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...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of geophysical research. Atmospheres 2023-05, Vol.128 (9), p.n/a
Hauptverfasser: Sarria, D., Østgaard, N., Marisaldi, M., Lehtinen, N., Mezentsev, A.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page n/a
container_issue 9
container_start_page
container_title Journal of geophysical research. Atmospheres
container_volume 128
creator Sarria, D.
Østgaard, N.
Marisaldi, M.
Lehtinen, N.
Mezentsev, A.
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
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2811437727</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2811437727</sourcerecordid><originalsourceid>FETCH-LOGICAL-c2960-5770290867697545e37779a2c90908dfbe2cc8144f2a9841d11cb58f00124303</originalsourceid><addsrcrecordid>eNp9kE1OwzAQhS0EElXpjgNYYkvAdhz_LKsWAlUlUOmiu8hJHMlVEgc7adUdR-CMnARDEWLFbGY0-vTmzQPgEqMbjIi8JYiQxRzFXCbsBIwIZjISUrLT35lvzsHE-y0KJVBMEzoCm6XJnXIHaCv4YpqhVr0uYaqaRn28va_UAaa13Xuo2hJOu642heqNbWFv4bPTO2MHD6fG5da1Gj7lXrvdN-AvwFmlaq8nP30M1vd369lDtHxKH2fTZVQQyVCUcB7MI8E4kzyhiY4551KRQqKwLatck6IQmNKKKCkoLjEu8kRUCGFCYxSPwdVRtnP2ddC-z7Z2cG24mBGBMQ1yhAfq-kgVznrvdJV1zjTh7Qyj7Cu97G96AY-P-N7U-vAvmy3S1TwRjKH4EwG5b40</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2811437727</pqid></control><display><type>article</type><title>Library of Simulated Gamma‐Ray Glows and Application to Previous Airborne Observations</title><source>Access via Wiley Online Library</source><source>Alma/SFX Local Collection</source><creator>Sarria, D. ; Østgaard, N. ; Marisaldi, M. ; Lehtinen, N. ; Mezentsev, A.</creator><creatorcontrib>Sarria, D. ; Østgaard, N. ; Marisaldi, M. ; Lehtinen, N. ; Mezentsev, A.</creatorcontrib><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><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 &amp; 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 &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; 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>
fulltext fulltext
identifier ISSN: 2169-897X
ispartof Journal of geophysical research. Atmospheres, 2023-05, Vol.128 (9), p.n/a
issn 2169-897X
2169-8996
language eng
recordid cdi_proquest_journals_2811437727
source Access via Wiley Online Library; Alma/SFX Local Collection
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
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-19T14%3A44%3A04IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Library%20of%20Simulated%20Gamma%E2%80%90Ray%20Glows%20and%20Application%20to%20Previous%20Airborne%20Observations&rft.jtitle=Journal%20of%20geophysical%20research.%20Atmospheres&rft.au=Sarria,%20D.&rft.date=2023-05-16&rft.volume=128&rft.issue=9&rft.epage=n/a&rft.issn=2169-897X&rft.eissn=2169-8996&rft_id=info:doi/10.1029/2022JD037956&rft_dat=%3Cproquest_cross%3E2811437727%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2811437727&rft_id=info:pmid/&rfr_iscdi=true