Library of Simulated Gamma‐Ray Glows and Application to Previous Airborne Observations
Gamma‐Ray Glows (GRGs) are high energy radiation originating from thunderclouds, in the MeV energy regime, with typical duration of seconds to minutes, and sources extended over several to tens of square kilometers. GRGs have been observed from detectors placed on ground, inside aircraft and on ball...
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description | Gamma‐Ray Glows (GRGs) are high energy radiation originating from thunderclouds, in the MeV energy regime, with typical duration of seconds to minutes, and sources extended over several to tens of square kilometers. GRGs have been observed from detectors placed on ground, inside aircraft and on balloons. In this paper, we present a general purpose Monte‐Carlo model of GRG production and propagation. This model is first compared to a model from Zhou et al. (2016, https://doi.org/10.1016/j.astropartphys.2016.08.004) relying on another Monte‐Carlo framework, and small differences are observed. We then have built an extensive simulation library, made available to the community. This library is used to reproduce five previous gamma‐ray glow observations, from five airborne campaigns: balloons from Eack et al. (1996b, https://doi.org/10.1029/96gl02570), Eack et al. (2000, https://doi.org/10.1029/1999gl010849); and aircrafts from ADELE (Kelley et al., 2015, https://doi.org/10.1038/ncomms8845), ILDAS (Kochkin et al., 2017, https://doi.org/10.1002/2017jd027405) and ALOFT (Østgaard et al., 2019, https://doi.org/10.1029/2019jd030312). Our simulation results confirm that fluxes of cosmic‐ray secondary particles present in the background at a given altitude can be enhanced by several percent (MOS process), and up to several orders of magnitude (RREA process) due to the effect of thunderstorms' electric fields, and explain the five observations. While some GRG could be explained purely by the MOS process, E‐fields significantly larger than Eth are required to explain the strongest GRGs observed. Some of the observations also came with in‐situ electric field measurements, that were always lower than Eth, but may not have been obtained from regions where the glows are produced. This study supports the claim that kilometer‐scale E‐fields magnitudes of at least the level of Eth must be present inside some thunderstorms.
Plain Language Summary
Gamma‐Ray Glows (GRGs) are high‐energy radiation that originates from thunderclouds. These radiations fall within the MeV energy range and last for seconds to minutes. The sources of GRGs are typically extended over a few to tens of square kilometers. In this study, we developed a general‐purpose model to understand the production of GRGs, including the cosmic ray fluxes and enhancement by thunderstorm's electric field, propagation, and instrumental response. Using this model, we were able to reproduce and constrain five previously rep |
doi_str_mv | 10.1029/2022JD037956 |
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Plain Language Summary
Gamma‐Ray Glows (GRGs) are high‐energy radiation that originates from thunderclouds. These radiations fall within the MeV energy range and last for seconds to minutes. The sources of GRGs are typically extended over a few to tens of square kilometers. In this study, we developed a general‐purpose model to understand the production of GRGs, including the cosmic ray fluxes and enhancement by thunderstorm's electric field, propagation, and instrumental response. Using this model, we were able to reproduce and constrain five previously reported airborne GRG observations, two from balloons, and three from aircraft. The results of our study showed that all of the observations could be explained by one of the two expected regimes: one involving purely particle acceleration (MOS: Modification of Spectrum) and the other involving particle multiplication (RREA: Relativistic Runaway Electron Avalanche). Our simulations suggest that the required large‐scale thunderstorm electric fields, which are compatible with our results, are generally larger than what was previously measured.
Key Points
A general‐purpose Monte‐Carlo model of gamma‐ray glow production is presented
Plausible Gamma‐ray Glow production conditions are provided for five previous airborne observations
Some cases could be explained by the Modification of Spectrum mechanism only while other require electric fields close to Relativistic Runaway Electron Avalanche process threshold, or above</description><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2169-8996</identifier><identifier>DOI: 10.1029/2022JD037956</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>airborne observations ; Aircraft ; Balloons ; Cosmic radiation ; Cosmic ray showers ; Cosmic rays ; Detectors ; Electric field ; Electric fields ; electron ; Electron avalanche ; Energy ; Fluxes ; gamma ray glow ; GEANT4 ; Geophysics ; High energy astronomy ; Libraries ; Meteorological balloons ; Modelling ; Particle acceleration ; positron ; Propagation ; Radiation ; Relativistic particles ; Simulation ; thunderstorm ; Thunderstorms ; Weather</subject><ispartof>Journal of geophysical research. Atmospheres, 2023-05, Vol.128 (9), p.n/a</ispartof><rights>2023. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2960-5770290867697545e37779a2c90908dfbe2cc8144f2a9841d11cb58f00124303</citedby><cites>FETCH-LOGICAL-c2960-5770290867697545e37779a2c90908dfbe2cc8144f2a9841d11cb58f00124303</cites><orcidid>0000-0001-5721-6783 ; 0000-0002-3471-7267 ; 0000-0002-2572-7033 ; 0000-0002-4000-3789</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2022JD037956$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2022JD037956$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,27924,27925,45574,45575</link.rule.ids></links><search><creatorcontrib>Sarria, D.</creatorcontrib><creatorcontrib>Østgaard, N.</creatorcontrib><creatorcontrib>Marisaldi, M.</creatorcontrib><creatorcontrib>Lehtinen, N.</creatorcontrib><creatorcontrib>Mezentsev, A.</creatorcontrib><title>Library of Simulated Gamma‐Ray Glows and Application to Previous Airborne Observations</title><title>Journal of geophysical research. Atmospheres</title><description>Gamma‐Ray Glows (GRGs) are high energy radiation originating from thunderclouds, in the MeV energy regime, with typical duration of seconds to minutes, and sources extended over several to tens of square kilometers. GRGs have been observed from detectors placed on ground, inside aircraft and on balloons. In this paper, we present a general purpose Monte‐Carlo model of GRG production and propagation. This model is first compared to a model from Zhou et al. (2016, https://doi.org/10.1016/j.astropartphys.2016.08.004) relying on another Monte‐Carlo framework, and small differences are observed. We then have built an extensive simulation library, made available to the community. This library is used to reproduce five previous gamma‐ray glow observations, from five airborne campaigns: balloons from Eack et al. (1996b, https://doi.org/10.1029/96gl02570), Eack et al. (2000, https://doi.org/10.1029/1999gl010849); and aircrafts from ADELE (Kelley et al., 2015, https://doi.org/10.1038/ncomms8845), ILDAS (Kochkin et al., 2017, https://doi.org/10.1002/2017jd027405) and ALOFT (Østgaard et al., 2019, https://doi.org/10.1029/2019jd030312). Our simulation results confirm that fluxes of cosmic‐ray secondary particles present in the background at a given altitude can be enhanced by several percent (MOS process), and up to several orders of magnitude (RREA process) due to the effect of thunderstorms' electric fields, and explain the five observations. While some GRG could be explained purely by the MOS process, E‐fields significantly larger than Eth are required to explain the strongest GRGs observed. Some of the observations also came with in‐situ electric field measurements, that were always lower than Eth, but may not have been obtained from regions where the glows are produced. This study supports the claim that kilometer‐scale E‐fields magnitudes of at least the level of Eth must be present inside some thunderstorms.
Plain Language Summary
Gamma‐Ray Glows (GRGs) are high‐energy radiation that originates from thunderclouds. These radiations fall within the MeV energy range and last for seconds to minutes. The sources of GRGs are typically extended over a few to tens of square kilometers. In this study, we developed a general‐purpose model to understand the production of GRGs, including the cosmic ray fluxes and enhancement by thunderstorm's electric field, propagation, and instrumental response. Using this model, we were able to reproduce and constrain five previously reported airborne GRG observations, two from balloons, and three from aircraft. The results of our study showed that all of the observations could be explained by one of the two expected regimes: one involving purely particle acceleration (MOS: Modification of Spectrum) and the other involving particle multiplication (RREA: Relativistic Runaway Electron Avalanche). Our simulations suggest that the required large‐scale thunderstorm electric fields, which are compatible with our results, are generally larger than what was previously measured.
Key Points
A general‐purpose Monte‐Carlo model of gamma‐ray glow production is presented
Plausible Gamma‐ray Glow production conditions are provided for five previous airborne observations
Some cases could be explained by the Modification of Spectrum mechanism only while other require electric fields close to Relativistic Runaway Electron Avalanche process threshold, or above</description><subject>airborne observations</subject><subject>Aircraft</subject><subject>Balloons</subject><subject>Cosmic radiation</subject><subject>Cosmic ray showers</subject><subject>Cosmic rays</subject><subject>Detectors</subject><subject>Electric field</subject><subject>Electric fields</subject><subject>electron</subject><subject>Electron avalanche</subject><subject>Energy</subject><subject>Fluxes</subject><subject>gamma ray glow</subject><subject>GEANT4</subject><subject>Geophysics</subject><subject>High energy astronomy</subject><subject>Libraries</subject><subject>Meteorological balloons</subject><subject>Modelling</subject><subject>Particle acceleration</subject><subject>positron</subject><subject>Propagation</subject><subject>Radiation</subject><subject>Relativistic particles</subject><subject>Simulation</subject><subject>thunderstorm</subject><subject>Thunderstorms</subject><subject>Weather</subject><issn>2169-897X</issn><issn>2169-8996</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp9kE1OwzAQhS0EElXpjgNYYkvAdhz_LKsWAlUlUOmiu8hJHMlVEgc7adUdR-CMnARDEWLFbGY0-vTmzQPgEqMbjIi8JYiQxRzFXCbsBIwIZjISUrLT35lvzsHE-y0KJVBMEzoCm6XJnXIHaCv4YpqhVr0uYaqaRn28va_UAaa13Xuo2hJOu642heqNbWFv4bPTO2MHD6fG5da1Gj7lXrvdN-AvwFmlaq8nP30M1vd369lDtHxKH2fTZVQQyVCUcB7MI8E4kzyhiY4551KRQqKwLatck6IQmNKKKCkoLjEu8kRUCGFCYxSPwdVRtnP2ddC-z7Z2cG24mBGBMQ1yhAfq-kgVznrvdJV1zjTh7Qyj7Cu97G96AY-P-N7U-vAvmy3S1TwRjKH4EwG5b40</recordid><startdate>20230516</startdate><enddate>20230516</enddate><creator>Sarria, D.</creator><creator>Østgaard, N.</creator><creator>Marisaldi, M.</creator><creator>Lehtinen, N.</creator><creator>Mezentsev, A.</creator><general>Blackwell Publishing Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0001-5721-6783</orcidid><orcidid>https://orcid.org/0000-0002-3471-7267</orcidid><orcidid>https://orcid.org/0000-0002-2572-7033</orcidid><orcidid>https://orcid.org/0000-0002-4000-3789</orcidid></search><sort><creationdate>20230516</creationdate><title>Library of Simulated Gamma‐Ray Glows and Application to Previous Airborne Observations</title><author>Sarria, D. ; Østgaard, N. ; Marisaldi, M. ; Lehtinen, N. ; Mezentsev, A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2960-5770290867697545e37779a2c90908dfbe2cc8144f2a9841d11cb58f00124303</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>airborne observations</topic><topic>Aircraft</topic><topic>Balloons</topic><topic>Cosmic radiation</topic><topic>Cosmic ray showers</topic><topic>Cosmic rays</topic><topic>Detectors</topic><topic>Electric field</topic><topic>Electric fields</topic><topic>electron</topic><topic>Electron avalanche</topic><topic>Energy</topic><topic>Fluxes</topic><topic>gamma ray glow</topic><topic>GEANT4</topic><topic>Geophysics</topic><topic>High energy astronomy</topic><topic>Libraries</topic><topic>Meteorological balloons</topic><topic>Modelling</topic><topic>Particle acceleration</topic><topic>positron</topic><topic>Propagation</topic><topic>Radiation</topic><topic>Relativistic particles</topic><topic>Simulation</topic><topic>thunderstorm</topic><topic>Thunderstorms</topic><topic>Weather</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sarria, D.</creatorcontrib><creatorcontrib>Østgaard, N.</creatorcontrib><creatorcontrib>Marisaldi, M.</creatorcontrib><creatorcontrib>Lehtinen, N.</creatorcontrib><creatorcontrib>Mezentsev, A.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of geophysical research. Atmospheres</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sarria, D.</au><au>Østgaard, N.</au><au>Marisaldi, M.</au><au>Lehtinen, N.</au><au>Mezentsev, A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Library of Simulated Gamma‐Ray Glows and Application to Previous Airborne Observations</atitle><jtitle>Journal of geophysical research. Atmospheres</jtitle><date>2023-05-16</date><risdate>2023</risdate><volume>128</volume><issue>9</issue><epage>n/a</epage><issn>2169-897X</issn><eissn>2169-8996</eissn><abstract>Gamma‐Ray Glows (GRGs) are high energy radiation originating from thunderclouds, in the MeV energy regime, with typical duration of seconds to minutes, and sources extended over several to tens of square kilometers. GRGs have been observed from detectors placed on ground, inside aircraft and on balloons. In this paper, we present a general purpose Monte‐Carlo model of GRG production and propagation. This model is first compared to a model from Zhou et al. (2016, https://doi.org/10.1016/j.astropartphys.2016.08.004) relying on another Monte‐Carlo framework, and small differences are observed. We then have built an extensive simulation library, made available to the community. This library is used to reproduce five previous gamma‐ray glow observations, from five airborne campaigns: balloons from Eack et al. (1996b, https://doi.org/10.1029/96gl02570), Eack et al. (2000, https://doi.org/10.1029/1999gl010849); and aircrafts from ADELE (Kelley et al., 2015, https://doi.org/10.1038/ncomms8845), ILDAS (Kochkin et al., 2017, https://doi.org/10.1002/2017jd027405) and ALOFT (Østgaard et al., 2019, https://doi.org/10.1029/2019jd030312). Our simulation results confirm that fluxes of cosmic‐ray secondary particles present in the background at a given altitude can be enhanced by several percent (MOS process), and up to several orders of magnitude (RREA process) due to the effect of thunderstorms' electric fields, and explain the five observations. While some GRG could be explained purely by the MOS process, E‐fields significantly larger than Eth are required to explain the strongest GRGs observed. Some of the observations also came with in‐situ electric field measurements, that were always lower than Eth, but may not have been obtained from regions where the glows are produced. This study supports the claim that kilometer‐scale E‐fields magnitudes of at least the level of Eth must be present inside some thunderstorms.
Plain Language Summary
Gamma‐Ray Glows (GRGs) are high‐energy radiation that originates from thunderclouds. These radiations fall within the MeV energy range and last for seconds to minutes. The sources of GRGs are typically extended over a few to tens of square kilometers. In this study, we developed a general‐purpose model to understand the production of GRGs, including the cosmic ray fluxes and enhancement by thunderstorm's electric field, propagation, and instrumental response. Using this model, we were able to reproduce and constrain five previously reported airborne GRG observations, two from balloons, and three from aircraft. The results of our study showed that all of the observations could be explained by one of the two expected regimes: one involving purely particle acceleration (MOS: Modification of Spectrum) and the other involving particle multiplication (RREA: Relativistic Runaway Electron Avalanche). Our simulations suggest that the required large‐scale thunderstorm electric fields, which are compatible with our results, are generally larger than what was previously measured.
Key Points
A general‐purpose Monte‐Carlo model of gamma‐ray glow production is presented
Plausible Gamma‐ray Glow production conditions are provided for five previous airborne observations
Some cases could be explained by the Modification of Spectrum mechanism only while other require electric fields close to Relativistic Runaway Electron Avalanche process threshold, or above</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2022JD037956</doi><tpages>17</tpages><orcidid>https://orcid.org/0000-0001-5721-6783</orcidid><orcidid>https://orcid.org/0000-0002-3471-7267</orcidid><orcidid>https://orcid.org/0000-0002-2572-7033</orcidid><orcidid>https://orcid.org/0000-0002-4000-3789</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | airborne observations Aircraft Balloons Cosmic radiation Cosmic ray showers Cosmic rays Detectors Electric field Electric fields electron Electron avalanche Energy Fluxes gamma ray glow GEANT4 Geophysics High energy astronomy Libraries Meteorological balloons Modelling Particle acceleration positron Propagation Radiation Relativistic particles Simulation thunderstorm Thunderstorms Weather |
title | Library of Simulated Gamma‐Ray Glows and Application to Previous Airborne Observations |
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