Academic literature on the topic 'Lightning and Sprites'

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Journal articles on the topic "Lightning and Sprites"

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McLeish, Peter. "The Historic Search for Red Sprites: Art Meets Science in Lightning's Angels." Leonardo 38, no. 2 (2005): 109–14. http://dx.doi.org/10.1162/0024094053722417.

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Sprites are fleeting, luminous shapes that shoot into the upper atmosphere during large thunderstorms as lightning simultaneously reaches down to Earth. For at least a century, scientists have attempted to confirm and explain the existence of sprites with visual images and data. The author's series Lightning's Angels supplements the documentation of sprites by exploring the properties of this natural phenomenon through digitally enhanced oil portraits set to music and displayed in a large scale multimedia format, such as at a planetarium.
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Füllekrug, M., R. Roussel-Dupré, E. M. D. Symbalisty, et al. "Relativistic electron beams above thunderclouds." Atmospheric Chemistry and Physics 11, no. 15 (2011): 7747–54. http://dx.doi.org/10.5194/acp-11-7747-2011.

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Abstract. Non-luminous relativistic electron beams above thunderclouds have been detected by the radio signals of low frequency ∼40–400 kHz which they radiate. The electron beams occur ∼2–9 ms after positive cloud-to-ground lightning discharges at heights between ∼22–72 km above thunderclouds. Intense positive lightning discharges can also cause sprites which occur either above or prior to the electron beam. One electron beam was detected without any luminous sprite which suggests that electron beams may also occur independently of sprites. Numerical simulations show that beams of electrons pa
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Pan, Cong, Jing Yang, Kun Liu, and Yu Wang. "Comprehensive Analysis of a Coast Thunderstorm That Produced a Sprite over the Bohai Sea." Atmosphere 12, no. 6 (2021): 718. http://dx.doi.org/10.3390/atmos12060718.

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Sprites are transient luminous events (TLEs) that occur over thunderstorm clouds that represent the direct coupling relationship between the troposphere and the upper atmosphere. We report the evolution of a mesoscale convective system (MCS) that produced only one sprite event, and the characteristics of this thunderstorm and the related lightning activity are analyzed in detail. The results show that the parent flash of the sprite was positive cloud-to-ground lightning (+CG) with a single return stroke, which was located in the trailing stratiform region of the MCS with a radar reflectivity o
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Marshall, R. A., U. S. Inan, T. Neubert, et al. "Optical observations geomagnetically conjugate to sprite-producing lightning discharges." Annales Geophysicae 23, no. 6 (2005): 2231–37. http://dx.doi.org/10.5194/angeo-23-2231-2005.

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Abstract. Theoretical studies have predicted that large positive cloud-to-ground discharges can trigger a runaway avalanche process of relativistic electrons, forming a geomagnetically trapped electron beam. The beam may undergo pitch angle and energy scattering during its traverse of the Earth's magnetosphere, with a small percentage of electrons remaining in the loss cone and precipitating in the magnetically conjugate atmosphere. In particular, N2 1P and N2+1N optical emissions are expected to be observable. In July and August 2003, an attempt was made to detect these optical emissions, cal
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Barrington-Leigh, C. P., U. S. Inan, M. Stanley, and S. A. Cummer. "Sprites triggered by negative lightning discharges." Geophysical Research Letters 26, no. 24 (1999): 3605–8. http://dx.doi.org/10.1029/1999gl010692.

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Lyons, Walter A., Eric C. Bruning, Tom A. Warner, et al. "Megaflashes: Just How Long Can a Lightning Discharge Get?" Bulletin of the American Meteorological Society 101, no. 1 (2019): E73—E86. http://dx.doi.org/10.1175/bams-d-19-0033.1.

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Abstract The existence of mesoscale lightning discharges on the order of 100 km in length has been known since the radar-based findings of Ligda in the mid-1950s. However, it took the discovery of sprites in 1989 to direct significant attention to horizontally extensive “megaflashes” within mesoscale convective systems (MCSs). More recently, 3D Lightning Mapping Arrays (LMAs) have documented sprite-initiating lightning discharges traversing several hundred kilometers. One such event in a 2007 Oklahoma MCS having an LMA-derived length of 321 km, has been certified by the WMO as the longest offi
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Valdivia, J. A., G. Milikh, and K. Papadopoulos. "Red sprites: Lightning as a fractal antenna." Geophysical Research Letters 24, no. 24 (1997): 3169–72. http://dx.doi.org/10.1029/97gl03188.

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Fernsler, R. F., and H. L. Rowland. "Models of lightning-produced sprites and elves." Journal of Geophysical Research: Atmospheres 101, no. D23 (1996): 29653–62. http://dx.doi.org/10.1029/96jd02159.

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Rodger, Craig J. "Red sprites, upward lightning, and VLF perturbations." Reviews of Geophysics 37, no. 3 (1999): 317–36. http://dx.doi.org/10.1029/1999rg900006.

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Kuo, Cheng-Ling, Tai-Yin Huang, Cheng-Mao Hsu, Mitsuteru Sato, Lou-Chuang Lee, and Neng-Huei Lin. "Resolving Elve, Halo and Sprite Halo Images at 10,000 Fps in the Taiwan 2020 Campaign." Atmosphere 12, no. 8 (2021): 1000. http://dx.doi.org/10.3390/atmos12081000.

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After almost thirty years’ efforts on studying transient luminous events (TLEs), ground-based observation has confirmed the TLE family, including elves, halos, sprites, and blue jets, etc. The typical elve has the shortest emission time (<1 ms) in comparison with other TLEs. The second shortest is the halo emission. Although elves and halos are supposed to be more frequent than sprites, ground campaigns still have less probability of recording their images due to their fleeting and short emission. Additionally, the submillisecond imaging of elves, halos, and sprite halos helps us resolve th
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Dissertations / Theses on the topic "Lightning and Sprites"

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Knutsson, Lars. "Sprite observations over France in relation to their parent thunderstorm system." Thesis, Uppsala universitet, Luft-, vatten och landskapslära, 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-303775.

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As a part of the European research program CAL, sprite observations were carried out from the OMP observatory in the French Pyrenees during the summer 2003. Images of the sprites were taken by two remotely controlled CCD cameras. The 23 July was considered particularly interesting because we then had access to data concerning both cloud-to-ground and intracloud lightning activity. This day was therefore chosen as the object of the present study. A large thunderstorm with two convective cores, one to the north and the other to the south, developed over the South of France during the late aftern
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Thomas, Jeremy Norman. "Lightning-driven electric and magnetic fields measured in the stratosphere : implications for sprites /." Thesis, Connect to this title online; UW restricted, 2005. http://hdl.handle.net/1773/6838.

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Allgood, Michael David Baginski Michael E. "Finite element analysis of the mesosphere's electromagnetic response to large scale lightning associated with sprites and other transient luminous events." Auburn, Ala, 2008. http://repo.lib.auburn.edu/EtdRoot/2008/SPRING/Electrical_and_Computer_Engineering/Thesis/Allgood_Michael_37.pdf.

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Hammond, C., D. Beauvarlet, A. Kipple, et al. "TELEMETERING SYSTEM FOR THE UA SATELLITE." International Foundation for Telemetering, 2000. http://hdl.handle.net/10150/607700.

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International Telemetering Conference Proceedings / October 23-26, 2000 / Town & Country Hotel and Conference Center, San Diego, California<br>This student paper was produced as part of the team design competition in the University of Arizona course ECE 485, Radiowaves and Telemetry. It presents a telemetering system proposed for UASat, a small satellite being designed for launch in the year 2004. The overall system architecture is described, including the transducers used by each subsystem, the command and telemetry packet formats, the antennas and modulation schemes, the link budget, and som
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Vieira, Antonioni de Freitas. ""Identificação de relâmpagos e sprites na atmosfera pelo imageador ALIS a bordo do satélite científico EQUARS"." Universidade de São Paulo, 2006. http://www.teses.usp.br/teses/disponiveis/55/55134/tde-02092006-010741/.

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O Sistema ALIS (Atmospheric Limb Imaging System), do Instituto Nacional de Pesquisas Espaciais (INPE) em São José dos Campos, a bordo do satélite EQUARS (Equatorial Atmosphere Research Satellite), tem como objetivo observar três fenômenos ópticos da atmosfera na direção horizontal (Limb) do satélite em órbita: a aeroluminescência, os relâmpagos e os sprites. Os sprites são fenômenos luminosos verticais que ocorrem na mesosfera e ionosfera inferior de coloração vermelho-alaranjada e o seu estudo é de grande importância devido à influência que exerce sobre o clima terrestre, juntamente com de
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Chang, Tom Y. 1976. "On the nature of electrified clouds that create positively polarized cloud-to-ground lightning and their link to sprites." Thesis, Massachusetts Institute of Technology, 1998. http://hdl.handle.net/1721.1/17452.

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Bailey, Matthew A. "Investigating Characteristics of Lightning-Induced Transient Luminous Events Over South America." DigitalCommons@USU, 2010. http://digitalcommons.usu.edu/etd/667.

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Sprites, halos, and elves are members of a family of short-lived, luminous phenomena known as Transient Luminous Events (TLEs), which occur in the middle atmosphere. Sprites are vertical glows occurring at altitudes typically ranging from ~40 to 90 km. In video imagery they exhibit a red color at their top, with blue tendril-like structure at low altitudes. Elves are disk-like glows that occur at the base of the ionosphere, with diameters of ~100-300 km, and have very short lifetimes (~2-3 ms). Halos are diffuse glows that occur at low altitudes, have diameters <100 km, and have a duration
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Cheng-HsiKuo and 郭政昕. "The Characteristics of the Sprites and Their Parent Lightning Captured by Taiwan TLE Observation Network." Thesis, 2019. http://ndltd.ncl.edu.tw/handle/w3bpzk.

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碩士<br>國立成功大學<br>物理學系<br>107<br>Williams et al. (2007) summazied that more than 99.9% sprites are initiated by positive cloud-to-ground (+CG) and high charge moment change (CMC). After the launch of Formosat-2, the Imager of Sprite Upper Atmosphere Lightning (ISUAL) obtained the sprite globally for the first time and had a chance to investigate their polarities. The result surprisingly indicated that more than 20% of sprite events were triggered by negative cloud-to-ground lightning, totally different from the previous statistic results. Furthermore, most of negative sprites distribute over low
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Lee, Young-Sook. "Summer high latitude mesospheric observations of supersonic bursts and O(1S) emission rate with the UARS/WINDII instrument and the association with sprites, meteors and lightning /." 2009. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&res_dat=xri:pqdiss&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:NR51732.

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Thesis (Ph.D.)--York University, 2009. Graduate Programme in Earth and Space Science and Engineering.<br>Typescript. Includes bibliographical references (leaves 149-174). Also available on the Internet. MODE OF ACCESS via web browser by entering the following URL: http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&res_dat=xri:pqdiss&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:NR51732
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Books on the topic "Lightning and Sprites"

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Füllekrug, Martin, Eugene A. Mareev, and Michael J. Rycroft, eds. Sprites, Elves and Intense Lightning Discharges. Springer Netherlands, 2006. http://dx.doi.org/10.1007/1-4020-4629-4.

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Füllekrug, Martin, Eugene A. Mareev, and Michael J. Rycroft. "Sprites, Elves and Intense Lightning Discharges". Springer, 2009.

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Füllekrug, Martin, Eugene A. Mareev, and Michael J. Rycroft. "Sprites, Elves and Intense Lightning Discharges". Springer, 2019.

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(Editor), Martin Füllekrug, Eugene A. Mareev (Editor), and 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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(Editor), Martin Füllekrug, Eugene A. Mareev (Editor), and 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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Goldsmith, Thomas. Earl Scruggs and Foggy Mountain Breakdown. University of Illinois Press, 2019. http://dx.doi.org/10.5622/illinois/9780252042966.001.0001.

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Earl Eugene Scruggs (1924-2012) came from the hills of North Carolina and learned the banjo from the days he was too small to hold it properly. While still a schoolboy in Boiling Springs, North Carolina, he developed the high-powered three-finger picking method that both him and the banjo famous. At age 21, he joined the founder of bluegrass music, Bill Monroe, on the Grand Ole Opry, completing a sound that Monroe had worked to conceive. Leaving Monroe in 1948, Scruggs and guitarist Lester Flatt started their own group and made recordings including “Foggy Mountain Breakdown.” The lightning-fas
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Book chapters on the topic "Lightning and Sprites"

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Mende, Stephen B., Y. S. Chang, A. B. Chen, et al. "SPACECRAFT BASED STUDIES OF TRANSIENT LUMINOUS EVENTS." In Sprites, Elves and Intense Lightning Discharges. Springer Netherlands, 2006. http://dx.doi.org/10.1007/1-4020-4629-4_6.

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Miller, Andrew, Iddo Bentov, Surya Bakshi, Ranjit Kumaresan, and Patrick McCorry. "Sprites and State Channels: Payment Networks that Go Faster Than Lightning." In Financial Cryptography and Data Security. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-32101-7_30.

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Shalimov, S. L., and T. Bösinger. "Sprite-Producing Lightning-Ionosphere Coupling and Associated Low-Frequency Phenomena." In Dynamic Coupling Between Earth’s Atmospheric and Plasma Environments. Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4614-5677-3_18.

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Conference papers on the topic "Lightning and Sprites"

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Hayakawa, M., T. Nakamura, Y. Hobara, and E. Williams. "Observation of sprites over the Sea of Japan and conditions for lightning-induced sprites in winter." In Proceedings. Asia-Pacific Conference on Environmental Electromagnetics. IEEE, 2003. http://dx.doi.org/10.1109/ceem.2003.238406.

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Rycroft, M. J., and A. Odzimek. "Modeling changes of the ionospheric potential due to lightning and sprites." In 2011 XXXth URSI General Assembly and Scientific Symposium. IEEE, 2011. http://dx.doi.org/10.1109/ursigass.2011.6050943.

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Wang, Yongping, Gaopeng Lu, Ming Ma, and Baoyou Zhu. "Analysis of Red Sprites in the Middle and High Latitudes of China." In 2019 11th Asia-Pacific International Conference on Lightning (APL). IEEE, 2019. http://dx.doi.org/10.1109/apl.2019.8816022.

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São Sabbas, F. T., O. Pinto Jr., O. Mendes Jr., and M. J. Taylor. "Study Of The Relationship Between Sprites And Lightning From The Associated Storms." In 6th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1999. http://dx.doi.org/10.3997/2214-4609-pdb.215.sbgf249.

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Yaniv, Roy, Adam D. Devir, Yoav Yair, et al. "Calibration of CCD Cameras for Measurements of Sprites and Elves." In COUPLING OF THUNDERSTORMS AND LIGHTNING DISCHARGES TO NEAR-EARTH SPACE: Proceedings of the Workshop. AIP, 2009. http://dx.doi.org/10.1063/1.3137719.

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Jianqi Qin, S. Celestin, and V. P. Pasko. "Minimum charge moment change in positive and negative cloud to ground lightning discharges producing sprites." In 2013 US National Committee of URSI National Radio Science Meeting (USNC-URSI NRSM). IEEE, 2013. http://dx.doi.org/10.1109/usnc-ursi-nrsm.2013.6524972.

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Rycroft, Michael J., Anna Odzimek, Norma B. Crosby, Tai-Yin Huang, and Michael J. Rycroft. "The Impact of Lightning Flashes and Sprites on the Earth’s Global Electric Circuit: An Overview of Recent Modeling Results." In COUPLING OF THUNDERSTORMS AND LIGHTNING DISCHARGES TO NEAR-EARTH SPACE: Proceedings of the Workshop. AIP, 2009. http://dx.doi.org/10.1063/1.3137704.

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Baginski, M. E., D. L. Faircloth, S. M. Rao, and S. M. Wentworth. "Finite element characterization of the power density, energy deposition, and transient electron density profiles associated with lightning induced sprites." In 2006 IEEE Antennas and Propagation Society International Symposium. IEEE, 2006. http://dx.doi.org/10.1109/aps.2006.1711187.

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Hiraki, Yasutaka. "On polarity asymmetry of the occurrence rate of sprite discharges." In 2010 30th International Conference on Lightning Protection (ICLP). IEEE, 2010. http://dx.doi.org/10.1109/iclp.2010.7845807.

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Ushio, Tomoo, Mitsuteru Sato, Takeshi Morimoto, et al. "Global lightning and sprite measurements from International Space Station." In 2014 XXXIth URSI General Assembly and Scientific Symposium (URSI GASS). IEEE, 2014. http://dx.doi.org/10.1109/ursigass.2014.6929579.

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Reports on the topic "Lightning and Sprites"

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Krehbiel, Paul R. Development of a Field-Deployable Observational System for Characterizing Lightning in Sprite-Producing Storms. Defense Technical Information Center, 1998. http://dx.doi.org/10.21236/ada359325.

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