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Dynamic Characterization of Equatorial Plasma Bubble Based on Triangle Network‐Joint Slope Approach

This paper introduces a Triangle Network‐Joint Slope (TN‐JS) approach to characterize the spatial and temporal dynamics of Equatorial Plasma Bubbles (EPBs) during geomagnetic storms. To collaboratively determine the EPB drift directions from multiple stations, a Delaunay triangle network is construc...

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Published in:Journal of geophysical research. Space physics 2024-08, Vol.129 (8), p.n/a
Main Authors: Miao, Xirui, Yang, Rong, Fu, Naifeng, Zhan, Xingqun, Morton, Y. Jade
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Yang, Rong
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Morton, Y. Jade
description This paper introduces a Triangle Network‐Joint Slope (TN‐JS) approach to characterize the spatial and temporal dynamics of Equatorial Plasma Bubbles (EPBs) during geomagnetic storms. To collaboratively determine the EPB drift directions from multiple stations, a Delaunay triangle network is constructed, utilizing the distribution of Ionospheric Piercing Points (IPPs). The Time Difference of Arrival (TDOA) is extracted through cross‐correlating the Rate of Total Electron Content (ROT). The EPB drift direction can be approximately calculated by considering TDOA and IPP distances within each individual triangle of the network. This calculation is then refined through a joint statistical analysis. Using a reference station as the origin, the remaining stations within the network are projected along the estimated EPB drift direction. A spatial‐temporal color map illustrating regional ionospheric anomaly ROT observations is constructed. The EPB drift velocity among multiple stations can be collectively estimated by fitting the slope of this map, facilitating outlier exclusion. Accounting for satellite dynamic effects and the diverse orbit characteristics of GPS and BDS, corresponding IPP scan velocity compensation is performed and analyzed for EPB dynamic estimation. Using the geomagnetic storm event that occurred on September 8 as a case study, the spatial‐temporal kinetic properties of EPBs is characterized by analyzing Global Navigation Satellite System (GNSS) observations from 17 Hong Kong monitoring stations with the proposed TN‐JS approach. The results indicate during this magnetic event, that EPBs exhibit a westward drift trend with velocities ranging from a few tens to hundreds of meters per second in GPS and BDS observations. Plain Language Summary Total Electron Content (TEC) is a path integrated electron density and its rate (ROT) of change reflect the ionospheric disturbance during magnetic storms. This article introduces a new method called Triangle Network‐Joint Slope (TN‐JS) to study the movement of Equatorial Plasma Bubbles (EPBs). TN‐JS uses a network of GNSS monitoring stations to determine the drift velocity of EPBs. By resampling ROT correlation using triangulation along the drift direction, TN‐JS transforms traditional EPB dynamic estimation into image processing of the color‐coded ROT maps. The TN‐JS algorithm is tested with data collected from 17 monitoring stations around Hong Kong during a geomagnetic storm on 8 September 2017 to show EP
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Jade</creator><creatorcontrib>Miao, Xirui ; Yang, Rong ; Fu, Naifeng ; Zhan, Xingqun ; Morton, Y. Jade</creatorcontrib><description>This paper introduces a Triangle Network‐Joint Slope (TN‐JS) approach to characterize the spatial and temporal dynamics of Equatorial Plasma Bubbles (EPBs) during geomagnetic storms. To collaboratively determine the EPB drift directions from multiple stations, a Delaunay triangle network is constructed, utilizing the distribution of Ionospheric Piercing Points (IPPs). The Time Difference of Arrival (TDOA) is extracted through cross‐correlating the Rate of Total Electron Content (ROT). The EPB drift direction can be approximately calculated by considering TDOA and IPP distances within each individual triangle of the network. This calculation is then refined through a joint statistical analysis. Using a reference station as the origin, the remaining stations within the network are projected along the estimated EPB drift direction. A spatial‐temporal color map illustrating regional ionospheric anomaly ROT observations is constructed. The EPB drift velocity among multiple stations can be collectively estimated by fitting the slope of this map, facilitating outlier exclusion. Accounting for satellite dynamic effects and the diverse orbit characteristics of GPS and BDS, corresponding IPP scan velocity compensation is performed and analyzed for EPB dynamic estimation. Using the geomagnetic storm event that occurred on September 8 as a case study, the spatial‐temporal kinetic properties of EPBs is characterized by analyzing Global Navigation Satellite System (GNSS) observations from 17 Hong Kong monitoring stations with the proposed TN‐JS approach. The results indicate during this magnetic event, that EPBs exhibit a westward drift trend with velocities ranging from a few tens to hundreds of meters per second in GPS and BDS observations. Plain Language Summary Total Electron Content (TEC) is a path integrated electron density and its rate (ROT) of change reflect the ionospheric disturbance during magnetic storms. This article introduces a new method called Triangle Network‐Joint Slope (TN‐JS) to study the movement of Equatorial Plasma Bubbles (EPBs). TN‐JS uses a network of GNSS monitoring stations to determine the drift velocity of EPBs. By resampling ROT correlation using triangulation along the drift direction, TN‐JS transforms traditional EPB dynamic estimation into image processing of the color‐coded ROT maps. The TN‐JS algorithm is tested with data collected from 17 monitoring stations around Hong Kong during a geomagnetic storm on 8 September 2017 to show EPBs drifting westward at speeds ranging from tens to hundreds of meters per second. Key Points A Delauny Triangle Network is built for statistically inferring EPB drift velocity by cross‐correlating and slope fitting multi‐sites' ROT The orbit diversity offered by GPS MEO and BDS GEO/IGSO satellites provides measures of ionospheric irregularities inhomogeneity The analysis unveiled a significant EPB westward drift event with a speed exceeding 500 m/s during the 2017 geomagnetic storm over Hong Kong</description><identifier>ISSN: 2169-9380</identifier><identifier>EISSN: 2169-9402</identifier><identifier>DOI: 10.1029/2024JA032912</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Algorithms ; Bubbles ; Color ; Data analysis ; Drift estimation ; drift velocity ; Electron density ; equatorial plasma bubble(EPB) ; Geomagnetic storms ; Geomagnetism ; Global navigation satellite system ; Global positioning systems ; GPS ; Image processing ; Ionospheric disturbances ; Magnetic properties ; Magnetic storms ; Monitoring ; Navigation satellites ; Navigation systems ; Outliers (statistics) ; Plasma bubbles ; Resampling ; ROT ; Satellite navigation systems ; Satellite observation ; Satellites ; Slopes ; Statistical analysis ; Storms ; time difference of arrival (TDOA) ; Total Electron Content ; triangle network‐joint slope (TN‐JS) ; Triangulation</subject><ispartof>Journal of geophysical research. Space physics, 2024-08, Vol.129 (8), p.n/a</ispartof><rights>2024. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c2323-9277f2e5dbb74bb2fc0adb0c0d76f4497a1e960f6d38996254864fd69454939e3</cites><orcidid>0000-0002-7655-067X ; 0000-0003-1533-8701 ; 0000-0001-9173-2888</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Miao, Xirui</creatorcontrib><creatorcontrib>Yang, Rong</creatorcontrib><creatorcontrib>Fu, Naifeng</creatorcontrib><creatorcontrib>Zhan, Xingqun</creatorcontrib><creatorcontrib>Morton, Y. Jade</creatorcontrib><title>Dynamic Characterization of Equatorial Plasma Bubble Based on Triangle Network‐Joint Slope Approach</title><title>Journal of geophysical research. Space physics</title><description>This paper introduces a Triangle Network‐Joint Slope (TN‐JS) approach to characterize the spatial and temporal dynamics of Equatorial Plasma Bubbles (EPBs) during geomagnetic storms. To collaboratively determine the EPB drift directions from multiple stations, a Delaunay triangle network is constructed, utilizing the distribution of Ionospheric Piercing Points (IPPs). The Time Difference of Arrival (TDOA) is extracted through cross‐correlating the Rate of Total Electron Content (ROT). The EPB drift direction can be approximately calculated by considering TDOA and IPP distances within each individual triangle of the network. This calculation is then refined through a joint statistical analysis. Using a reference station as the origin, the remaining stations within the network are projected along the estimated EPB drift direction. A spatial‐temporal color map illustrating regional ionospheric anomaly ROT observations is constructed. The EPB drift velocity among multiple stations can be collectively estimated by fitting the slope of this map, facilitating outlier exclusion. Accounting for satellite dynamic effects and the diverse orbit characteristics of GPS and BDS, corresponding IPP scan velocity compensation is performed and analyzed for EPB dynamic estimation. Using the geomagnetic storm event that occurred on September 8 as a case study, the spatial‐temporal kinetic properties of EPBs is characterized by analyzing Global Navigation Satellite System (GNSS) observations from 17 Hong Kong monitoring stations with the proposed TN‐JS approach. The results indicate during this magnetic event, that EPBs exhibit a westward drift trend with velocities ranging from a few tens to hundreds of meters per second in GPS and BDS observations. Plain Language Summary Total Electron Content (TEC) is a path integrated electron density and its rate (ROT) of change reflect the ionospheric disturbance during magnetic storms. This article introduces a new method called Triangle Network‐Joint Slope (TN‐JS) to study the movement of Equatorial Plasma Bubbles (EPBs). TN‐JS uses a network of GNSS monitoring stations to determine the drift velocity of EPBs. By resampling ROT correlation using triangulation along the drift direction, TN‐JS transforms traditional EPB dynamic estimation into image processing of the color‐coded ROT maps. The TN‐JS algorithm is tested with data collected from 17 monitoring stations around Hong Kong during a geomagnetic storm on 8 September 2017 to show EPBs drifting westward at speeds ranging from tens to hundreds of meters per second. Key Points A Delauny Triangle Network is built for statistically inferring EPB drift velocity by cross‐correlating and slope fitting multi‐sites' ROT The orbit diversity offered by GPS MEO and BDS GEO/IGSO satellites provides measures of ionospheric irregularities inhomogeneity The analysis unveiled a significant EPB westward drift event with a speed exceeding 500 m/s during the 2017 geomagnetic storm over Hong Kong</description><subject>Algorithms</subject><subject>Bubbles</subject><subject>Color</subject><subject>Data analysis</subject><subject>Drift estimation</subject><subject>drift velocity</subject><subject>Electron density</subject><subject>equatorial plasma bubble(EPB)</subject><subject>Geomagnetic storms</subject><subject>Geomagnetism</subject><subject>Global navigation satellite system</subject><subject>Global positioning systems</subject><subject>GPS</subject><subject>Image processing</subject><subject>Ionospheric disturbances</subject><subject>Magnetic properties</subject><subject>Magnetic storms</subject><subject>Monitoring</subject><subject>Navigation satellites</subject><subject>Navigation systems</subject><subject>Outliers (statistics)</subject><subject>Plasma bubbles</subject><subject>Resampling</subject><subject>ROT</subject><subject>Satellite navigation systems</subject><subject>Satellite observation</subject><subject>Satellites</subject><subject>Slopes</subject><subject>Statistical analysis</subject><subject>Storms</subject><subject>time difference of arrival (TDOA)</subject><subject>Total Electron Content</subject><subject>triangle network‐joint slope (TN‐JS)</subject><subject>Triangulation</subject><issn>2169-9380</issn><issn>2169-9402</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp9kE1OwzAQhS0EElXpjgNYYkvA8V_iZVpKoaoAQVlHTmLTlDRO7URVWHEEzshJMCpIrJjNjN77NE96AJyG6CJEWFxihOk8QQSLEB-AAQ65CARF-PD3JjE6BiPn1shP7KWQDYC66mu5KXM4WUkr81bZ8k22pamh0XC67WRrbCkr-FBJt5Fw3GVZpeBYOlVADy29Wb945U61O2NfP98_5qasW_hUmUbBpGmskfnqBBxpWTk1-tlD8Hw9XU5ugsX97HaSLIIcE0wCgaNIY8WKLItolmGdI1lkKEdFxDWlIpKhEhxpXpBYCI4ZjTnVBReUUUGEIkNwtv_rY7edcm26Np2tfWRKkIgoY4JFnjrfU7k1zlml08aWG2n7NETpd5fp3y49Tvb4rqxU_y-bzmePCYs5IuQLz9N1aQ</recordid><startdate>202408</startdate><enddate>202408</enddate><creator>Miao, Xirui</creator><creator>Yang, Rong</creator><creator>Fu, Naifeng</creator><creator>Zhan, Xingqun</creator><creator>Morton, Y. 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Space physics</jtitle><date>2024-08</date><risdate>2024</risdate><volume>129</volume><issue>8</issue><epage>n/a</epage><issn>2169-9380</issn><eissn>2169-9402</eissn><abstract>This paper introduces a Triangle Network‐Joint Slope (TN‐JS) approach to characterize the spatial and temporal dynamics of Equatorial Plasma Bubbles (EPBs) during geomagnetic storms. To collaboratively determine the EPB drift directions from multiple stations, a Delaunay triangle network is constructed, utilizing the distribution of Ionospheric Piercing Points (IPPs). The Time Difference of Arrival (TDOA) is extracted through cross‐correlating the Rate of Total Electron Content (ROT). The EPB drift direction can be approximately calculated by considering TDOA and IPP distances within each individual triangle of the network. This calculation is then refined through a joint statistical analysis. Using a reference station as the origin, the remaining stations within the network are projected along the estimated EPB drift direction. A spatial‐temporal color map illustrating regional ionospheric anomaly ROT observations is constructed. The EPB drift velocity among multiple stations can be collectively estimated by fitting the slope of this map, facilitating outlier exclusion. Accounting for satellite dynamic effects and the diverse orbit characteristics of GPS and BDS, corresponding IPP scan velocity compensation is performed and analyzed for EPB dynamic estimation. Using the geomagnetic storm event that occurred on September 8 as a case study, the spatial‐temporal kinetic properties of EPBs is characterized by analyzing Global Navigation Satellite System (GNSS) observations from 17 Hong Kong monitoring stations with the proposed TN‐JS approach. The results indicate during this magnetic event, that EPBs exhibit a westward drift trend with velocities ranging from a few tens to hundreds of meters per second in GPS and BDS observations. Plain Language Summary Total Electron Content (TEC) is a path integrated electron density and its rate (ROT) of change reflect the ionospheric disturbance during magnetic storms. This article introduces a new method called Triangle Network‐Joint Slope (TN‐JS) to study the movement of Equatorial Plasma Bubbles (EPBs). TN‐JS uses a network of GNSS monitoring stations to determine the drift velocity of EPBs. By resampling ROT correlation using triangulation along the drift direction, TN‐JS transforms traditional EPB dynamic estimation into image processing of the color‐coded ROT maps. The TN‐JS algorithm is tested with data collected from 17 monitoring stations around Hong Kong during a geomagnetic storm on 8 September 2017 to show EPBs drifting westward at speeds ranging from tens to hundreds of meters per second. Key Points A Delauny Triangle Network is built for statistically inferring EPB drift velocity by cross‐correlating and slope fitting multi‐sites' ROT The orbit diversity offered by GPS MEO and BDS GEO/IGSO satellites provides measures of ionospheric irregularities inhomogeneity The analysis unveiled a significant EPB westward drift event with a speed exceeding 500 m/s during the 2017 geomagnetic storm over Hong Kong</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2024JA032912</doi><tpages>19</tpages><orcidid>https://orcid.org/0000-0002-7655-067X</orcidid><orcidid>https://orcid.org/0000-0003-1533-8701</orcidid><orcidid>https://orcid.org/0000-0001-9173-2888</orcidid><oa>free_for_read</oa></addata></record>
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ispartof Journal of geophysical research. Space physics, 2024-08, Vol.129 (8), p.n/a
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subjects Algorithms
Bubbles
Color
Data analysis
Drift estimation
drift velocity
Electron density
equatorial plasma bubble(EPB)
Geomagnetic storms
Geomagnetism
Global navigation satellite system
Global positioning systems
GPS
Image processing
Ionospheric disturbances
Magnetic properties
Magnetic storms
Monitoring
Navigation satellites
Navigation systems
Outliers (statistics)
Plasma bubbles
Resampling
ROT
Satellite navigation systems
Satellite observation
Satellites
Slopes
Statistical analysis
Storms
time difference of arrival (TDOA)
Total Electron Content
triangle network‐joint slope (TN‐JS)
Triangulation
title Dynamic Characterization of Equatorial Plasma Bubble Based on Triangle Network‐Joint Slope Approach
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