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Libros sobre el tema "Atmospheric discharges"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 14 de febrero de 2022

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1

Kukkonen, Jaakko. Modelling of discharges and atmospheric dispersion of toxic gases. Helsinki: Finnish Meteorological Institute, 1987.

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2

D, Borisov N. y Milikh G. M, eds. Physics of microwave discharges: Artifically ionized regions in the atmosphere. Amsterdam, The Netherlands: Gordon and Breach, 1997.

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3

Workshop on Coupling of Thunderstorms and Lightning Discharges to Near-Earth Space (2008 University of Corsica). Coupling of thunderstorms and lightning discharges to near-earth space: Proceedings of the workshop, Corte, France, 23-27 June 2008. Editado por Crosby N. (Norma), Huang Tai-Yin y Rycroft Michael J. Melville, N.Y: American Institute of Physics, 2009.

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4

Jarzembski, M. A. Low-pressure electrical discharge experiment to simulate high-altitude lightning above thunderclouds. MSFC, Ala: National Aeronautics and Space Administration, Marshall Space Flight Center, 1995.

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5

Jarzembski, M. A. Low-pressure electrical discharge experiment to simulate high-altitude lightning above thunderclouds. MSFC, Ala: National Aeronautics and Space Administration, Marshall Space Flight Center, 1995.

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6

Jarzembski, M. A. Low-pressure electrical discharge experiment to simulate high-altitude lightning above thunderclouds. Marshall Space Flight Center, Alabama: Marshall Space Flight Center, 1995.

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7

Jarzembski, M. A. Low-pressure electrical discharge experiment to simulate high-altitude lightning above thunderclouds. MSFC, Ala: National Aeronautics and Space Administration, Marshall Space Flight Center, 1995.

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8

Tooraj, Jamasb y Pollitt Michael G, eds. Delivering a low carbon electricity system: Technologies, economics, and policy. Cambridge: Cambridge University Press, 2008.

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9

Roth, J. Reece. Boundary layer flow control with a One Atmosphere Uniform Glow Disclharge Surface Plasmaa. Reston, Va: American Institute of Aeronautics and Astronautics, 1998.

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10

Ash, Robert F. Enhanced glow discharge production of oxygen: Final report for the period ending December 31, 1997; under research grant NAG-1-1140. Norfolk, Va: Dept. of Aerospace Engineering, College of Engineering and Technology, Old Dominion University, 1998.

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11

The Atmosphere And Ionosphere Elementary Processes Discharges And Plasmoids. Springer, 2012.

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12

Electrode erosion in arc discharges at atmospheric pressure. [Washington, D.C: National Aeronautics and Space Administration, 1985.

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13

Issledovanii͡a︡ ėlektricheskikh razri͡a︡dov v atmosfere: Sbornik nauchnykh trudov. I͡A︡roslavlʹ: I͡A︡roslavskiĭ gos. universitet, 1991.

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14

Bychkov, Vladimir, Gennady Golubkov y Anatoly Nikitin. The Atmosphere and Ionosphere: Elementary Processes, Discharges and Plasmoids. Springer, 2015.

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15

Baur, Susanna S. An atmospheric pressure glow discharge detector for capillary column gas chromatography. 1995.

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16

(Editor), Martin Füllekrug, Eugene A. Mareev (Editor) y Michael J. Rycroft (Editor), eds. Sprites, Elves and Intense Lightning Discharges (NATO Science Series II: Mathematics, Physics and Chemistry). Springer, 2006.

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17

Vandanā, Śrīvāstava, ed. Low pressure experimental simulation of electrical discharges above and inside a cloud. [Washington, D.C: National Aeronautics and Space Administration, 1997.

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18

Vandanā, Śrīvāstava y United States. National Aeronautics and Space Administration., eds. Low pressure experimental simulation of electrical discharges above and inside a cloud. [Washington, D.C: National Aeronautics and Space Administration, 1997.

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19

Foster, P. M. y A. G. Robins. The Effects of Buildings on Low-level Atmospheric Discharges (Nuclear Science and Technology). European Communities / Union (EUR-OP/OOPEC/OPOCE), 1985.

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20

Eggleton, A. E. J. The Possible Impact of Atmospheric Radioactive Discharges from UK Nuclear Installations on Acid Deposition. AEA Technology Plc, 1986.

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21

E. M. Van Veldhuizen (Editor) y E. M. Van Veldhuizen (Editor), eds. Electrical Discharges for Environmental Purposes: Fundamentals and Applications. Nova Science Publishers, 2000.

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22

Lodge, Oliver. Lightning Conductors and Lightning Guards: A Treatise on the Protection of Buildings, of Telegraph Instruments and Submarine Cables, and of Electrical Installations Generally, from Damage by Atmospheric Discharges. University of Cambridge ESOL Examinations, 2012.

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23

Wheatley, C. J. Discharge of Liquid Ammonia to Moist Atmospheres. AEA Technology, 1987.

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24

Behera, Swadhin y Toshio Yamagata. Climate Dynamics of ENSO Modoki Phenomena. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.612.

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The El Niño Modoki/La Niña Modoki (ENSO Modoki) is a newly acknowledged face of ocean-atmosphere coupled variability in the tropical Pacific Ocean. The oceanic and atmospheric conditions associated with the El Niño Modoki are different from that of canonical El Niño, which is extensively studied for its dynamics and worldwide impacts. A typical El Niño event is marked by a warm anomaly of sea surface temperature (SST) in the equatorial eastern Pacific. Because of the associated changes in the surface winds and the weakening of coastal upwelling, the coasts of South America suffer from widespread fish mortality during the event. Quite opposite of this characteristic change in the ocean condition, cold SST anomalies prevail in the eastern equatorial Pacific during the El Niño Modoki events, but with the warm anomalies intensified in the central Pacific. The boreal winter condition of 2004 is a typical example of such an event, when a tripole pattern is noticed in the SST anomalies; warm central Pacific flanked by cold eastern and western regions. The SST anomalies are coupled to a double cell in anomalous Walker circulation with rising motion in the central parts and sinking motion on both sides of the basin. This is again a different feature compared to the well-known single-cell anomalous Walker circulation during El Niños. La Niña Modoki is the opposite phase of the El Niño Modoki, when a cold central Pacific is flanked by warm anomalies on both sides.The Modoki events are seen to peak in both boreal summer and winter and hence are not seasonally phase-locked to a single seasonal cycle like El Niño/La Niña events. Because of this distinction in the seasonality, the teleconnection arising from these events will vary between the seasons as teleconnection path will vary depending on the prevailing seasonal mean conditions in the atmosphere. Moreover, the Modoki El Niño/La Niña impacts over regions such as the western coast of the United States, the Far East including Japan, Australia, and southern Africa, etc., are opposite to those of the canonical El Niño/La Niña. For example, the western coasts of the United States suffer from severe droughts during El Niño Modoki, whereas those regions are quite wet during El Niño. The influences of Modoki events are also seen in tropical cyclogenesis, stratosphere warming of the Southern Hemisphere, ocean primary productivity, river discharges, sea level variations, etc. A remarkable feature associated with Modoki events is the decadal flattening of the equatorial thermocline and weakening of zonal thermal gradient. The associated ocean-atmosphere conditions have caused frequent and persistent developments of Modoki events in recent decades.
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25

Plotkin, Mark J. The Amazon. Oxford University Press, 2020. http://dx.doi.org/10.1093/wentk/9780190668297.001.0001.

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The Amazon is a land of superlatives. The complex ecosystem covers an area about the size of the continental U.S. The Amazon River discharges 57 million gallons of water per second--in two hours, this would be enough to supply all of New York City’s 7.5 million residents with water for a year. Its flora and fauna are abundant. Approximately one of every four flowering plant species on earth resides in the Amazon. A single Amazonian river may contain more fish species than all the rivers in Europe combined. It is home to the world's largest anteater, armadillo, freshwater turtle, and spider, as well as the largest rodent (which weighs over 200 lbs.), catfish (250 lbs.), and alligator (more than half a ton). The rainforest, which contains approximately 390 billion trees, plays a vital role in stabilizing the global climate by absorbing massive amounts of carbon dioxide--or releasing it into the atmosphere if the trees are destroyed. Severe droughts in both Brazil and Southeast Asia have been linked to Amazonian deforestation, as have changing rainfall patterns in the U.S., Europe, and China. The Amazon also serves as home to millions of people. Approximately seventy tribes of isolated and uncontacted people are concentrated in the western Amazon, completely dependent on the land and river. These isolated groups have been described as the most marginalized peoples in the western hemisphere, with no voice in the decisions made about their futures and the fate of their forests. In this addition to the What Everyone Needs to Know® series, ecologist and conservation expert, Mark J. Plotkin, who has spent 40 years studying Amazonia, its peoples, flora, and fauna. The Amazon offers an engaging overview of this irreplaceable ecosystem and the challenges it faces.
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