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Gamma Ray Glow Observations at 20‐km Altitude.

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Title: Gamma Ray Glow Observations at 20‐km Altitude.
Authors: Østgaard, N.1, Sarria, D.1, Mezentsev, A.1, Kochkin, P.1, Lehtinen, N.1, Genov, G.1, Ullaland, K.1, Marisaldi, M.1, Yang, S.1, Christian, H. J.2, Grove, J. E.3, Wulf, E.3, Quick, M.4, Blakeslee, R. J.4, Al‐Nussirat, S.5
Source: Journal of Geophysical Research. Atmospheres. 7/16/2019, Vol. 124 Issue 13, p7236-7254. 19p.
Subject Terms: *Clouds, *Thunderstorms, Gamma rays, Atmospheric electricity
Geographic Terms: Georgia
Abstract: In the spring of 2017 an ER‐2 aircraft campaign was undertaken over continental United States to observe energetic radiation from thunderstorms and lightning. The payload consisted of a suite of instruments designed to detect optical signals, electric fields, and gamma rays from lightning. Starting from Georgia, USA, 16 flights were performed, for a total of about 70 flight hours at a cruise altitude of 20 km. Of these, 45 flight hours were over thunderstorm regions. An analysis of two gamma ray glow events that were observed over Colorado at 21:47 UT on 8 May 2017 is presented. We explore the charge structure of the cloud system, as well as possible mechanisms that can produce the gamma ray glows. The thundercloud system we passed during the gamma ray glow observation had strong convection in the core of the cloud system. Electric field measurements combined with radar and radio measurements suggest an inverted charge structure, with an upper negative charge layer and a lower positive charge layer. Based on modeling results, we were not able to unambiguously determine the production mechanism. Possible mechanisms are either an enhancement of cosmic background locally (above or below 20 km) by an electric field below the local threshold or an enhancement of the cosmic background inside the cloud but then with normal polarity and an electric field well above the Relativistic Runaway Electron Avalanche threshold. Key Points: Gamma ray glows were observed for the first time at 20‐km altitude above thundercloudsThe thunderclouds below the aircraft had an anomalous charge structurePossible production mechanisms for gamma ray glow are tested by Monte Carlo modeling [ABSTRACT FROM AUTHOR]
Copyright of Journal of Geophysical Research. Atmospheres is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: Gamma Ray Glow Observations at 20‐km Altitude.
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  Data: <searchLink fieldCode="AR" term="%22Østgaard%2C+N%2E%22">Østgaard, N.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Sarria%2C+D%2E%22">Sarria, D.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Mezentsev%2C+A%2E%22">Mezentsev, A.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Kochkin%2C+P%2E%22">Kochkin, P.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Lehtinen%2C+N%2E%22">Lehtinen, N.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Genov%2C+G%2E%22">Genov, G.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Ullaland%2C+K%2E%22">Ullaland, K.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Marisaldi%2C+M%2E%22">Marisaldi, M.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Yang%2C+S%2E%22">Yang, S.</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Christian%2C+H%2E+J%2E%22">Christian, H. J.</searchLink><relatesTo>2</relatesTo><br /><searchLink fieldCode="AR" term="%22Grove%2C+J%2E+E%2E%22">Grove, J. E.</searchLink><relatesTo>3</relatesTo><br /><searchLink fieldCode="AR" term="%22Wulf%2C+E%2E%22">Wulf, E.</searchLink><relatesTo>3</relatesTo><br /><searchLink fieldCode="AR" term="%22Quick%2C+M%2E%22">Quick, M.</searchLink><relatesTo>4</relatesTo><br /><searchLink fieldCode="AR" term="%22Blakeslee%2C+R%2E+J%2E%22">Blakeslee, R. J.</searchLink><relatesTo>4</relatesTo><br /><searchLink fieldCode="AR" term="%22Al‐Nussirat%2C+S%2E%22">Al‐Nussirat, S.</searchLink><relatesTo>5</relatesTo>
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  Data: <searchLink fieldCode="JN" term="%22Journal+of+Geophysical+Research%2E+Atmospheres%22">Journal of Geophysical Research. Atmospheres</searchLink>. 7/16/2019, Vol. 124 Issue 13, p7236-7254. 19p.
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  Data: *<searchLink fieldCode="DE" term="%22Clouds%22">Clouds</searchLink><br />*<searchLink fieldCode="DE" term="%22Thunderstorms%22">Thunderstorms</searchLink><br /><searchLink fieldCode="DE" term="%22Gamma+rays%22">Gamma rays</searchLink><br /><searchLink fieldCode="DE" term="%22Atmospheric+electricity%22">Atmospheric electricity</searchLink>
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  Data: <searchLink fieldCode="DE" term="%22Georgia%22">Georgia</searchLink>
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  Data: In the spring of 2017 an ER‐2 aircraft campaign was undertaken over continental United States to observe energetic radiation from thunderstorms and lightning. The payload consisted of a suite of instruments designed to detect optical signals, electric fields, and gamma rays from lightning. Starting from Georgia, USA, 16 flights were performed, for a total of about 70 flight hours at a cruise altitude of 20 km. Of these, 45 flight hours were over thunderstorm regions. An analysis of two gamma ray glow events that were observed over Colorado at 21:47 UT on 8 May 2017 is presented. We explore the charge structure of the cloud system, as well as possible mechanisms that can produce the gamma ray glows. The thundercloud system we passed during the gamma ray glow observation had strong convection in the core of the cloud system. Electric field measurements combined with radar and radio measurements suggest an inverted charge structure, with an upper negative charge layer and a lower positive charge layer. Based on modeling results, we were not able to unambiguously determine the production mechanism. Possible mechanisms are either an enhancement of cosmic background locally (above or below 20 km) by an electric field below the local threshold or an enhancement of the cosmic background inside the cloud but then with normal polarity and an electric field well above the Relativistic Runaway Electron Avalanche threshold. Key Points: Gamma ray glows were observed for the first time at 20‐km altitude above thundercloudsThe thunderclouds below the aircraft had an anomalous charge structurePossible production mechanisms for gamma ray glow are tested by Monte Carlo modeling [ABSTRACT FROM AUTHOR]
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  Data: <i>Copyright of Journal of Geophysical Research. Atmospheres is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
PLink https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&db=8gh&AN=137720644
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        Value: 10.1029/2019JD030312
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        Text: English
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        PageCount: 19
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      – SubjectFull: Clouds
        Type: general
      – SubjectFull: Thunderstorms
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      – SubjectFull: Gamma rays
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      – SubjectFull: Atmospheric electricity
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      – SubjectFull: Georgia
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      – TitleFull: Gamma Ray Glow Observations at 20‐km Altitude.
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              Text: 7/16/2019
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