Articles | Volume 9, issue 3
https://doi.org/10.5194/esd-9-1141-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esd-9-1141-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
27 Sep 2018
Research article |
| 27 Sep 2018
| 27 Sep 2018
Pipes to Earth's subsurface: the role of atmospheric conditions in controlling air transport through boreholes and shafts
Elad Levintal
Environmental Hydrology and Microbiology, the Zuckerberg Institute for Water Research, The Jacob Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Midreshet Ben-Gurion 8499000, Israel
Nadav G. Lensky
Geological Survey of Israel, Jerusalem 9550161, Israel
Amit Mushkin
Department of Earth & Space Sciences, University of Washington, Seattle, WA 98105, USA
Environmental Hydrology and Microbiology, the Zuckerberg Institute for Water Research, The Jacob Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Midreshet Ben-Gurion 8499000, Israel
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Do-it-yourself hardware is a new approach for improving measurement resolution in research. Here we present a low-cost, automated system for field measurements of nitrate in soil pore water and open water bodies. All data hardware components cost is $1,100, much cheaper than other available commercial solutions. We provide the complete building guide to reduce any technical barriers, which we hope will allow easier reproducibility and open new soil and environmental monitoring applications.
Elad Levintal, Yonatan Ganot, Gail Taylor, Peter Freer-Smith, Kosana Suvocarev, and Helen E. Dahlke
SOIL, 8, 85–97, https://doi.org/10.5194/soil-8-85-2022, https://doi.org/10.5194/soil-8-85-2022, 2022
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Do-it-yourself hardware is a new approach for improving measurement resolution in research. Here we present a new low-cost, wireless underground sensor network for soil monitoring. All data logging, power, and communication component cost is USD 150, much cheaper than other available commercial solutions. We provide the complete building guide to reduce any technical barriers, which we hope will allow easier reproducibility and open new environmental monitoring applications.
Shai Abir, Hamish A. McGowan, Yonatan Shaked, Hezi Gildor, Efrat Morin, and Nadav G. Lensky
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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 year-1 evaporation rate. Inconsistent with bulk formulae estimation 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.
Sahiti Bulusu, Cristina Prieto García, Helen E. Dahlke, and Elad Levintal
EGUsphere, https://doi.org/10.5194/egusphere-2023-3159, https://doi.org/10.5194/egusphere-2023-3159, 2024
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Do-it-yourself hardware is a new approach for improving measurement resolution in research. Here we present a low-cost, automated system for field measurements of nitrate in soil pore water and open water bodies. All data hardware components cost is $1,100, much cheaper than other available commercial solutions. We provide the complete building guide to reduce any technical barriers, which we hope will allow easier reproducibility and open new soil and environmental monitoring applications.
Ido Arad, Aviya Ziner, Shany Ben Moshe, Noam Weisbrod, and Alex Furman
Hydrol. Earth Syst. Sci., 27, 2509–2522, https://doi.org/10.5194/hess-27-2509-2023, https://doi.org/10.5194/hess-27-2509-2023, 2023
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In a series of long-column experiments, subsurface air injection in soil aquifer treatment (Air-SAT) was tested as an alternative to conventional flooding–drying operation (FDO) in tertiary wastewater (WW) treatment. Our results show that Air-SAT allows for the treatment of increased WW volumes and results in similar or better effluent quality compared with FDO. These results highlight the possibility of using air injection to treat more effluent and alleviate the pressure on existing SAT sites.
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.
Tuvia Turkeltaub, Alex Furman, Ron Mannheim, and Noam Weisbrod
Hydrol. Earth Syst. Sci., 26, 1565–1578, https://doi.org/10.5194/hess-26-1565-2022, https://doi.org/10.5194/hess-26-1565-2022, 2022
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The quality control and optimization of soil aquifer treatment (SAT) performance is challenging due to the multiple factors and costs involved. We installed in situ subsurface monitoring sensors that provided continuous high-resolution monitoring of the biochemical and physical conditions of an active SAT system. Data analysis facilitated the determination of the optimal drying and wetting stages, which are critical for suitable SAT management.
Elad Levintal, Yonatan Ganot, Gail Taylor, Peter Freer-Smith, Kosana Suvocarev, and Helen E. Dahlke
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Shany Ben Moshe, Noam Weisbrod, Felix Barquero, Jana Sallwey, Ofri Orgad, and Alex Furman
Hydrol. Earth Syst. Sci., 24, 417–426, https://doi.org/10.5194/hess-24-417-2020, https://doi.org/10.5194/hess-24-417-2020, 2020
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In soil aquifer treatment (a soil-based treatment for wastewater), infiltration ponds are operated in flooding and drying cycles, and the reclaimed water may be used for irrigation. We tested the effect of hydraulic operation on the biogeochemical system via long-column experiments. We found that longer drying periods not only were beneficial for the upper area of the profile but also increased the volume of the system that maintained oxidizing conditions.
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Hydrol. Earth Syst. Sci., 22, 6323–6333, https://doi.org/10.5194/hess-22-6323-2018, https://doi.org/10.5194/hess-22-6323-2018, 2018
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In recent years, surpluses of desalinated seawater (DSW) are stored in the Israeli coastal aquifer. We monitor DSW spread in the aquifer using the difference between isotope composition of reverse-osmosis DSW and natural fresh water, which simplifies the system to two distinct end-members. A hydrogeological flow and transport model is used to demonstrate the robustness of this simplification, predict the future spread of DSW in the aquifer and mixing in wells, and estimate DSW recovery efficacy.
Yonatan Ganot, Ran Holtzman, Noam Weisbrod, Ido Nitzan, Yoram Katz, and Daniel Kurtzman
Hydrol. Earth Syst. Sci., 21, 4479–4493, https://doi.org/10.5194/hess-21-4479-2017, https://doi.org/10.5194/hess-21-4479-2017, 2017
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We monitor infiltration at multiple scales during managed aquifer recharge with desalinated seawater in an infiltration pond, while groundwater recharge is evaluated by simplified and numerical models. We found that pond-surface clogging is negated by the high-quality desalinated seawater or negligible compared to the low-permeability layers of the unsaturated zone. We show that a numerical model with a 1-D representative sediment profile is able to capture infiltration and recharge dynamics.
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Earth Syst. Dynam., 13, 1077–1096, https://doi.org/10.5194/esd-13-1077-2022, https://doi.org/10.5194/esd-13-1077-2022, 2022
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Earth Syst. Dynam., 13, 1029–1039, https://doi.org/10.5194/esd-13-1029-2022, https://doi.org/10.5194/esd-13-1029-2022, 2022
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Michael J. Prather
Earth Syst. Dynam., 13, 703–709, https://doi.org/10.5194/esd-13-703-2022, https://doi.org/10.5194/esd-13-703-2022, 2022
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Atmospheric CO2 fluctuations point to changes in fossil fuel emissions plus natural and perturbed variations in the natural carbon cycle. One unstudied source of variability is the stratosphere, where the influx of aged CO2-depleted air can cause surface fluctuations. Using modeling and, separately, scaling the observed N2O variability, I find that stratosphere-driven surface variability in CO2 is not a significant uncertainty (at most 10 % of the observed interannual variability).
Matthias Jonas, Rostyslav Bun, Iryna Ryzha, and Piotr Żebrowski
Earth Syst. Dynam., 13, 439–455, https://doi.org/10.5194/esd-13-439-2022, https://doi.org/10.5194/esd-13-439-2022, 2022
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We interpret carbon dioxide emissions from fossil fuel burning and land use as a global stress–strain experiment to reflect the overall behavior of the atmosphere–land and ocean system in response to increasing CO2 emissions since 1850. The system has been trapped progressively in terms of persistence, while its ability to build up memory has been reduced. We expect system failures globally well before 2050 if the current trend in emissions is not reversed immediately and sustainably.
Andreas Lehmann, Kai Myrberg, Piia Post, Irina Chubarenko, Inga Dailidiene, Hans-Harald Hinrichsen, Karin Hüssy, Taavi Liblik, H. E. Markus Meier, Urmas Lips, and Tatiana Bukanova
Earth Syst. Dynam., 13, 373–392, https://doi.org/10.5194/esd-13-373-2022, https://doi.org/10.5194/esd-13-373-2022, 2022
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The salinity in the Baltic Sea is not only an important topic for physical oceanography as such, but it also integrates the complete water and energy cycle. It is a primary external driver controlling ecosystem dynamics of the Baltic Sea. The long-term dynamics are controlled by river runoff, net precipitation, and the water mass exchange between the North Sea and Baltic Sea. On shorter timescales, the ephemeral atmospheric conditions drive a very complex and highly variable salinity regime.
Si Chen, Zhenghui Xie, Jinbo Xie, Bin Liu, Binghao Jia, Peihua Qin, Longhuan Wang, Yan Wang, and Ruichao Li
Earth Syst. Dynam., 13, 341–356, https://doi.org/10.5194/esd-13-341-2022, https://doi.org/10.5194/esd-13-341-2022, 2022
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This study discusses the changes in the summer thermal environment in the Chengdu–Chongqing urban agglomeration due to urban expansion in complex terrain conditions in the recent 40 years, using high-resolution simulations with the WRF model. We quantify the influence of a single urban expansion factor and a single complex terrain factor on the urban thermal environment. Under the joint influence of complex terrain and urban expansion, the heat island effect caused by urbanization was enhanced.
Lisa Jach, Thomas Schwitalla, Oliver Branch, Kirsten Warrach-Sagi, and Volker Wulfmeyer
Earth Syst. Dynam., 13, 109–132, https://doi.org/10.5194/esd-13-109-2022, https://doi.org/10.5194/esd-13-109-2022, 2022
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The land surface can influence the occurrence of local rainfall through different feedback mechanisms. In Europe, this happens most frequently in summer. Here, we examine how differences in atmospheric temperature and moisture change where and how often the land surface can influence rainfall. The results show that the differences barely move the region of strong surface influence over Scandinavia and eastern Europe, but they can change the frequency of coupling events.
Marcus Reckermann, Anders Omstedt, Tarmo Soomere, Juris Aigars, Naveed Akhtar, Magdalena Bełdowska, Jacek Bełdowski, Tom Cronin, Michał Czub, Margit Eero, Kari Petri Hyytiäinen, Jukka-Pekka Jalkanen, Anders Kiessling, Erik Kjellström, Karol Kuliński, Xiaoli Guo Larsén, Michelle McCrackin, H. E. Markus Meier, Sonja Oberbeckmann, Kevin Parnell, Cristian Pons-Seres de Brauwer, Anneli Poska, Jarkko Saarinen, Beata Szymczycha, Emma Undeman, Anders Wörman, and Eduardo Zorita
Earth Syst. Dynam., 13, 1–80, https://doi.org/10.5194/esd-13-1-2022, https://doi.org/10.5194/esd-13-1-2022, 2022
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As part of the Baltic Earth Assessment Reports (BEAR), we present an inventory and discussion of different human-induced factors and processes affecting the environment of the Baltic Sea region and their interrelations. Some are naturally occurring and modified by human activities, others are completely human-induced, and they are all interrelated to different degrees. The findings from this study can largely be transferred to other comparable marginal and coastal seas in the world.
Sebastian Landwehr, Michele Volpi, F. Alexander Haumann, Charlotte M. Robinson, Iris Thurnherr, Valerio Ferracci, Andrea Baccarini, Jenny Thomas, Irina Gorodetskaya, Christian Tatzelt, Silvia Henning, Rob L. Modini, Heather J. Forrer, Yajuan Lin, Nicolas Cassar, Rafel Simó, Christel Hassler, Alireza Moallemi, Sarah E. Fawcett, Neil Harris, Ruth Airs, Marzieh H. Derkani, Alberto Alberello, Alessandro Toffoli, Gang Chen, Pablo Rodríguez-Ros, Marina Zamanillo, Pau Cortés-Greus, Lei Xue, Conor G. Bolas, Katherine C. Leonard, Fernando Perez-Cruz, David Walton, and Julia Schmale
Earth Syst. Dynam., 12, 1295–1369, https://doi.org/10.5194/esd-12-1295-2021, https://doi.org/10.5194/esd-12-1295-2021, 2021
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The Antarctic Circumnavigation Expedition surveyed a large number of variables describing the dynamic state of ocean and atmosphere, freshwater cycle, atmospheric chemistry, ocean biogeochemistry, and microbiology in the Southern Ocean. To reduce the dimensionality of the dataset, we apply a sparse principal component analysis and identify temporal patterns from diurnal to seasonal cycles, as well as geographical gradients and
hotspotsof interaction. Code and data are open access.
Pascal Perolo, Bieito Fernández Castro, Nicolas Escoffier, Thibault Lambert, Damien Bouffard, and Marie-Elodie Perga
Earth Syst. Dynam., 12, 1169–1189, https://doi.org/10.5194/esd-12-1169-2021, https://doi.org/10.5194/esd-12-1169-2021, 2021
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Wind blowing over the ocean creates waves that, by increasing the level of turbulence, promote gas exchange at the air–water interface. In this study, for the first time, we measured enhanced gas exchanges by wind-induced waves at the surface of a large lake. We adapted an ocean-based model to account for the effect of surface waves on gas exchange in lakes. We finally show that intense wind events with surface waves contribute disproportionately to the annual CO2 gas flux in a large lake.
Tommaso Alberti, Reik V. Donner, and Stéphane Vannitsem
Earth Syst. Dynam., 12, 837–855, https://doi.org/10.5194/esd-12-837-2021, https://doi.org/10.5194/esd-12-837-2021, 2021
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We provide a novel approach to diagnose the strength of the ocean–atmosphere coupling by using both a reduced order model and reanalysis data. Our findings suggest the ocean–atmosphere dynamics presents a rich variety of features, moving from a chaotic to a coherent coupled dynamics, mainly attributed to the atmosphere and only marginally to the ocean. Our observations suggest further investigations in characterizing the occurrence and spatial dependency of the ocean–atmosphere coupling.
Alan Bartholet, Glenn A. Milne, and Konstantin Latychev
Earth Syst. Dynam., 12, 783–795, https://doi.org/10.5194/esd-12-783-2021, https://doi.org/10.5194/esd-12-783-2021, 2021
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Improving the accuracy of regional sea-level projections is an important aim that will impact estimates of sea-level hazard around the globe. The computation of sea-level fingerprints is a key component of any such projection, and to date these computations have been based on the assumption that elastic deformation accurately describes the solid Earth response on century timescales. We show here that this assumption is inaccurate in some glaciated regions characterized by low mantle viscosity.
Achim Wirth and Florian Lemarié
Earth Syst. Dynam., 12, 689–708, https://doi.org/10.5194/esd-12-689-2021, https://doi.org/10.5194/esd-12-689-2021, 2021
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We show that modern concepts of non-equilibrium statistical mechanics can be applied to large-scale environmental fluid dynamics, where fluctuations are not thermal but come from turbulence. The work theorems developed by Jarzynski and Crooks are applied to air–sea interaction. Rather than looking at the average values of thermodynamic variables, their probability density functions are considered, which allows us to replace the inequalities of equilibrium statistical mechanics with equalities.
Nico Wunderling, Jonathan F. Donges, Jürgen Kurths, and Ricarda Winkelmann
Earth Syst. Dynam., 12, 601–619, https://doi.org/10.5194/esd-12-601-2021, https://doi.org/10.5194/esd-12-601-2021, 2021
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In the Earth system, climate tipping elements exist that can undergo qualitative changes in response to environmental perturbations. If triggered, this would result in severe consequences for the biosphere and human societies. We quantify the risk of tipping cascades using a conceptual but fully dynamic network approach. We uncover that the risk of tipping cascades under global warming scenarios is enormous and find that the continental ice sheets are most likely to initiate these failures.
Frederik Wolf, Aiko Voigt, and Reik V. Donner
Earth Syst. Dynam., 12, 353–366, https://doi.org/10.5194/esd-12-353-2021, https://doi.org/10.5194/esd-12-353-2021, 2021
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In our work, we employ complex networks to study the relation between the time mean position of the intertropical convergence zone (ITCZ) and sea surface temperature (SST) variability. We show that the information hidden in different spatial SST correlation patterns, which we access utilizing complex networks, is strongly correlated with the time mean position of the ITCZ. This research contributes to the ongoing discussion on drivers of the annual migration of the ITCZ.
Frederik Wolf, Ugur Ozturk, Kevin Cheung, and Reik V. Donner
Earth Syst. Dynam., 12, 295–312, https://doi.org/10.5194/esd-12-295-2021, https://doi.org/10.5194/esd-12-295-2021, 2021
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Motivated by a lacking onset prediction scheme, we examine the temporal evolution of synchronous heavy rainfall associated with the East Asian Monsoon System employing a network approach. We find, that the evolution of the Baiu front is associated with the formation of a spatially separated double band of synchronous rainfall. Furthermore, we identify the South Asian Anticyclone and the North Pacific Subtropical High as the main drivers, which have been assumed to be independent previously.
Margarida L. R. Liberato, Irene Montero, Célia Gouveia, Ana Russo, Alexandre M. Ramos, and Ricardo M. Trigo
Earth Syst. Dynam., 12, 197–210, https://doi.org/10.5194/esd-12-197-2021, https://doi.org/10.5194/esd-12-197-2021, 2021
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Extensive, long-standing dry and wet episodes are frequent climatic extreme events (EEs) in the Iberian Peninsula (IP). A method for ranking regional extremes of persistent, widespread drought and wet events is presented, using different SPEI timescales. Results show that there is no region more prone to EE occurrences in the IP, the most extreme extensive agricultural droughts evolve into hydrological and more persistent extreme droughts, and widespread wet and dry EEs are anti-correlated.
Breno Raphaldini, André S. W. Teruya, Pedro Leite da Silva Dias, Lucas Massaroppe, and Daniel Yasumasa Takahashi
Earth Syst. Dynam., 12, 83–101, https://doi.org/10.5194/esd-12-83-2021, https://doi.org/10.5194/esd-12-83-2021, 2021
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Several recent studies suggest a modulation of the Madden–Julian oscillation (MJO) by the quasi-biennial oscillation (QBO). The physics behind this interaction, however, remain poorly understood. In this study, we investigated the QBO–MJO interaction and the role of stratospheric ozone as a forcing mechanism. A normal-mode decomposition procedure combined with causality analysis reveals significant interactions between MJO-related modes and QBO-related modes.
Derrick K. Danso, Sandrine Anquetin, Arona Diedhiou, Kouakou Kouadio, and Arsène T. Kobea
Earth Syst. Dynam., 11, 1133–1152, https://doi.org/10.5194/esd-11-1133-2020, https://doi.org/10.5194/esd-11-1133-2020, 2020
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The atmospheric and surface conditions that exist during the occurrence of daytime low-level clouds (LLCs) and their influence on solar radiation were investigated in West Africa. During the monsoon season, these LLCs are linked to high moisture flux driven by strong southwesterly winds from the Gulf of Guinea and significant background moisture levels. Their occurrence leads to a strong reduction in the incoming solar radiation and has large impacts on the surface energy budget.
David García-García, Isabel Vigo, and Mario Trottini
Earth Syst. Dynam., 11, 1089–1106, https://doi.org/10.5194/esd-11-1089-2020, https://doi.org/10.5194/esd-11-1089-2020, 2020
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The global water cycle involves water-mass transport on land, in the atmosphere, in the ocean, and among them. The GRACE mission has allowed for the quantification of water-mass variations. It was a revolution in the understanding of Earth dynamics. Here, we develop and apply a novel method, based on GRACE data and atmospheric models, that allows systematic estimation of water-mass exchange among ocean basins. This is valuable for understanding the role of the ocean within the water cycle.
Marie-Noëlle Woillez, Gaël Giraud, and Antoine Godin
Earth Syst. Dynam., 11, 1073–1087, https://doi.org/10.5194/esd-11-1073-2020, https://doi.org/10.5194/esd-11-1073-2020, 2020
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To illustrate the fact that future economic damage from global warming is often highly underestimated, we applied two different statistically based damage functions available in the literature to a global cooling of 4 °C. We show that the gross domestic product (GDP) projections obtained are at odds with the state of the planet during an ice age. We conclude that such functions do not provide relevant information on potential damage from a large climate change, be it cooling or warming.
Jonas Van Breedam, Heiko Goelzer, and Philippe Huybrechts
Earth Syst. Dynam., 11, 953–976, https://doi.org/10.5194/esd-11-953-2020, https://doi.org/10.5194/esd-11-953-2020, 2020
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We made projections of global mean sea-level change during the next 10 000 years for a range in climate forcing scenarios ranging from a peak in carbon dioxide concentrations in the next decades to burning most of the available carbon reserves over the next 2 centuries. We find that global mean sea level will rise between 9 and 37 m, depending on the emission of greenhouse gases. In this study, we investigated the long-term consequence of climate change for sea-level rise.
Praveen Kumar Pothapakula, Cristina Primo, Silje Sørland, and Bodo Ahrens
Earth Syst. Dynam., 11, 903–923, https://doi.org/10.5194/esd-11-903-2020, https://doi.org/10.5194/esd-11-903-2020, 2020
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Information exchange (IE) from the Indian Ocean Dipole (IOD) and El Niño–Southern Oscillation (ENSO) to Indian summer monsoon rainfall (ISMR) is investigated. Observational data show that IOD and ENSO synergistically exchange information on ISMR variability over central India. IE patterns observed in three global climate models (GCMs) differ from observations. Our study highlights new perspectives that IE metrics could bring to climate science.
Min Chen and Ken Caldeira
Earth Syst. Dynam., 11, 875–883, https://doi.org/10.5194/esd-11-875-2020, https://doi.org/10.5194/esd-11-875-2020, 2020
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We examine the implications of future motivation for humans to migrate by analyzing today’s relationships between climatic factors and population density, with all other factors held constant. Such analyses are unlikely to make accurate predictions but can still be useful for informing discussions about the broad range of incentives that might influence migration decisions. Areas with the highest projected population growth rates tend to be the areas most adversely affected by climate change.
Paolo De Luca, Gabriele Messori, Davide Faranda, Philip J. Ward, and Dim Coumou
Earth Syst. Dynam., 11, 793–805, https://doi.org/10.5194/esd-11-793-2020, https://doi.org/10.5194/esd-11-793-2020, 2020
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In this paper we quantify Mediterranean compound temperature and precipitation dynamical extremes (CDEs) over the 1979–2018 period. The strength of the temperature–precipitation coupling during summer increased and is driven by surface warming. We also link the CDEs to compound hot–dry and cold–wet events during summer and winter respectively.
Simon Opie, Richard G. Taylor, Chris M. Brierley, Mohammad Shamsudduha, and Mark O. Cuthbert
Earth Syst. Dynam., 11, 775–791, https://doi.org/10.5194/esd-11-775-2020, https://doi.org/10.5194/esd-11-775-2020, 2020
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Knowledge of the relationship between climate and groundwater is limited and typically undermined by the scale, duration and accessibility of observations. Using monthly satellite measurements newly compiled over 14 years in the tropics and sub-tropics, we show that the imprint of precipitation history on groundwater, i.e. hydraulic memory, is longer in drylands than humid environments with important implications for the understanding and management of groundwater resources under climate change.
Thomas Mölg, Douglas R. Hardy, Emily Collier, Elena Kropač, Christina Schmid, Nicolas J. Cullen, Georg Kaser, Rainer Prinz, and Michael Winkler
Earth Syst. Dynam., 11, 653–672, https://doi.org/10.5194/esd-11-653-2020, https://doi.org/10.5194/esd-11-653-2020, 2020
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The glaciers on Kilimanjaro summit are like sample spots of the climate in the tropical mid-troposphere. Measurements of air temperature, air humidity, and precipitation with automated weather stations show that the differences in these meteorological elements between two altitudes (~ 5600 and ~ 5900 m) vary significantly over the day and the seasons, in concert with airflow dynamics around the mountain. Knowledge of these variations will improve atmosphere and cryosphere models.
Xinnong Pan, Geli Wang, Peicai Yang, Jun Wang, and Anastasios A. Tsonis
Earth Syst. Dynam., 11, 525–535, https://doi.org/10.5194/esd-11-525-2020, https://doi.org/10.5194/esd-11-525-2020, 2020
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The variations in oceanic and atmospheric modes play important roles in global and regional climate variability. The relationships between their variations and regional climate variability have been extensively examined, but the interconnections among these climate modes remain unclear. We show that the base periods and their harmonic oscillations that appear to be related to QBO, ENSO, and solar activities act as key connections among the climatic modes with synchronous behaviors.
Martin Wegmann, Marco Rohrer, María Santolaria-Otín, and Gerrit Lohmann
Earth Syst. Dynam., 11, 509–524, https://doi.org/10.5194/esd-11-509-2020, https://doi.org/10.5194/esd-11-509-2020, 2020
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Predicting the climate of the upcoming season is of big societal benefit, but finding out which component of the climate system can act as a predictor is difficult. In this study, we focus on Eurasian snow cover as such a component and show that knowing the snow cover in November is very helpful in predicting the state of winter over Europe. However, this mechanism was questioned in the past. Using snow data that go back 150 years into the past, we are now very confident in this relationship.
Hannah S. Davies, J. A. Mattias Green, and Joao C. Duarte
Earth Syst. Dynam., 11, 291–299, https://doi.org/10.5194/esd-11-291-2020, https://doi.org/10.5194/esd-11-291-2020, 2020
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We have confirmed that there is a supertidal cycle associated with the supercontinent cycle. As continents drift due to plate tectonics, oceans also change size, controlling the strength of the tides and causing periods of supertides. In this work, we used a coupled tectonic–tidal model of Earth's future to test four different scenarios that undergo different styles of ocean closure and periods of supertides. This has implications for the Earth system and for other planets with liquid oceans.
Paolo De Luca, Gabriele Messori, Robert L. Wilby, Maurizio Mazzoleni, and Giuliano Di Baldassarre
Earth Syst. Dynam., 11, 251–266, https://doi.org/10.5194/esd-11-251-2020, https://doi.org/10.5194/esd-11-251-2020, 2020
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We show that floods and droughts can co-occur in time across remote regions on the globe and introduce metrics that can help in quantifying concurrent wet and dry hydrological extremes. We then link wet–dry extremes to major modes of climate variability (i.e. ENSO, PDO, and AMO) and provide their spatial patterns. Such concurrent extreme hydrological events may pose risks to regional hydropower production and agricultural yields.
Yang Liu, Jisk Attema, Ben Moat, and Wilco Hazeleger
Earth Syst. Dynam., 11, 77–96, https://doi.org/10.5194/esd-11-77-2020, https://doi.org/10.5194/esd-11-77-2020, 2020
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Poleward meridional energy transport (MET) has significant impact on the climate in the Arctic. In this study, we quantify and intercompare MET at subpolar latitudes from six reanalysis data sets. The results indicate that the spatial distribution and temporal variations of MET differ substantially among the reanalysis data sets. Our study suggests that the MET estimated from reanalyses is useful for the evaluation of energy transports but should be used with great care.
Mia H. Gross, Markus G. Donat, Lisa V. Alexander, and Steven C. Sherwood
Earth Syst. Dynam., 11, 97–111, https://doi.org/10.5194/esd-11-97-2020, https://doi.org/10.5194/esd-11-97-2020, 2020
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This study explores the amplified warming of cold extremes relative to average temperatures for both the recent past and future in the Northern Hemisphere and the possible physical processes that are driving this. We find that decreases in snow cover and
warmer-than-usual winds are driving the disproportionate rates of warming in cold extremes relative to average temperatures. These accelerated warming rates in cold extremes have implications for tourism, insect longevity and human health.
Giorgia Di Capua, Marlene Kretschmer, Reik V. Donner, Bart van den Hurk, Ramesh Vellore, Raghavan Krishnan, and Dim Coumou
Earth Syst. Dynam., 11, 17–34, https://doi.org/10.5194/esd-11-17-2020, https://doi.org/10.5194/esd-11-17-2020, 2020
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Drivers from both the mid-latitudes and the tropical regions have been proposed to influence the Indian summer monsoon (ISM) subseasonal variability. To understand the relative importance of tropical and mid-latitude drivers, we apply recently developed causal discovery techniques to disentangle the causal relationships among these processes. Our results show that there is indeed a two-way interaction between the mid-latitude circulation and ISM rainfall over central India.
Nele Tim, Eduardo Zorita, Kay-Christian Emeis, Franziska U. Schwarzkopf, Arne Biastoch, and Birgit Hünicke
Earth Syst. Dynam., 10, 847–858, https://doi.org/10.5194/esd-10-847-2019, https://doi.org/10.5194/esd-10-847-2019, 2019
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Our study reveals that the latitudinal position and intensity of Southern Hemisphere trades and westerlies are correlated. In the last decades the westerlies have shifted poleward and intensified. Furthermore, the latitudinal shifts and intensity of the trades and westerlies impact the sea surface temperatures around southern Africa and in the South Benguela upwelling region. The future development of wind stress depends on the strength of greenhouse gas forcing.
Ashok Kumar Pokharel and Michael L. Kaplan
Earth Syst. Dynam., 10, 651–666, https://doi.org/10.5194/esd-10-651-2019, https://doi.org/10.5194/esd-10-651-2019, 2019
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This study contributes to a better understanding of how large-scale dust transport can be organized from northwest Africa to the US, Amazon basin, and Europe and might be due in part to Kelvin waves. We also think there is still a need to study major historical dust events that occurred in this region to confirm that this location is suitable and responsible for the generation of the Kelvin waves and the transport of dust on a regular basis.
Christoph Heinze, Veronika Eyring, Pierre Friedlingstein, Colin Jones, Yves Balkanski, William Collins, Thierry Fichefet, Shuang Gao, Alex Hall, Detelina Ivanova, Wolfgang Knorr, Reto Knutti, Alexander Löw, Michael Ponater, Martin G. Schultz, Michael Schulz, Pier Siebesma, Joao Teixeira, George Tselioudis, and Martin Vancoppenolle
Earth Syst. Dynam., 10, 379–452, https://doi.org/10.5194/esd-10-379-2019, https://doi.org/10.5194/esd-10-379-2019, 2019
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Earth system models for producing climate projections under given forcings include additional processes and feedbacks that traditional physical climate models do not consider. We present an overview of climate feedbacks for key Earth system components and discuss the evaluation of these feedbacks. The target group for this article includes generalists with a background in natural sciences and an interest in climate change as well as experts working in interdisciplinary climate research.
Leying Zhang, Haiming Xu, Jing Ma, Ning Shi, and Jiechun Deng
Earth Syst. Dynam., 10, 261–270, https://doi.org/10.5194/esd-10-261-2019, https://doi.org/10.5194/esd-10-261-2019, 2019
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Net heat flux dominates the frontogenesis of the NPSTF from October to December, while oceanic meridional temperature advection contributes equally as much or even more net heat flux in January and February. The atmosphere is critical to frontogenesis through net heat flux and the Aleutian low, the latter of which benefits meridional temperature advection.
Miguel Nogueira
Earth Syst. Dynam., 10, 219–232, https://doi.org/10.5194/esd-10-219-2019, https://doi.org/10.5194/esd-10-219-2019, 2019
Mathias Hauser, Wim Thiery, and Sonia Isabelle Seneviratne
Earth Syst. Dynam., 10, 157–169, https://doi.org/10.5194/esd-10-157-2019, https://doi.org/10.5194/esd-10-157-2019, 2019
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We develop a method to keep the amount of water in the soil at the present-day level, using only local water sources in a global climate model. This leads to less drying over many land areas, but also decreases river runoff. We find that temperature extremes in the 21st century decrease substantially using our method. This provides a new perspective on how land water can influence regional climate and introduces land water management as potential tool for local mitigation of climate change.
Stéphane Vannitsem and Pierre Ekelmans
Earth Syst. Dynam., 9, 1063–1083, https://doi.org/10.5194/esd-9-1063-2018, https://doi.org/10.5194/esd-9-1063-2018, 2018
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The El Niño–Southern Oscillation phenomenon is a slow dynamics present in the coupled ocean–atmosphere tropical Pacific system which has important teleconnections with the northern extratropics. These teleconnections are usually believed to be the source of an enhanced predictability in the northern extratropics at seasonal to decadal timescales. This question is challenged by investigating the causality between these regions using an advanced technique known as convergent cross mapping.
Monica Ionita, Patrick Scholz, Klaus Grosfeld, and Renate Treffeisen
Earth Syst. Dynam., 9, 939–954, https://doi.org/10.5194/esd-9-939-2018, https://doi.org/10.5194/esd-9-939-2018, 2018
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In austral spring 2016 the Antarctic region experienced anomalous sea ice retreat in all sectors, with sea ice extent in October and November 2016 being the lowest in the Southern Hemisphere over the observational record (1979–present). The extreme sea ice retreat was accompanied by the wettest and warmest spring on record, over large areas covering the Indian ocean, the Ross Sea, and the Weddell Sea.
Sergio M. Vicente-Serrano, Raquel Nieto, Luis Gimeno, Cesar Azorin-Molina, Anita Drumond, Ahmed El Kenawy, Fernando Dominguez-Castro, Miquel Tomas-Burguera, and Marina Peña-Gallardo
Earth Syst. Dynam., 9, 915–937, https://doi.org/10.5194/esd-9-915-2018, https://doi.org/10.5194/esd-9-915-2018, 2018
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We analyzed changes in surface relative humidity (RH) at the global scale from 1979 to 2014 and compared the variability and trends in RH with those in land evapotranspiration and ocean evaporation in moisture source areas across a range of selected regions worldwide. Our results stress that the different hypotheses that may explain the decrease in RH under a global warming scenario could act together to explain recent RH trends.
Cited articles
Allaire, S. E., Roulier, S., and Cessna, A. J.: Quantifying preferential flow
in soils: A review of different techniques, J. Hydrol., 378, 179–204,
https://doi.org/10.1016/j.jhydrol.2009.08.013, 2009.
Amundson, R. G. and Davidson, E. A.: Carbon dioxide and nitrogenous gases in
the soil atmosphere, J. Geoche. Explor., 38, 13–41, https://doi.org/10.1016/0375-6742(90)90091-N, 1990.
Auvray, C., Homand, F., and Hoxha, D.: The influence of relative humidity on
the rate of convergence in an underground gypsum mine, Int. J. Rock Mech. Min.
Sci., 45, 1454–1468, https://doi.org/10.1016/j.ijrmms.2008.02.008, 2008.
Bayer, A. D., Lindeskog, M., Pugh, T. A. M., Anthoni, P. M., Fuchs, R., and
Arneth, A.: Uncertainties in the land-use flux resulting from land-use change
reconstructions and gross land transitions, Earth Syst. Dynam., 8, 91–111,
https://doi.org/10.5194/esd-8-91-2017, 2017.
Berthold, S.: Synthetic convection log – characterization of vertical transport
processes in fluid-filled boreholes, J. Appl. Geophys., 72, 20–27,
https://doi.org/10.1016/j.jappgeo.2010.06.007, 2010.
Berthold, S. and Börner, F.: Detection of free vertical convection and
double-diffusion in groundwater monitoring wells with geophysical borehole
measurements, Environ. Geol., 54, 1547–1566, https://doi.org/10.1007/s00254-007-0936-y, 2008.
Berthold, S. and Resagk, C.: Investigation of thermal convection in water columns
using particle image velocimetry, Exp. Fluids, 52, 1465–1474, https://doi.org/10.1007/s00348-012-1267-7, 2012.
Boothroyd, I. M., Almond, S., Qassim, S. M., Worrall, F., and Davies, R. J.:
Fugitive emissions of methane from abandoned, decommissioned oil and gas wells,
Sci. Total Environ., 547, 461–469, https://doi.org/10.1016/j.scitotenv.2015.12.096, 2016.
Bourges, F., Genthon, P., Genty, D., Lorblanchet, M., Mauduit, E. and D'Hulst,
D.: Conservation of prehistoric caves and stability of their inner climate:
Lessons from Chauvet and other French caves, Sci. Total Environ., 493, 79–91,
https://doi.org/10.1016/j.scitotenv.2014.05.137, 2014.
Choi, J.-W. and Smith, J. A.: Geoenvironmental Factors Affecting Organic Vapor
Advection and Diffusion Fluxes from the Unsaturated Zone to the Atmosphere under
Natural Conditions, Environ. Eng. Sci., 22, 95–108, https://doi.org/10.1089/ees.2005.22.95, 2005.
Denis, A., Lastennet, R., Huneau, F., and Malaurent, P.: Identification of
functional relationships between atmospheric pressure and CO2 in the
cave of Lascaux using the concept of entropy of curves, Geophys. Res. Lett.,
32, 1–4, https://doi.org/10.1029/2004GL022226, 2005.
Eckert, E. R. G. and Diaguila, A. J.: Experimental investigation of free-convection
heat transfer in vertical tube at large Grashof numbers, US Government printing office,
Cleveland, Ohio, 1955.
Ellerd, M. G., Massmann, J. W., Schwaegler, D. P., and Rohay, V. J.: Enhancements
for Passive Vapor Extraction: The Hanford Study, Ground Water, 37, 427–437,
https://doi.org/10.1111/j.1745-6584.1999.tb01122.x, 1999.
Eppelbaum, L. V. and Kutasov, I. M.: Estimation of the effect of thermal
convection and casing on the temperature regime of boreholes: a review, J.
Geophys. Eng., 8, R1–R10, https://doi.org/10.1088/1742-2132/8/1/R01, 2011.
Finkelstein, M., Eppelbaum, L. V., and Price, C.: Analysis of temperature
influences on the amplitude-frequency characteristics of Rn gas concentration,
J. Environ. Radioact., 86, 251–270, https://doi.org/10.1016/j.jenvrad.2005.09.004, 2006.
Ganot, Y., Dragila, M. I., and Weisbrod, N.: Impact of thermal convection on
air circulation in a mammalian burrow under arid conditions, J. Arid Environ.,
84, 51–62, https://doi.org/10.1016/j.jaridenv.2012.04.003, 2012.
Ganot, Y., Dragila, M. I., and Weisbrod, N.: Impact of thermal convection on
CO2 flux across the earth–atmosphere boundary in high-permeability
soils, Agr. Forest Meteorol., 184, 12–24, https://doi.org/10.1016/j.agrformet.2013.09.001, 2014.
Goren, O., Burg, A., Gavrieli, I., Negev, I., Guttman, J., Kraitzer, T.,
Kloppmann, W., and Lazar, B.: Biogeochemical processes in infiltration basins
and their impact on the recharging effluent, the soil aquifer treatment (SAT)
system of the Shafdan plant, Israel, Appl. Geochem., 48, 58–69, https://doi.org/10.1016/j.apgeochem.2014.06.017, 2014.
Grossmann, S. and Lohse, D.: Scaling in thermal convection: a unifying theory,
J. Fluid Mech., 407, 27–56, https://doi.org/10.1017/S0022112099007545, 2000.
Guillon, S., Agrinier, P., and Pili, É.: Monitoring CO2 concentration
and δ13C in an underground cavity using a commercial isotope ratio
infrared spectrometer, Appl. Phys. B, 119, 165–175, https://doi.org/10.1007/s00340-015-6013-4, 2015.
Hall, S. J., Learned, J., Ruddell, B., Larson, K. L., Cavender-Bares, J., Bettez,
N., Groffman, P. M., Grove, J. M., Heffernan, J. B., Hobbie, S. E., Morse, J.
L., Neill, C., Nelson, K. C., O'Neil-Dunne, J. P. M., Ogden, L., Pataki, D. E.,
Pearse, W. D., Polsky, C., Chowdhury, R. R., Steele, M. K., and Trammell, T. L.
E.: Convergence of microclimate in residential landscapes across diverse cities
in the United States, Landsc. Ecol., 31, 101–117, https://doi.org/10.1007/s10980-015-0297-y, 2016.
Hillel, D.: Environmental Soil Physics, Academic Press, San Diego, CA,
available at: https://books.google.com.co/books?id=tP__y5xRd0oC (last
access: 10 May 2014), 1998.
James, E. W., Banner, J. L., and Hardt, B.: A global model for cave ventilation
and seasonal bias in speleothem paleoclimate records, Geochem. Geophy. Geosy.,
16, 1044–1051, https://doi.org/10.1002/2014GC005658, 2015.
Kang, M., Kanno, C. M., Reid, M. C., Zhang, X., Mauzerall, D. L., Celia, M. A.,
Chen, Y., and Onstott, T. C.: Direct measurements of methane emissions from
abandoned oil and gas wells in Pennsylvania, P. Natl. Acad. Sci. USA, 111,
18173–18177, https://doi.org/10.1073/pnas.1408315111, 2014.
Kang, M., Baik, E., Miller, A. R., Bandilla, K. W., and Celia, M. A.: Effective
Permeabilities of Abandoned Oil and Gas Wells: Analysis of Data from Pennsylvania,
Environ. Sci. Technol., 49, 4757–4764, https://doi.org/10.1021/acs.est.5b00132, 2015.
Kardashov, V. R., Eppelbaum, L. V., and Vasilyev, O. V.: The role of nonlinear
source terms in geophysics, Geophys. Res. Lett., 27, 2069–2072, https://doi.org/10.1029/1999GL011192, 2000.
Kawamoto, K., Moldrup, P., Schjønning, P., Iversen, B. V., Rolston, D. E.,
and Komatsu, T.: Gas transport parameters in the vadose zone, Vadose Zone J.,
5, 1194–1204, https://doi.org/10.2136/vzj2006.0014, 2006.
Klepikova, M. V., Le Borgne, T., Bour, O., and Davy, P.: A methodology for
using borehole temperature-depth profiles under ambient, single and
cross-borehole pumping conditions to estimate fracture hydraulic properties,
J. Hydrol., 407, 145–152, https://doi.org/10.1016/j.jhydrol.2011.07.018, 2011.
Kowalski, A. S. and Sánchez-Cañete, E. P.: A New Definition of the
Virtual Temperature, Valid for the Atmosphere and the CO2-Rich Air
of the Vadose Zone, J. Appl. Meteorol. Clim., 49, 1692–1695, https://doi.org/10.1175/2010JAMC2534.1, 2010.
Kuang, X., Jiao, J. J., and Li, H.: Review on airflow in unsaturated zones
induced by natural forcings, Water Resour. Res., 49, 6137–6165, https://doi.org/10.1002/wrcr.20416, 2013.
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.
Levintal, E., Dragila, M. I., Kamai, T., and Weisbrod, N.: Free and forced gas
convection in highly permeable, dry porous media, Agr. Forest Meteorol., 232,
469–478, https://doi.org/10.1016/j.agrformet.2016.10.001, 2017.
Massmann, J., Shock, S., and Johannesen, L.: Uncertainties in cleanup times for
soil vapor extraction, Water Resour. Res., 36, 679–692, https://doi.org/10.1029/1999WR900305, 2000.
Moore, J. R., Gischig, V., Katterbach, M., and Loew, S.: Air circulation in
deep fractures and the temperature field of an alpine rock slope, Earth Surf.
Proc. Land., 36, 1985–1996, https://doi.org/10.1002/esp.2217, 2011.
Nachshon, U., Weisbrod, N., and Dragila, M. I.: Quantifying Air Convection
through Surface-Exposed Fractures: A Laboratory Study, Vadose Zone J., 7,
948–956, https://doi.org/10.2136/vzj2007.0165, 2008.
Nativ, R., Adar, E., Assaf, L., and Nygaard, E.: Characterization of the
hydraulic properties of fractures in chalk, Ground Water, 41, 532–543,
https://doi.org/10.1111/j.1745-6584.2003.tb02387.x, 2003.
Neeper, D. A.: Investigation of the vadose zone using barometric pressure cycles,
J. Contam. Hydrol., 54, 59–80, https://doi.org/10.1016/S0169-7722(01)00146-2, 2002.
Neeper, D. A.: Harmonic analysis of flow in open boreholes due to barometric
pressure cycles, J. Contam. Hydrol., 60, 135–162, https://doi.org/10.1016/S0169-7722(02)00086-4, 2003.
Neeper, D. A. and Stauffer, P. H.: Transport by Oscillatory Flow in Soils with
Rate-Limited Mass Transfer: 1. Theory, Vadose Zone J., 11, 2,
https://doi.org/10.2136/vzj2011.0094, 2012.
Noronha, A. L., Hardt, B. F., Banner, J. L., Jenson, J. W., Partin, J. W., James,
E. W., Lander, M. A., and Bautista, K. K.: Trade winds drive pronounced
seasonality in carbonate chemistry in a tropical Western Pacific island
cave-Implications for speleothem paleoclimatology, Geochem. Geophy. Geosy.,
18, 384–399, https://doi.org/10.1002/2016GC006644, 2017.
Perina, T.: General well function for soil vapor extraction, Adv. Water Resour.,
66, 1–7, https://doi.org/10.1016/j.advwatres.2014.01.005, 2014.
Perrier, F. and Le Mouël, J.-L.: Stationary and transient thermal states
of barometric pumping in the access pit of an underground quarry, Sci. Total
Environ., 550, 1044–1056, https://doi.org/10.1016/j.scitotenv.2016.01.125, 2016.
Perrier, F., Morat, P., and Le Mouël, J. L.: Dynamics of air avalanches
in the access pit of an underground quarry, Phys. Rev. Lett., 89, 1–4,
https://doi.org/10.1103/PhysRevLett.89.134501, 2002.
Perrier, F., Le Mouël, J.-L., Kossobokov, V., Crouzeix, C., Morat, P., and
Richon, P.: Properties of turbulent air avalanches in a vertical pit, Eur. Phys.
J. B, 46, 563–579, https://doi.org/10.1140/epjb/e2005-00289-9, 2005.
Pla, C., Cuezva, S., Garcia-Anton, E., Fernandez-Cortes, A., Cañaveras, J.
C., Sanchez-Moral, S., and Benavente, D.: Changes in the CO2 dynamics
in near-surface cavities under a future warming scenario: Factors and evidence
from the field and experimental findings, Sci. Total Environ., 565, 1151–1164,
https://doi.org/10.1016/j.scitotenv.2016.05.160, 2016.
Rayleigh, L.: LIX. On convection currents in a horizontal layer of fluid, when
the higher temperature is on the under side, Philos. Mag. Ser., 32, 529–546,
https://doi.org/10.1080/14786441608635602, 1916.
Rossabi, J. and Falta, R. W.: Analytical Solution for Subsurface Gas Flow to a
Well Induced by Surface Pressure Fluctuations, Ground Water, 40, 67–75,
https://doi.org/10.1111/j.1745-6584.2002.tb02492.x, 2002.
Sánchez-Cañete, E., Serrano-Ortiz, P., Domingo, F., and Kowalski, A.:
Cave ventilation is influenced by variations in the CO2-dependent
virtual temperature, Int. J. Speleol., 42, 1–8, https://doi.org/10.5038/1827-806X.42.1.1, 2013.
Sánchez-Cañete, E. P., Serrano-Ortiz, P., Kowalski, A. S., Oyonarte,
C., and Domingo, F.: Subterranean CO2 ventilation and its role in the
net ecosystem carbon balance of a karstic shrubland, Geophys. Res. Lett., 38,
L09802, https://doi.org/10.1029/2011GL047077, 2011.
Schwarz, J., Bear, J., and Dagan, G.: Groundwater Development in Israel,
Ground Water, 54, 143–148, https://doi.org/10.1111/gwat.12384, 2016.
Serrano-Ortiz, P., Roland, M., Sanchez-Moral, S., Janssens, I. A., Domingo, F.,
Goddéris, Y., and Kowalski, A. S.: Hidden, abiotic CO2 flows and
gaseous reservoirs in the terrestrial carbon cycle: Review and perspectives,
Agr. Forest Meteorol., 150, 321–329, https://doi.org/10.1016/j.agrformet.2010.01.002, 2010.
Shentsis, I., Meirovich, L., Ben-Zvi, A., and Rosenthal, E.: Assessment of
transmission losses and groundwater recharge from runoff events in a wadi under
shortage of data on lateral inflow, Negev, Israel, Hydrol. Process., 13,
1649–1663, https://doi.org/10.1002/(SICI)1099-1085(19990815)13:11<1649::AID-HYP834>3.0.CO;2-N, 1999.
Steinitz, G. and Piatibratova, O.: Radon signals at the Roded site, southern
Israel, Solid Earth, 1, 99–109, https://doi.org/10.5194/se-1-99-2010, 2010.
Thorstenson, D. C., Weeks, E. P., Haas, H., Busenberg, E., Plummer, N., and
Peters, C. A.: Chemistry of unsaturated zone gases sampled in open boreholes
at the crest of Yucca Mountain, Nevada: Data and basic concepts of chemical
and physical processes in the mountain, Water Resour. Res., 34, 1507–1529,
https://doi.org/10.1029/98WR00267, 1998.
Weisbrod, N. and Dragila, M. I.: Potential impact of convective fracture venting
on salt-crust buildup and ground-water salinization in arid environments, J.
Arid Environ., 65, 386–399, https://doi.org/10.1016/j.jaridenv.2005.07.011, 2006.
Weisbrod, N., Dragila, M. I., Nachshon, U., and Pillersdorf, M.: Falling through
the cracks: The role of fractures in Earth-atmosphere gas exchange, Geophys.
Res. Lett., 36, L02401, https://doi.org/10.1029/2008GL036096, 2009.
You, K. and Zhan, H.: Can atmospheric pressure and water table fluctuations be
neglected in soil vapor extraction?, Adv. Water Resour., 35, 41–54,
https://doi.org/10.1016/j.advwatres.2011.10.008, 2012.
You, K., Zhan, H., and Li, J.: A new solution and data analysis for gas flow to
a barometric pumping well, Adv. Water Resour., 33, 1444–1455, https://doi.org/10.1016/j.advwatres.2010.07.008, 2010.
You, K., Zhan, H., and Li, J.: Gas flow to a barometric pumping well in a
multilayer unsaturated zone, Water Resour. Res., 47, W05522, https://doi.org/10.1029/2010WR009411, 2011.
Zeng, Y., Xie, Z., and Liu, S.: Seasonal effects of irrigation on land–atmosphere
latent heat, sensible heat, and carbon fluxes in semiarid basin, Earth Syst.
Dynam., 8, 113–127, https://doi.org/10.5194/esd-8-113-2017, 2017.
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