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Sources and transport routes of fine detritus material to the Late Quaternary Dead Sea basin

Quaternary science reviews, 2012-09, Vol.50, p.55-70

2012

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The extent of seawater circulation in the aquifer and its role in elemental mass balances: A lesson from the Dead Sea

Earth and planetary science letters, 2014-05, Vol.394, p.146-158

2014

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Primary carbonates and Ca-chloride brines as monitors of a paleo-hydrological regime in the Dead Sea basin

Quaternary science reviews, 2007-09, Vol.26 (17), p.2219-2228

2007

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Mornings with the highest non‐rainfall water during 2 years of measurements in the Negev–Ecological implications

Hydrological processes, 2024-05, Vol.38 (5), p.n/a

2024

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The enigmatic enrichment of potassium and magnesium in runoff and floodwater in the Negev: Do biocrusts hold the key?

The Science of the total environment, 2024-02, Vol.911, p.168753-168753, Article 168753

2024

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Essential nutritional ions show enrichment (K + , Mg 2+ ) and depletion ( NO 3 − ) in runoff water generated by biocrusts covering arid sand dunes under natural rain conditions

Hydrological processes, 2024-09, Vol.38 (9)

2024

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No drawdown and no hyperaridity in the ancient Dead Sea: (Comments to Torfstein's et al. (2015) paper, EPSL 412, 235–244)

Earth and planetary science letters, 2015-10, Vol.427, p.303-305

2015

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Mechanisms for biocrust-modulated runoff generation – A review

Earth-science reviews, 2022-08, Vol.231, p.104100, Article 104100

2022

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Measurements and ecological implications of non‐rainfall water in desert ecosystems—A review

Ecohydrology, 2019-09, Vol.12 (6), p.n/a

2019

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No drawdown and no hyperaridity in the ancient Dead Sea

Earth and planetary science letters, 2015-10, Vol.427, p.303-305

2015

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Even in a dew desert: Dewfall does not provide sufficient moisture for biocrust growth – Evidence from direct measurements and a meteorological model

Journal of hydrology (Amsterdam), 2023-12, Vol.627, p.130450, Article 130450

2023

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The consequences of using microlysimeters: Why microlysimeters grossly overestimate dew amounts in arid regions? A critical review

The Science of the total environment, 2024-10, Vol.947, p.174640, Article 174640

2024

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The behavior of lithium and its isotopes in oilfield brines: evidence from the Heletz-Kokhav field, Israel

Geochimica et cosmochimica acta, 2002-02, Vol.66 (4), p.615-623

2002

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Hypolith Distribution Within a Dewy Drainage Basin: Possible Link to Dew or Rather to Rain?

Ecohydrology, 2024-10

2024

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Mornings with the highest non‐rainfall water during 2years of measurements in the Negev–Ecological implications

Hydrological processes, 2024-05, Vol.38 (5)

2024

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Drought effect on biocrust resilience: High-speed winds result in crust burial and crust rupture and flaking

The Science of the total environment, 2017-02, Vol.579, p.848-859

2017

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Application of radon and radium isotopes to groundwater flow dynamics: An example from the Dead Sea

Chemical geology, 2015-09, Vol.411, p.155-171

2015

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Groundwater ages and reaction rates during seawater circulation in the Dead Sea aquifer

Geochimica et cosmochimica acta, 2013-12, Vol.122, p.17-35

2013

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Ra isotopes and Rn in brines and ground waters of the Jordan-Dead Sea Rift Valley: enrichment, retardation, and mixing

Geochimica et cosmochimica acta, 2000-07, Vol.64 (14), p.2371-2388

2000

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Geochemical History of the Dead Sea

Aquatic geochemistry, 2009-02, Vol.15 (1-2), p.159-194

2009

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The effect of the water source on niche partioning of chlorolichens and cyanobacteria—implications for resilience?

Planta, 2023-07, Vol.258 (1), p.8-8, Article 8

2023

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Wind as a cooling agent: substrate temperatures are responsible for variable lithobiont-induced weathering patterns on west- and east-facing limestone bedrock of the Negev

Earth surface processes and landforms, 2016-11, Vol.41 (14), p.2078-2084

2016

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Wet–dry cycles on sandy and loessial Negev soils: Implications for biocrust establishment and growth?

Ecohydrology, 2022-03, Vol.15 (2), p.n/a

2022

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Cyanobacteria are confined to dewless habitats within a dew desert: Implications for past and future climate change for lithic microorganisms

Journal of hydrology (Amsterdam), 2014-11, Vol.519, p.3606-3614

2014

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Late Quaternary changes in desert dust inputs to the Red Sea and Gulf of Aden from 87Sr/ 86Sr ratios in deep-sea cores

Earth and planetary science letters, 2007-09, Vol.261 (1), p.104-119

2007

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Sources and transport routes of fine detritus material to the Late Quaternary Dead Sea basin

The extent of seawater circulation in the aquifer and its role in elemental mass balances: A lesson from the Dead Sea

Primary carbonates and Ca-chloride brines as monitors of a paleo-hydrological regime in the Dead Sea basin

Mornings with the highest non‐rainfall water during 2 years of measurements in the Negev–Ecological implications

The enigmatic enrichment of potassium and magnesium in runoff and floodwater in the Negev: Do biocrusts hold the key?

Essential nutritional ions show enrichment (K + , Mg 2+ ) and depletion ( NO 3 − ) in runoff water generated by biocrusts covering arid sand dunes under natural rain conditions

No drawdown and no hyperaridity in the ancient Dead Sea: (Comments to Torfstein's et al. (2015) paper, EPSL 412, 235–244)

Mechanisms for biocrust-modulated runoff generation – A review

Measurements and ecological implications of non‐rainfall water in desert ecosystems—A review

No drawdown and no hyperaridity in the ancient Dead Sea

Even in a dew desert: Dewfall does not provide sufficient moisture for biocrust growth – Evidence from direct measurements and a meteorological model

The consequences of using microlysimeters: Why microlysimeters grossly overestimate dew amounts in arid regions? A critical review

The behavior of lithium and its isotopes in oilfield brines: evidence from the Heletz-Kokhav field, Israel

Hypolith Distribution Within a Dewy Drainage Basin: Possible Link to Dew or Rather to Rain?

Mornings with the highest non‐rainfall water during 2years of measurements in the Negev–Ecological implications

Drought effect on biocrust resilience: High-speed winds result in crust burial and crust rupture and flaking

Application of radon and radium isotopes to groundwater flow dynamics: An example from the Dead Sea

Groundwater ages and reaction rates during seawater circulation in the Dead Sea aquifer

Ra isotopes and Rn in brines and ground waters of the Jordan-Dead Sea Rift Valley: enrichment, retardation, and mixing

Geochemical History of the Dead Sea

The effect of the water source on niche partioning of chlorolichens and cyanobacteria—implications for resilience?

Wind as a cooling agent: substrate temperatures are responsible for variable lithobiont-induced weathering patterns on west- and east-facing limestone bedrock of the Negev

Wet–dry cycles on sandy and loessial Negev soils: Implications for biocrust establishment and growth?

Cyanobacteria are confined to dewless habitats within a dew desert: Implications for past and future climate change for lithic microorganisms

Late Quaternary changes in desert dust inputs to the Red Sea and Gulf of Aden from 87Sr/ 86Sr ratios in deep-sea cores

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