Bibliografías temáticas / Groundwater-Atmosphere processes

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Literatura académica sobre el tema "Groundwater-Atmosphere processes"

Autor: Grafiati

Publicado: 9 de noviembre de 2024

Última modificación: 31 de julio de 2025

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Artículos de revistas sobre el tema "Groundwater-Atmosphere processes"

Maxwell, Reed M., Julie K. Lundquist, Jeffrey D. Mirocha, Steven G. Smith, Carol S. Woodward, and Andrew F. B. Tompson. "Development of a Coupled Groundwater–Atmosphere Model." Monthly Weather Review 139, no. 1 (2011): 96–116. http://dx.doi.org/10.1175/2010mwr3392.1.

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Abstract Complete models of the hydrologic cycle have gained recent attention as research has shown interdependence between the coupled land and energy balance of the subsurface, land surface, and lower atmosphere. PF.WRF is a new model that is a combination of the Weather Research and Forecasting (WRF) atmospheric model and a parallel hydrology model (ParFlow) that fully integrates three-dimensional, variably saturated subsurface flow with overland flow. These models are coupled in an explicit, operator-splitting manner via the Noah land surface model (LSM). Here, the coupled model formulatio

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Decharme, Bertrand, and Jeanne Colin. "Influence of floodplains and groundwater dynamics on the present-day climate simulated by the CNRM climate model." Earth System Dynamics 16, no. 3 (2025): 729–52. https://doi.org/10.5194/esd-16-729-2025.

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Abstract. The climate impacts of floodwater stored over large inundated areas and groundwater stored in large unconfined aquifers at the global scale are not yet well documented, despite their potential to affect the atmosphere through contributions to land surface evapotranspiration fluxes. To address these gaps in knowledge, the present study aims to assess the potential role of these processes in present-day climate using the CNRM-CM6-1 global climate model, the physical core of the Earth system model (ESM) used by the French National Center for Meteorological Research (CNRM) for climate pr

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FOX, R. J., T. R. FISHER, A. B. GUSTAFSON, T. E. JORDAN, T. M. KANA, and M. W. LANG. "Searching for the missing nitrogen: biogenic nitrogen gases in groundwater and streams." Journal of Agricultural Science 152, S1 (2014): 96–106. http://dx.doi.org/10.1017/s0021859614000070.

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SUMMARYBiogenic nitrogen (N2) and nitrous oxide (N2O) accumulations were measured in groundwater, streams and the vadose zone of small agricultural watersheds in the Mid-Atlantic USA. In general, N2and N2O in excess of atmospheric equilibrium were found in groundwater virtually everywhere that was sampled. Excess N2in groundwater ranged from undetectable to 616 μmol N2-N/l, the latter representingc. 50% of background N2. The N2O-N concentrations varied from undetectable to 75 μm, and usually greatly exceeded values at atmospheric equilibrium (25–30 nM); however, N2O was generally 1–10% of exce

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Sulis, Mauro, John L. Williams, Prabhakar Shrestha, et al. "Coupling Groundwater, Vegetation, and Atmospheric Processes: A Comparison of Two Integrated Models." Journal of Hydrometeorology 18, no. 5 (2017): 1489–511. http://dx.doi.org/10.1175/jhm-d-16-0159.1.

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Abstract This study compares two modeling platforms, ParFlow.WRF (PF.WRF) and the Terrestrial Systems Modeling Platform (TerrSysMP), with a common 3D integrated surface–groundwater model to examine the variability in simulated soil–vegetation–atmosphere interactions. Idealized and hindcast simulations over the North Rhine–Westphalia region in western Germany for clear-sky conditions and strong convective precipitation using both modeling platforms are presented. Idealized simulations highlight the strong variability introduced by the difference in land surface parameterizations (e.g., ground e

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Coxon, Catherine E. "Carbonate Deposition in Turloughs (Seasonal Lakes) on the Western Limestone Lowlands of Ireland - I: Present Day Processes." Irish Geography 27, no. 1 (2015): 14–27. http://dx.doi.org/10.55650/igj.1994.428.

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This paper describes an investigation of carbonate deposition in seasonal groundwater-fed lakes (turloughs) situated on the limestone lowland of south-east county Mayo. Chemical data from four turloughs suggest that present-day calcite deposition is due predominantly to supersaturation caused by the loss of excess carbon dioxide from the water to the atmosphere. This process occurs throughout the winter. Biological influences appear to play only a minor role, although investigations of turlough trophic status and algal biomass are required to confirm this.

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Richard, A., S. Galle, M. Descloitres, et al. "Riparian forest and permanent groundwater: a key coupling for balancing the hillslope water budget in Sudanian West Africa." Hydrology and Earth System Sciences Discussions 10, no. 5 (2013): 5643–86. http://dx.doi.org/10.5194/hessd-10-5643-2013.

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Abstract. Forests are thought to play an important role in the regional dynamics of the West African monsoon, through their capacity to extract water from permanent aquifers located deep in the soil and pump it into the atmosphere even during the dry season. This is especially true for riparian forests located at the bottom of the hillslopes. This coupling between the riparian forests and the permanent aquifers is investigated, looking for quantifying its contribution to the catchment water balance. To this end, use is made of the observations available from a comprehensively instrumented hill

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Pavlov, S. Kh. "PROCESSES OF FORMATION OF SODIUM BICARBONATE GROUNDWATER IN THE RAINWATER – SANDSTONE SYSTEM." Geodynamics & Tectonophysics 14, no. 6 (2023): 0733. http://dx.doi.org/10.5800/gt-2023-14-6-0733.

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In modeling, a study was made of the processes of the physical-chemical interaction between rainwater and sandstone. It was stated that as a result of the interaction, already in mineralization of water equal to 55 mg/l, there emerges a pure soda solution whose sharp oxidation properties, retaining up to 200 mg/l, change to sharp restorative when exceeding this value. At the mineralization of water equal to 30 mg/l, an intensive increase in the number of hydroxide ions in a solution makes it highly alkaline. The active removal of calcium from solution is due to the formation of not only solid

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Al-Najjar, Hassan, Gokmen Ceribasi, Emrah Dogan, Khalid Qahman, Mazen Abualtayef, and Ahmet Iyad Ceyhunlu. "Statistical modeling of spatial and temporal vulnerability of groundwater level in the Gaza Strip (Palestine)." H2Open Journal 4, no. 1 (2021): 352–65. http://dx.doi.org/10.2166/h2oj.2021.120.

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Abstract The water supply in the Gaza Strip substantially depends on the groundwater resource of the Gaza coastal aquifer. The climate changes and the over-exploiting processes negatively impact the recovery of the groundwater balance. The climate variability is characterized by the decline in the precipitation of −5.2% and an increase in temperature of +1 °C in the timeframe of 2020–2040. The potential evaporation and the sunshine period are expected to increase by about 111 mm and 5 hours, respectively, during the next 20 years. However, the atmosphere is predicted to be drier where the rela

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Barenbaum, Azariy A. "On the relationship of oil and gas formation and degassing processes with groundwater decomposition." Georesursy 20, no. 4 (2018): 290–300. http://dx.doi.org/10.18599/grs.2018.4.290-300.

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The article is referred to important consequence of the biosphere oil and gas formation concept, according to which the process of hydrocarbons generation in the subsoil and degassing of the Earth are a single natural phenomenon. The main role in this phenomenon is played by geochemical circulation of carbon and water through the Earth’s surface accompanied by polycondensation synthesis of hydrocarbons by CO2+H2O reaction. This reaction is accompanied by a colossal decomposition of groundwater into hydrogen and oxygen within the sedimentary cover of the earth’s crust. Unreacted CO2, as well as

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Martínez-de la Torre, Alberto, and Gonzalo Miguez-Macho. "Groundwater influence on soil moisture memory and land–atmosphere fluxes in the Iberian Peninsula." Hydrology and Earth System Sciences 23, no. 12 (2019): 4909–32. http://dx.doi.org/10.5194/hess-23-4909-2019.

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Abstract. Groundwater plays an important role in the terrestrial water cycle, interacting with the land surface via vertical fluxes through the water table and distributing water resources spatially via gravity-driven lateral transport. It is therefore essential to have a correct representation of groundwater processes in land surface models, as land–atmosphere coupling is a key factor in climate research. Here we use the LEAFHYDRO land surface and groundwater model to study the groundwater influence on soil moisture distribution and memory, and evapotranspiration (ET) fluxes in the Iberian Pe

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Tesis sobre el tema "Groundwater-Atmosphere processes"

Jomaa, Fatima. "Précipitations sur le sud de la France : caractérisation, source et impacts sur le cycle hydrologique régional." Electronic Thesis or Diss., Université Grenoble Alpes, 2024. http://www.theses.fr/2024GRALU025.

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La région méditerranéenne se distingue comme un « point chaud » potentiel en matière de science du climat, ce qui signifie une région où les impacts du changement climatique devraient être particulièrement importants. Dans la région méditerranéenne, il existe une interaction complexe entre l’atmosphère océanique et la terre ferme, associée à des caractéristiques morphologiques distinctes. Ce couplage fort fait référence aux interactions entre la mer Méditerranée, l’atmosphère et les terres environnantes, influençant des dynamiques climatiques locales spécifiques. Dans cette thèse, nous nous so

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Grassa, F. "Geochemical processes governing the chemistry of groundwater hosted within the Hyblean aquifers." Thesis, 2002. http://hdl.handle.net/2122/416.

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A raingauge network made of six stations was installed in the Hyblean region. Stations were located at different altitudes (from 5 m to 986 m a.s.l.) and along two directions (E-W and SW-NE). Rainwater samples were monthly collected for stable isotope measurements. Spatial distribution of rainwater isotope composition has confirmed the wet air masses move from South-East/South-West toward North. Water balance has highlighted that the annual volume of infiltrating waters is in the range of 1-1.5 *105 m3 Km-2. 82 well waters and 12 spring waters located within the Hyblean Plateau (South-Ester

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Son, Eun Kyeu. "Characterization of bacterial processes in the subsurface and the atmosphere." 2009. http://hdl.rutgers.edu/1782.2/rucore10001600001.ETD.000051910.

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Capítulos de libros sobre el tema "Groundwater-Atmosphere processes"

Zhao, Ying, Ji Qi, Qiuli Hu, and Yi Wang. "The “Groundwater Benefit Zone”, Proposals, Contributions and New Scientific Issues." In Soil Science - Emerging Technologies, Global Perspectives and Applications [Working Title]. IntechOpen, 2021. http://dx.doi.org/10.5772/intechopen.100299.

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The groundwater has great potential for water resource utilization, accounting for about a quarter of vegetation transpiration globally and contributing up to 84% in shallow groundwater areas. However, in irrigated agricultural regions or coastal areas with shallow groundwater levels, due to the high groundwater salinity, the contribution of groundwater to transpiration is small and even harmful. This paper proposes a new conception of groundwater benefit zone in the groundwater-soil–plant-atmosphere continuum (GSPAC) system. Firstly, it analyzes the mutual feedback processes of the undergroun

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Perdrial, Julia, Aaron Thompson, and Jon Chorover. "Soil Geochemistry in the Critical Zone: Influence on Atmosphere, Surface- and Groundwater Composition." In Developments in Earth Surface Processes. Elsevier, 2015. http://dx.doi.org/10.1016/b978-0-444-63369-9.00006-9.

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Verweij, Hanneke, Gualbert Oude Essink, Niels Hartog, and Willem Jan Zaadnoordijk. "Hydrogeology." In Geology of the Netherlands. Amsterdam University Press, 2025. https://doi.org/10.5117/9789463728362_ch17.

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Abstract Groundwater is a crucial source of fresh water for domestic, agricultural and industrial uses, and for maintaining aquatic- and groundwater-dependent ecosystems. It is also of importance for identifying and securing sustainable use of energy resources and subsurface storage sites. Groundwater interacts with different parts of system earth, including the atmosphere, surface water, soil, geological environment and with many geological processes. This chapter provides an overview of groundwater systems in the Netherlands and the Dutch continental shelf at depths from the surface down to

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Hose*, Louise D., Harvey R. DuChene*, Daniel Jones, et al. "Hypogenic karst of the Great Basin." In Field Excursions from the 2021 GSA Section Meetings. Geological Society of America, 2021. http://dx.doi.org/10.1130/2020.0061(05).

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ABSTRACT Discoveries in the 1980s greatly expanded speleologists’ understanding of the role that hypogenic groundwater flow can play in developing caves at depth. Ascending groundwater charged with carbon dioxide and, especially, hydrogen sulfide can readily dissolve carbonate bedrock just below and above the water table. Sulfuric acid speleogenesis, in which anoxic, rising, sulfidic groundwater mixes with oxygenated cave atmosphere to form aggressive sulfuric acid (H2SO4) formed spectacular caves in Carlsbad Caverns National Park, USA. Cueva de Villa Luz in Mexico provides an aggressively act

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Gunasekaran, Madhan, Subhamay Banerjee, Hitha S, Arunima S, Ruchi Prakash, and Suman Kashyap. "WATER SUSTAINABILITY." In Futuristic Trends in Renewable & Sustainable Energy Volume 3 Book 2. Iterative International Publishers, Selfypage Developers Pvt Ltd, 2024. http://dx.doi.org/10.58532/v3bars2p2ch8.

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Water is our largest natural resource, but only 3% is freshwater and only one- third of it is available for agriculture and drinking purposes. The freshwater we use comes from two sources: Surface water runoff and groundwater. Precipitation that flows into water bodies such as streams, rivers, and lakes at the surface of the earth without infiltrating the surface or returning to the atmosphere by evaporation or transpiration is called surface water runoff [1]. Some of the precipitation percolates to the surface, where it collects as soil water, partially filling the pores between surface soil

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Sposito, Garrison. "Colloidal Phenomena." In The Surface Chemistry of Natural Particles. Oxford University PressNew York, NY, 2004. http://dx.doi.org/10.1093/oso/9780195117806.003.0005.

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Abstract The natural particles whose surface reactions figure most importantly in the geochemistry of soils and sediments range in size from approximately 10 nm to 10 µ,m—from fine clay to fine silt—while comprising a heterogeneous mixture of crystalline minerals, amorphous weathering residues, humus, and microbial biomass. The size range just given, which can be broadened in certain circumstances by as much as an order of magnitude from either endpoint, encompasses typical groundwater colloids and viruses in its lower portion, with riverine suspended solids and phytoplankton included in its u

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Hopmans, Jan W., and Jan M. H. Hendrickx. "Emerging Measurement Techniques for Vadose Zone Characterization." In Vadose Zone Hydrology. Oxford University Press, 1999. http://dx.doi.org/10.1093/oso/9780195109900.003.0015.

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Variables and parameters required to characterize soil water flow and solute transport are often measured at different spatial scales from those for which they are needed. This poses a problem since results from field and laboratory measurements at one spatial scale are not necessarily valid for application at another. Herein lies a challenge that vadose zone hydrologists are faced with. For example, vadose zone studies can include flow at the groundwater-unsaturated zone as well as at the soil surface-atmosphere interface at either one specific location or representing an entire field or land

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Sposito, Garrison. "The Composition of Soils." In The Chemistry of Soils. Oxford University Press, 2016. http://dx.doi.org/10.1093/oso/9780190630881.003.0005.

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Soils are porous media created at the land surface through weathering processes mediated by biological, geological, and hydrological phenomena. From the point of view of chemistry, soils are open biogeochemical systems containing reactive solids, liquids, and gases. That they are open systems means they exchange both matter and energy with the surrounding atmosphere, biosphere, and hydrosphere. That they are biogeochemical systems means their development over time is a result of chemical transformations of earth materials linked to the life cycles of the soil biota and plant roots. Soils are t

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Gage, Stuart H. "Climate Variability in the North Central Region: Characterizing Drought Severity Patterns." In Climate Variability and Ecosystem Response in Long-Term Ecological Research Sites. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195150599.003.0010.

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This chapter examines the spatial and temporal variability and patterns of climate for the period 1972–1991 in the North Central Region of North America (NCR). Since the mid-1970s, climate has become more variable in the region, compared to the more benign period 1950–1970. The regional perspective presented in this chapter characterizes the general climatology of the NCR from 1972 to 1991 and compares the climate to a severe drought that occurred in 1988. This one-year drought was one of the most substantial in the region’s recent history, and it had a significant impact on the region’s agric

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Bethke, Craig M. "Evaporation." In Geochemical Reaction Modeling. Oxford University Press, 1996. http://dx.doi.org/10.1093/oso/9780195094756.003.0022.

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The process of evaporation, including transpiration (evaporation from plants), returns to the atmosphere more than half of the water reaching the Earth’s land surface; thus, it plays an important role in controlling the chemistry of surface water and groundwater, especially in relatively arid climates. Geochemists study the evaporation process to understand the evolution of water in desert playas and lakes as well as the origins of evaporite deposits. They also investigate environmental aspects of evaporation (e.g., Appelo and Postma, 1993), such as its effects on the chemistry of rainfall and

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Actas de conferencias sobre el tema "Groundwater-Atmosphere processes"

Bublias, V. M., and O. L. Shevchenko. "Monitoring of Geophysical Fields and Natural Phenomena in the Atmosphere and Lithosphere for the Study of Groundwater Recharge Mechanisms." In 17th International Conference Monitoring of Geological Processes and Ecological Condition of the Environment. European Association of Geoscientists & Engineers, 2023. http://dx.doi.org/10.3997/2214-4609.2023520184.

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