Relevant bibliographies by topics / Atmospheric Energy Fluxes

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Atmospheric Energy Fluxes'

Author: Grafiati
Published: 22 June 2021
Last updated: 29 July 2025

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Journal articles on the topic "Atmospheric Energy Fluxes"

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Sun, Jielun. "Incorporating the Work Done by Vertical Density Fluxes in Both Kinetic and Thermal Energy Conservation Equations to Satisfy Total Energy Conservation." Journal of Applied Meteorology and Climatology 58, no. 2 (2019): 213–30. http://dx.doi.org/10.1175/jamc-d-17-0350.1.

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AbstractConservation of total, kinetic, and thermal energy in the atmosphere is revisited, and the derived thermal energy balance is examined with observations. Total energy conservation (TEC) provides a constraint for the sum of kinetic, thermal, and potential energy changes. In response to air thermal expansion/compression, air density variation leads to vertical density fluxes and potential energy changes, which in turn impact the thermal energy balance as well as the kinetic energy balance due to the constraint of TEC. As vertical density fluxes can propagate through a large vertical domai
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Chilingarian, Ashot. "Thunderstorm Ground Enhancements Measured on Aragats and Progress of High-Energy Physics in the Atmosphere." Atmosphere 14, no. 2 (2023): 300. http://dx.doi.org/10.3390/atmos14020300.

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High-energy physics in the atmosphere (HEPA) has undergone an intense reformation in the last decade. Correlated measurements of particle fluxes modulated by strong atmospheric electric fields, simultaneous measurements of the disturbances of the near-surface electric fields and lightning location, and registration of various meteorological parameters on the Earth have led to a better understanding of the complex processes in the terrestrial atmosphere. The cooperation of cosmic rays and atmospheric physics has led to the development of models for the origin of particle bursts recorded on the
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Bannon, Peter R. "Atmospheric Available Energy." Journal of the Atmospheric Sciences 69, no. 12 (2012): 3745–62. http://dx.doi.org/10.1175/jas-d-12-059.1.

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Abstract The total potential energy of the atmosphere is the sum of its internal and gravitational energies. The portion of this total energy available to be converted into kinetic energy is determined relative to an isothermal, hydrostatic, equilibrium atmosphere that is convectively and dynamically “dead.” The temperature of this equilibrium state is determined by minimization of a generalized Gibbs function defined between the atmosphere and its equilibrium. Thus, this function represents the maximum amount of total energy that can be converted into kinetic energy and, hence, the available
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Shaffrey, Len, and Rowan Sutton. "Bjerknes Compensation and the Decadal Variability of the Energy Transports in a Coupled Climate Model." Journal of Climate 19, no. 7 (2006): 1167–81. http://dx.doi.org/10.1175/jcli3652.1.

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Abstract In the 1960s, Jacob Bjerknes suggested that if the top-of-the-atmosphere (TOA) fluxes and the oceanic heat storage did not vary too much, then the total energy transport by the climate system would not vary too much either. This implies that any large anomalies of oceanic and atmospheric energy transport should be equal and opposite. This simple scenario has become known as Bjerknes compensation. A long control run of the Third Hadley Centre Coupled Ocean–Atmosphere General Circulation Model (HadCM3) has been investigated. It was found that northern extratropical decadal anomalies of
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Gilchrist-Millar, Caitlin A., David B. Jess, Samuel D. T. Grant, et al. "Magnetoacoustic wave energy dissipation in the atmosphere of solar pores." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 379, no. 2190 (2020): 20200172. http://dx.doi.org/10.1098/rsta.2020.0172.

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The suitability of solar pores as magnetic wave guides has been a key topic of discussion in recent years. Here, we present observational evidence of propagating magnetohydrodynamic wave activity in a group of five photospheric solar pores. Employing data obtained by the Facility Infrared Spectropolarimeter at the Dunn Solar Telescope, oscillations with periods of the order of 5 min were detected at varying atmospheric heights by examining Si ɪ 10827 Å line bisector velocities. Spectropolarimetric inversions, coupled with the spatially resolved root mean square bisector velocities, allowed the
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Barr, Giles. "Atmospheric Neutrino Fluxes." Nuclear Physics B - Proceedings Supplements 143 (June 2005): 89–95. http://dx.doi.org/10.1016/j.nuclphysbps.2005.01.092.

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Gaisser, Thomas K. "Atmospheric neutrino fluxes." Nuclear Physics B - Proceedings Supplements 118 (April 2003): 109–17. http://dx.doi.org/10.1016/s0920-5632(03)01309-4.

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Donohoe, Aaron, and David S. Battisti. "The Seasonal Cycle of Atmospheric Heating and Temperature." Journal of Climate 26, no. 14 (2013): 4962–80. http://dx.doi.org/10.1175/jcli-d-12-00713.1.

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Abstract The seasonal cycle of the heating of the atmosphere is divided into a component due to direct solar absorption in the atmosphere and a component due to the flux of energy from the surface to the atmosphere via latent, sensible, and radiative heat fluxes. Both observations and coupled climate models are analyzed. The vast majority of the seasonal heating of the northern extratropics (78% in the observations and 67% in the model average) is due to atmospheric shortwave absorption. In the southern extratropics, the seasonal heating of the atmosphere is entirely due to atmospheric shortwa
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Mayer, Michael, Leopold Haimberger, John M. Edwards, and Patrick Hyder. "Toward Consistent Diagnostics of the Coupled Atmosphere and Ocean Energy Budgets." Journal of Climate 30, no. 22 (2017): 9225–46. http://dx.doi.org/10.1175/jcli-d-17-0137.1.

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The widely used diagnostic vertically integrated total energy budget equations of atmosphere and ocean contain inconsistencies that should no longer be disregarded. The neglect of enthalpy fluxes associated with precipitation and evaporation leads to a spurious dependence on reference temperature. This seemingly small inconsistency is amplified because enthalpy of water vapor implicitly included in lateral atmospheric energy transports usually is computed on the Kelvin scale, leading to inconsistencies that, although zero when globally averaged, attain values on the order of 20 W m−2 in the tr
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Liu, Chunlei, Ni Chen, Jingchao Long, et al. "Review of the Observed Energy Flow in the Earth System." Atmosphere 13, no. 10 (2022): 1738. http://dx.doi.org/10.3390/atmos13101738.

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The energy budget imbalance at the top of the atmosphere (TOA) and the energy flow in the Earth’s system plays an essential role in climate change over the global and regional scales. Under the constraint of observations, the radiative fluxes at TOA have been reconstructed prior to CERES (Clouds and the Earth’s Radiant Energy System) between 1985 and 2000. The total atmospheric energy divergence has been mass corrected based on ERA5 (the fifth generation ECMWF ReAnalysis) atmospheric reanalysis by a newly developed method considering the enthalpy removing of the atmospheric water vapor, which
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Dissertations / Theses on the topic "Atmospheric Energy Fluxes"

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Ramstrom, William D. (William Douglas). "Tropical cyclone momentum and energy fluxes." Thesis, Massachusetts Institute of Technology, 2001. http://hdl.handle.net/1721.1/59095.

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Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2001.<br>Includes bibliographical references (leaves 82-84).<br>Many modeling studies of tropical cyclones use the bulk aerodynamic formulae to determine angular momentum and enthalpy fluxes at the sea surface. These results show that the intensification of a hurricane is very sensitive to the values of the coefficients defined in these formulae (Emanuel, 1995). Using these formulae allows the model to make bulk estimates of these fluxes as a function of wind speed, without having to cons
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GISOLO, DAVIDE. "Water, carbon and energy fluxes on grasslands of Western Alps: methodological issues, experimental data, hydrological modelling and atmospheric boundary layer phenomena." Doctoral thesis, Politecnico di Torino, 2021. http://hdl.handle.net/11583/2957761.

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Zhang, Jun. "An Airborne Investigation of the Atmospheric Boundary Layer Structure in the Hurricane Force Wind Regime." Scholarly Repository, 2007. http://scholarlyrepository.miami.edu/oa_dissertations/15.

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As part of the ONR sponsored Coupled Boundary Layer/Air-Sea Transfer (CBLAST) experiment, data from the NOAA WP-3D research aircraft measurements into major Hurricanes in the 2002-2004 seasons are analyzed to investigate the structure of the boundary layer. The turbulent fluxes of momentum and enthalpy are derived using the eddy correlation method. For the first time, the momentum and enthalpy fluxes were directly measured in the boundary layer of a hurricane with wind speeds up to 30 m/s. A new bulk parameterization of the momentum and enthalpy flux is developed. The vertical structure of t
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Burnett, Benjamin F. "Exploratory Eddy Covariance Measurements of Surface Heat and CO2 Fluxes in the Roughness Sublayer of an Urban Environment." PDXScholar, 2010. https://pdxscholar.library.pdx.edu/open_access_etds/401.

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In this study eddy covariance was used to measure sensible heat, latent heat, and carbon dioxide fluxes for the months of August, September, and October of 2009 within the roughness sublayer (RSL) of the urban center of Portland, OR. Vehicle traffic and solar radiation were also measured for the month of October. Flux measurements were compared with measurements from other urban areas as a test of reasonableness. CO₂ fluxes were nearly always positive and were strongly correlated with the weekday diurnal traffic cycle. CO₂ fluxes averaged 6.6 μmol/m^²s, which is less than other published measu
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Arsego, Diogo Alessandro. "FLUXOS DE CALOR E TRANSFERÊNCIA DE ENERGIA CALORÍFICA ENTRE O OCEANO E A ATMOSFERA SOBRE ESTRUTURAS OCEÂNICAS DE MESOESCALA NO ATLÂNTICO SUL." Universidade Federal de Santa Maria, 2012. http://repositorio.ufsm.br/handle/1/10263.

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Understanding the interactions between ocean and atmosphere in regions of oceanographic fronts is of vital importance for the improvement of numerical models for weather and climate forecasting. In the South Atlantic Ocean (SAO) the meeting between the warm waters of the Brazil Current (BC) and the cold waters of the Malvinas (Falkland) Current (MC) in the region known as the Brazil-Malvinas Confluence (BMC), results in intense mesoscale oceanic activity and, for this reason, this region is considered one of the most energetic of the Global Ocean. The interactions resulting from the thermal co
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Lytle, William. "Coupled Evaluation of Below- and Above-Ground Energy and Water Cycle Variables from Reanalysis Products Over Five Flux Tower Sites in the U.S." Thesis, The University of Arizona, 2015. http://hdl.handle.net/10150/595636.

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Reanalysis products are widely used to study the land-atmosphere exchanges of energy, water, and carbon fluxes, and have been evaluated using in situ data above or below ground. Here measurements for several years at five flux tower sites in the U.S. (with a total of 315,576 hours of data) are used for the coupled evaluation of both below- and above-ground processes from three global reanalysis products and six global land data assimilation products. All products show systematic errors in precipitation, snow depth, and the timing of the melting and onset of snow. Despite the biases in soil mo
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Fan, Yalin. "Effects of surface waves on air-sea momentum and energy fluxes and ocean response to hurricanes /." View online ; access limited to URI, 2007. http://0-digitalcommons.uri.edu.helin.uri.edu/dissertations/AAI3276981.

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Ayet, Alex. "Flux de quantité de mouvement à l'interface air-mer : approche théorique du couplage entre turbulence et vagues de vent On the Impact of Long Wind-Waves on Near-Surface Turbulence and Momentum Fluxes, in Boundary-Layer Meteorology volume 174, March 2020 Scalewise return to isotropy in stratified boundary layer flows, in JGR Atmospheres 125 (16), August 2020 Scaling laws for the length scale of energy‐containing eddies in a sheared and thermally stratified atmospheric surface layer, in Geophysical Research Letters 47(23), December 2020." Thesis, Brest, 2020. http://www.theses.fr/2020BRES0038.

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Malgré de nombreuses études, le lien de causalité entre vent et vagues fait toujours l’objet de controverses : cela est dû entre autres au caractère multi-échelle d'une surface océanique réaliste, et à la présence de déferlements, qui modifient radicalement sa topologie. Dans cette thèse, ces deux questions sont abordées sous un angle théorique, à travers un modèle phénoménologique, qui relie les propriétés spectrales et moyennées de la turbulence proche de paroi en utilisant la géométrie de tourbillons attachés à celle-ci. La première partie de la thèse revisite ce modèle phénoménologique en
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Gavrilovic, Nikola. "Endurance improvement of mini UAVs through energy harvesting from atmospheric gusts." Thesis, Toulouse, ISAE, 2018. http://www.theses.fr/2018ESAE0024/document.

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Cette thèse a pour but de découvrir la faisabilité et le potentiel de la récupération d'énergie à partir de rafales atmosphériques pour les micro et mini véhicules aériens sans pilote. L'atmosphère sert de grande source d'énergie pouvant être récoltée afin d'accroître la performance des petits UAV sous la forme d'une autonomie et d'une autonomie étendues. Il est bien connu que de nombreuses espèces d'oiseaux utilisent diverses techniques de vol pour obtenir des performances de vol étonnantes. Compte tenu du fait que les véhicules susmentionnés partagent la taille et la vitesse de vol avec des
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Vogel, Christoph Alexander. "An investigation of the role of flux divergence in the turbulent kinetic energy balance of the atmospheric surface layer." Diss., Georgia Institute of Technology, 1992. http://hdl.handle.net/1853/25789.

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Books on the topic "Atmospheric Energy Fluxes"

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Burkhardt, Thomas. Subgrid-scale vertical energy fluxes over the African-Atlantic region. Dümmler, 1990.

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J, Dobosy Ronald, Birdwell Kevin R, and Air Resources Laboratory (U.S.), eds. Airborne measurements of mass, momentum, and energy fluxes for the Boardman-Arm Regional Flux Experiment--1991 preliminary data release. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Air Resources Laboratory, 1993.

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Jet Propulsion Laboratory (U.S.) and Nova University, eds. Air-sea interaction with SSM/I and altimeter: Report of the NASA Ocean Energy Fluxes Science Working Group. Jet Propulsion Laboratory, California Institute of Technology, 1985.

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Jet Propulsion Laboratory (U.S.) and Nova University, eds. Air-sea interaction with SSM/I and altimeter: Report of the NASA Ocean Energy Fluxes Science Working Group. Jet Propulsion Laboratory, California Institute of Technology, 1985.

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Siegrist, Franziska C. Determination of energy and trace gas fluxes on a regional scale: Combination of local surface flux measurements and vertical flux profiles throughout the atmospheric boundary layer in complex terrain (Swiss Seeland Region). Institute of Geographiy, 2001.

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International Conference Soils and the Greenhouse Effect (1989 Wageningen, Netherlands). Soils and the greenhouse effect: The present status and future trends concerning the effect of soils and their cover on the fluxes of greenhouse gases, the surface energy balance, and the water balance : proceedings of the International Conference Soils and the Greenhouse Effect. Wiley, 1990.

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Sivaramakrishnan, S., of Indian Institute of Tropical Meteorology. and Indian Institute of Tropical Meteorology., eds. Measurement of profiles and surface energy fluxes on the west coast of India at Vasco-Da-Gama, Goa during ARMEX 2002-03. Indian Institute of Tropical Meteorology, 2003.

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United States. National Aeronautics and Space Administration., ed. Global Ultraviolet Imager (GUVI) Investigation: Period of performance, 08 Nov 1993 through 07 Dec 1994 : GUVI final report : final report : NASA contract no. NAS5-32572. National Aeronautics and Space Administration, 1995.

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United States. National Aeronautics and Space Administration., ed. Global ultraviolet imager (GUVI) investigation: Period of performance, 08 Nov 1993 through 07 Dec 1994 : GUVI final report. National Aeronautics and Space Administration, 1995.

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F, Young David, Racel Anne M, and United States. National Aeronautics and Space Administration., eds. The CERES S'COOL project: Development and operational phases. National Aeronautics and Space Administration, 1998.

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Book chapters on the topic "Atmospheric Energy Fluxes"

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Honda, Morihiro. "Calculation of Low-Energy Atmospheric Neutrino Fluxes." In Physics and Astrophysics of Neutrinos. Springer Japan, 1994. http://dx.doi.org/10.1007/978-4-431-67029-2_8.

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Hatfield, Jerry L., and John H. Prueger. "Variable Atmospheric, Canopy, and Soil Effects on Energy and Carbon Fluxes over Crops." In Improving Modeling Tools to Assess Climate Change Effects on Crop Response. American Society of Agronomy and Soil Science Society of America, 2016. http://dx.doi.org/10.2134/advagricsystmodel7.2014.0018.

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Oswald, Claire J., Wayne R. Rouse, and Jacqueline Binyamin. "Modeling Lake Energy Fluxes in the Mackenzie River Basin using Bulk Aerodynamic Mass Transfer Theory." In Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience. Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-75136-6_9.

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Vanzandt, Thomas E., and David C. Fritts. "Spectral Estimates of Gravity Wave Energy and Momentum Fluxes." In Coupling Processes in the Lower and Middle Atmosphere. Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-1594-0_18.

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Dolman, A. J., E. J. Moors, T. Grunwald, P. Berbigier, and C. Bernhofer. "Factors Controlling Forest Atmosphere Exchange of Water, Energy, and Carbon." In Fluxes of Carbon, Water and Energy of European Forests. Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05171-9_10.

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Barker, H. W., S. Kato, and T. Wehr. "Computation of Solar Radiative Fluxes by 1D and 3D Methods Using Cloudy Atmospheres Inferred from A-train Satellite Data." In Observing and Modelling Earth's Energy Flows. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-4327-4_21.

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Palme, Massimo. "Technological Imagination to Stay Within Planetary Boundaries." In The Urban Book Series. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-29515-7_35.

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AbstractTechnological imagination has been, until now, a stronger driver of development and has permitted to scale economy and even to obtain increasing returns of investments. However, times are a changing. Humanity faces now societal and environmental changes that are pushing the planet Earth toward a danger zone, overpassing recommended limits for several critical processes, such as bio-geochemical fluxes of nitrogen and phosphorus, greenhouse gases concentration in the atmosphere, biodiversity loss and land use change. The role of technology applied to built environment design should be re
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Zhang, Zhenyu, Patrick Laux, Jussi Baade, Hassane Moutahir, and Harald Kunstmann. "Regional Land–Atmosphere Interactions in Southern Africa: Potential Impact and Sensitivity of Forest and Plantation Change." In Sustainability of Southern African Ecosystems under Global Change. Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-10948-5_10.

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AbstractSouthern Africa is experiencing increasing land transformation and natural vegetation losses. Deforestation is one type of this land degradation where there are indigenous forests present, and afforestation of other nature ecosystems with timber plantations. This study performs regional coupled land–atmosphere model simulations using the Weather Research and Forecast (WRF) model with a resolution of 12 km, to assess the impact of forest and plantation cover change on regional climate in southern Africa. Three WRF simulations were designed for different land covers: (i) MODIS-derived la
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Tuck, Adrian F. "Non-Equilibrium Statistical Mechanics." In Atmospheric Turbulence. Oxford University Press, 2008. http://dx.doi.org/10.1093/oso/9780199236534.003.0010.

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The Earth’s atmosphere is far from equilibrium; it is constantly in motion from the combined effects of gravity and planetary rotation, is constantly absorbing and emitting radiation, and hosts ongoing chemical reactions which are ultimately fuelled by solar photons. It has fluxes of material and energy across its boundaries with the planetary surface, both terrestrial and marine, and also emits a continual outward flux of infrared photons to space. The gaseous atmosphere is manifestly a kinetic system, meaning that its evolution must be described by time dependent differential equations. The
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Kaimal, J. C., and J. J. Finnigan. "Sensors and Techniques for Observing the Boundary Layer." In Atmospheric Boundary Layer Flows. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195062397.003.0009.

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Sensors used for boundary layer measurements fall into two broad categories: in situ sensors that can be mounted on the ground, on masts, towers, tethered balloons, free balloons, or aircraft; and remote sensors, ground-based or aircraft-mounted, that infer atmospheric properties through their effects on acoustic, microwave, and optical signals propagating through the air. In situ sensors are the traditional instruments of choice for surface and lower boundary layer studies, being the only ones capable of the accuracy and resolution needed for quantitative work. A major portion of this chapter
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Conference papers on the topic "Atmospheric Energy Fluxes"

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Mandal, Maitrayee. "The appearance of tau neutrinos in the flux of atmospheric neutrinos at Super-Kamiokande." In 42nd International Conference on High Energy Physics. Sissa Medialab, 2024. https://doi.org/10.22323/1.476.0154.

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Gaisser, T. K., and Todor Stanev. "Atmospheric neutrino fluxes at low energy." In AIP Conference Proceedings Vol.126. AIP, 1985. http://dx.doi.org/10.1063/1.35157.

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Stevens, Blake, and Magdi Ragheb. "Atmospheric heat fluxes and restoration of the circumglobal equatorial current." In Renewable Energy Conference (INREC). IEEE, 2010. http://dx.doi.org/10.1109/inrec.2010.5462597.

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Kokovin, A. O., A. V. Kozyrev, V. Yu Kozhevnikov, and N. S. Semeniuk. "Characteristics of stationary negative corona discharge in atmospheric air." In 8th International Congress on Energy Fluxes and Radiation Effects. Crossref, 2022. http://dx.doi.org/10.56761/efre2022.s5-p-019502.

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The paper presents a 2D-axisymmetric multi-fluid model of a stationary negative corona discharge in atmospheric-pressure air in the needle-to-plane diode. Discharges with a cathode tip with a curvature radius of 20–200 μm, a gap length of 3–10 mm, and a power source voltage of 5–35 kV were studied. The spatial distribution of the discharge plasma at a current level of 2.2 mA with a gap voltage of 5.8 kV, gap length of 10 mm, tip radius of 100 μm is described in detail. This corona discharge has a glow discharge structure with a subnormal current density of 5 A/cm2.
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Mesyats, G. A., and I. V. Vasenina. "Nanosecond discharge in atmospheric air in submillimeter gaps in a uniform electric field." In 8th International Congress on Energy Fluxes and Radiation Effects. Crossref, 2022. http://dx.doi.org/10.56761/efre2022.s5-o-954301.

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A nanosecond electric discharge in air in submillimeter gaps at the overvoltages up to 15-fold is under investigation. The initial electric field in such discharges is up to 106 V/cm. This field is sufficient for the electrons that initiate the discharge, as well as those obtained during the discharge, to go into the runaway mode. These electrons are called runaway electrons (RE). REs create plasma in the period 10-9 s. When the plasma density is reached of 104 cm-3, a glow discharge (GD) is initiated. The process of transition of the discharge to the GD mode lasts 10-11 s. During this time, a
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Dyachenko, A. A., O. M. Stepanova, I. L. Iov, and M. E. Pinchuk. "Visualization of the temperature distribution in a DBD driven helium atmospheric pressure plasma jet." In 8th International Congress on Energy Fluxes and Radiation Effects. Crossref, 2022. http://dx.doi.org/10.56761/efre2022.s4-o-008705.

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A technique to visualize a gas temperature field in DBD-driven helium plasma jets is presented. It is implemented with recording infrared images on a thin glossy paper sheet placed into the jet in the line of the gas flow. The entrapment of the ambient air by the helium flow produces distortions in the measurement result; therefore, additional post processing of the images obtained has been carried out.
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Kokorina, Aleksandra, and Alexander Pak. "Hard Metal Waste Recycling by the Atmospheric Direct Current Arc Plasma." In 2020 7th International Congress on Energy Fluxes and Radiation Effects (EFRE). IEEE, 2020. http://dx.doi.org/10.1109/efre47760.2020.9241911.

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Tarasenko, Victor, Vladimir Kuznetsov, Viktor Skakun, Evgeniy Baksht, Viktor Panarin, and Edward Sosnin. "Ignition Different Mode of Corona Discharge in Air at Atmospheric Pressure." In 2020 7th International Congress on Energy Fluxes and Radiation Effects (EFRE). IEEE, 2020. http://dx.doi.org/10.1109/efre47760.2020.9241997.

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Kozlov, Boris, Dmitry Makhan'ko, and Mai The Nguyen. "Volume Discharges in CO2-Laser Mixtures at Atmospheric Pressures With High Energy Density." In 2020 7th International Congress on Energy Fluxes and Radiation Effects (EFRE). IEEE, 2020. http://dx.doi.org/10.1109/efre47760.2020.9242065.

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Zubarev, Nikolay, Konstantin Sharypov, Sergey Shunailov, Anna Sadykova, Valery Shpak, and Michael Yalandin. "Formation of the Secondary Runaway Electron Flow in an Elongated Atmospheric Gap." In 2020 7th International Congress on Energy Fluxes and Radiation Effects (EFRE). IEEE, 2020. http://dx.doi.org/10.1109/efre47760.2020.9241912.

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Reports on the topic "Atmospheric Energy Fluxes"

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Colby, Sean, Venkatraman Srinivasan, Tamas Varga, and Amirhossein Ahkami. Influence of vegetation canopy architecture on dynamics of spatiotemporal light distribution and its effect on land-biosphere-atmosphere fluxes of energy, carbon, and water. Office of Scientific and Technical Information (OSTI), 2020. http://dx.doi.org/10.2172/1987655.

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