nat. Geosci., 10, 908–913, https://doi.org/10.1038/s41561-017-0001-8, 2017.
Tarolli, P., Borga, M., Morin, E., and Delrieu, G.: Analysis of flash flood regimes in the North-Western and South-Eastern Mediterranean regions, Nat. Hazards Earth Syst. Sci., 12, 1255–1265, https://doi.org/10.5194/nhess-12-1255-2012, 2012.
Torfstein, A. and Enzel, Y.: Dead Sea Lake Level Changes and Levant
Palaeoclimate, in: Quaternary of the Levant, edited by: Enzel, Y. and
Bar-Yosef, O., Cambridge University Press, Cambridge, 115–126, https://doi.org/10.1017/9781316106754.013, 2017.
Torfstein, A., Gavrieli, I., Katz, A., Kolodny, Y., and Stein, M.: Gypsum as
a monitor of the paleo-limnological–hydrological conditions in Lake Lisan
and the Dead Sea, Geochim. Cosmochim. Ac., 72, 2491–2509, 2008.
Torfstein, A., Haase-Schramm, A., Waldmann, N., Kolodny, Y., and Stein, M.:
U-series and oxygen isotope chronology of the mid-Pleistocene Lake Amora
(Dead Sea basin), Geochim. Cosmochim. Ac., 73, 2603–2630, 2009.
Torfstein, A., Goldstein, S. L., Kagan, E. J., and Stein, M.: Integrated
multi-site U–Th chronology of the last glacial Lake Lisan, Geochim.
Cosmochim. Ac., 104, 210–231, 2013a.
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, 2013b.
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, 2015.
Torrence, C. and Compo, G. P.: A practical guide to wavelet analysis,
B. Am. Meteorol. Soc., 79, 61–78, 1998.
Tsvieli, Y. and Zangvil, A.: Synoptic climatological analysis of “wet” and
“dry” Red Sea troughs over Israel, Int. J. Climatol., 25,
1997–2015, 2005.
Tubi, A. and Dayan, U.: Tropical Plumes over the Middle East: Climatology
and synoptic conditions, Atmos. Res., 145, 168–181, 2014.
Tyrlis, E., Lelieveld, J., and Steil, B.: The summer circulation over the
eastern Mediterranean and the Middle East: influence of the South Asian
monsoon, Clim. Dynam., 40, 1103–1123, 2013.
Vautard, R. and Ghil, M.: Singular spectrum analysis in nonlinear dynamics,
with applications to paleoclimatic time series, Physica D, 35, 395–424, 1989.
Waldmann, N., Neugebauer, I., Palchan, D., Hadzhiivanova, E., Taha, N.,
Brauer, A., and Enzel, Y.: Sedimentology of the Lacustrine Formations in the
Dead Sea Basin, in: Quaternary of the Levant: Environments, Climate Change,
and Humans, edited by: Enzel, Y. and Bar-Yosef, O., Cambridge University
Press, Cambridge, 83–90, https://doi.org/10.1017/9781316106754.009, 2017.
Welch, P. D.: The use of fast Fourier transform for the estimation of power
spectra: A method based on time averaging over short, modified periodograms,
IEEE T. Acoust. Speech, 15, 70–73, 1967.
Witt, A., Malamud, B. D., Mangili, C., and Brauer, A.: Analysis and modelling of a 9.3 kyr palaeoflood record: correlations, clustering, and cycles, Hydrol. Earth Syst. Sci., 21, 5547–5581, https://doi.org/10.5194/hess-21-5547-2017, 2017.
Yosef, Y., Aguilar, E., and Alpert, P.: Changes in extreme temperature and
precipitation indices: using an innovative daily homogenized database in
Israel, Int. J. Climatol., 39, 5022–5045, 2019.
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.
Ziv, B.: A subtropical rainstorm associated with a tropical plume overAfrica
and the Middle-East, Theor. Appl. Climatol., 69, 91–102, 2001.
Ziv, B., Saaroni, H., and Alpert, P.: The factors governing the summer
regime of the eastern Mediterranean, Int. J. Climatol.,
24, 1859–1871, 2004.
Ziv, B., Dayan, U., Kushnir, Y., Roth, C., and Enzel, Y.: Regional and
global atmospheric patterns governing rainfall in the southern Levant,
Int. J. Climatol., 26, 55–73, 2006.
Zolitschka, B., Francus, P., Ojala, A. E., and Schimmelmann, A.: Varves in
lake sediments – a review, Quaternary Sci. Rev., 117, 1–41, 2015.
Short summary
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.
Laminated sediments from the deepest part of the Dead Sea unravel the hydrological response of...
