The March 2015 Superstorm Revisited: Phase Space Density Profiles and Fast ULF Wave Diffusive Transport

We present the temporal evolution of electron Phase Space Density (PSD) in the outer radiation belt during the intense March 2015 geomagnetic storm. Comparing observed PSD profiles as a function of L* at fixed first, M, and second, K, adiabatic invariants with those produced by simulations is critic...

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Veröffentlicht in:Journal of geophysical research. Space physics 2019-02, Vol.124 (2), p.1143-1156
Hauptverfasser: Ozeke, L. G., Mann, I. R., Claudepierre, S. G., Henderson, M., Morley, S. K., Murphy, K. R., Olifer, L., Spence, H. E., Baker, D. N.
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container_title Journal of geophysical research. Space physics
container_volume 124
creator Ozeke, L. G.
Mann, I. R.
Claudepierre, S. G.
Henderson, M.
Morley, S. K.
Murphy, K. R.
Olifer, L.
Spence, H. E.
Baker, D. N.
description We present the temporal evolution of electron Phase Space Density (PSD) in the outer radiation belt during the intense March 2015 geomagnetic storm. Comparing observed PSD profiles as a function of L* at fixed first, M, and second, K, adiabatic invariants with those produced by simulations is critical for determining the physical processes responsible for the outer radiation belt dynamics. Here we show that the bulk of the accelerated and enhanced outer radiation belt population consists of electrons with K 
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G. ; Mann, I. R. ; Claudepierre, S. G. ; Henderson, M. ; Morley, S. K. ; Murphy, K. R. ; Olifer, L. ; Spence, H. E. ; Baker, D. N.</creator><creatorcontrib>Ozeke, L. G. ; Mann, I. R. ; Claudepierre, S. G. ; Henderson, M. ; Morley, S. K. ; Murphy, K. R. ; Olifer, L. ; Spence, H. E. ; Baker, D. N.</creatorcontrib><description>We present the temporal evolution of electron Phase Space Density (PSD) in the outer radiation belt during the intense March 2015 geomagnetic storm. Comparing observed PSD profiles as a function of L* at fixed first, M, and second, K, adiabatic invariants with those produced by simulations is critical for determining the physical processes responsible for the outer radiation belt dynamics. Here we show that the bulk of the accelerated and enhanced outer radiation belt population consists of electrons with K &lt; 0.17 G1/2Re. For these electrons, the observed PSD versus L* profiles during the recovery phase of the storm have a positive radial gradient. We compare the observed temporal evolution of the PSD profiles during the recovery phase with those produced by radial diffusion simulations driven by observed Ultralow Frequency wave power as measured on the ground. Our results indicate that the dominant flux enhancement, inside L* &lt; 5, in the heart of the outer radiation belt during the March 2015 geomagnetic storm is consistent with that produced by fast inward radial diffusion of electrons from a dynamic outer boundary driven by enhanced Ultralow Frequency wave power. Key Points The March 2015 outer radiation belt flux enhancement was dominated by a population of accelerated low‐K electrons with K &lt; 0.17 G1/2Re During the flux recovery phase no growing PSD peaks occurred inside L*≲5, suggesting local heating was not the dominant acceleration process The observed flux enhancement inside L* &lt; 5 is reproduced by our ULF wave radial diffusion simulation without including local acceleration</description><identifier>ISSN: 2169-9380</identifier><identifier>EISSN: 2169-9402</identifier><identifier>DOI: 10.1029/2018JA026326</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Diffusion ; Diffusion rate ; Electrons ; Evolution ; Extremely low frequencies ; Geomagnetic storms ; Geomagnetism ; local acceleration ; Magnetic storms ; March 2015 storm ; Outer radiation belt ; phase space density ; radial diffusion ; Radiation ; radiation belt ; Recovery ; Space density ; Storms ; ULF waves ; Wave power</subject><ispartof>Journal of geophysical research. 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Here we show that the bulk of the accelerated and enhanced outer radiation belt population consists of electrons with K &lt; 0.17 G1/2Re. For these electrons, the observed PSD versus L* profiles during the recovery phase of the storm have a positive radial gradient. We compare the observed temporal evolution of the PSD profiles during the recovery phase with those produced by radial diffusion simulations driven by observed Ultralow Frequency wave power as measured on the ground. Our results indicate that the dominant flux enhancement, inside L* &lt; 5, in the heart of the outer radiation belt during the March 2015 geomagnetic storm is consistent with that produced by fast inward radial diffusion of electrons from a dynamic outer boundary driven by enhanced Ultralow Frequency wave power. Key Points The March 2015 outer radiation belt flux enhancement was dominated by a population of accelerated low‐K electrons with K &lt; 0.17 G1/2Re During the flux recovery phase no growing PSD peaks occurred inside L*≲5, suggesting local heating was not the dominant acceleration process The observed flux enhancement inside L* &lt; 5 is reproduced by our ULF wave radial diffusion simulation without including local acceleration</description><subject>Diffusion</subject><subject>Diffusion rate</subject><subject>Electrons</subject><subject>Evolution</subject><subject>Extremely low frequencies</subject><subject>Geomagnetic storms</subject><subject>Geomagnetism</subject><subject>local acceleration</subject><subject>Magnetic storms</subject><subject>March 2015 storm</subject><subject>Outer radiation belt</subject><subject>phase space density</subject><subject>radial diffusion</subject><subject>Radiation</subject><subject>radiation belt</subject><subject>Recovery</subject><subject>Space density</subject><subject>Storms</subject><subject>ULF waves</subject><subject>Wave power</subject><issn>2169-9380</issn><issn>2169-9402</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp9kEtLAzEUhYMoWLQ7f0DAraN5z8RdqbZaKpY-cBkyk8ROaWfGZKbSf2-kCq68m3s4fJzLPQBcYXSLEZF3BOFsMkBEUCJOQI9gIRPJEDn91TRD56AfwgbFyaKFeQ-8L9cWvmhfrGEM4HDRNdaHtvY7OLf7MpStNfdwttbBwkWjCwsfbBXdA5z52pVbG6CuDBzp0MLVdATf9D4ipXNdKKNael2FpvbtJThzehts_2dfgNXocTl8Sqav4-fhYJoUNKUokUTn1DCSYyOFQalLcSYLJnJknWSMFs5EzEktMTW5c4Q44YTBjGNJNdb0Alwfcxtff3Q2tGpTd76KJxXBkvNMSJ5F6uZIFb4OwVunGl_utD8ojNR3m-pvmxGnR_wzPnz4l1WT8XzAWcoR_QITz3QT</recordid><startdate>201902</startdate><enddate>201902</enddate><creator>Ozeke, L. 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G.</au><au>Henderson, M.</au><au>Morley, S. K.</au><au>Murphy, K. R.</au><au>Olifer, L.</au><au>Spence, H. E.</au><au>Baker, D. N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The March 2015 Superstorm Revisited: Phase Space Density Profiles and Fast ULF Wave Diffusive Transport</atitle><jtitle>Journal of geophysical research. Space physics</jtitle><date>2019-02</date><risdate>2019</risdate><volume>124</volume><issue>2</issue><spage>1143</spage><epage>1156</epage><pages>1143-1156</pages><issn>2169-9380</issn><eissn>2169-9402</eissn><abstract>We present the temporal evolution of electron Phase Space Density (PSD) in the outer radiation belt during the intense March 2015 geomagnetic storm. Comparing observed PSD profiles as a function of L* at fixed first, M, and second, K, adiabatic invariants with those produced by simulations is critical for determining the physical processes responsible for the outer radiation belt dynamics. Here we show that the bulk of the accelerated and enhanced outer radiation belt population consists of electrons with K &lt; 0.17 G1/2Re. For these electrons, the observed PSD versus L* profiles during the recovery phase of the storm have a positive radial gradient. We compare the observed temporal evolution of the PSD profiles during the recovery phase with those produced by radial diffusion simulations driven by observed Ultralow Frequency wave power as measured on the ground. Our results indicate that the dominant flux enhancement, inside L* &lt; 5, in the heart of the outer radiation belt during the March 2015 geomagnetic storm is consistent with that produced by fast inward radial diffusion of electrons from a dynamic outer boundary driven by enhanced Ultralow Frequency wave power. Key Points The March 2015 outer radiation belt flux enhancement was dominated by a population of accelerated low‐K electrons with K &lt; 0.17 G1/2Re During the flux recovery phase no growing PSD peaks occurred inside L*≲5, suggesting local heating was not the dominant acceleration process The observed flux enhancement inside L* &lt; 5 is reproduced by our ULF wave radial diffusion simulation without including local acceleration</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2018JA026326</doi><tpages>14</tpages><orcidid>https://orcid.org/0000-0001-8520-0199</orcidid><orcidid>https://orcid.org/0000-0003-1004-7841</orcidid><orcidid>https://orcid.org/0000-0002-6479-2778</orcidid><orcidid>https://orcid.org/0000-0002-2526-2205</orcidid><orcidid>https://orcid.org/0000-0002-5917-7113</orcidid><orcidid>https://orcid.org/0000-0001-5513-5947</orcidid><orcidid>https://orcid.org/0000-0003-4975-9029</orcidid><orcidid>https://orcid.org/0000-0002-3063-6451</orcidid><orcidid>https://orcid.org/0000-0001-5909-0926</orcidid></addata></record>
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subjects Diffusion
Diffusion rate
Electrons
Evolution
Extremely low frequencies
Geomagnetic storms
Geomagnetism
local acceleration
Magnetic storms
March 2015 storm
Outer radiation belt
phase space density
radial diffusion
Radiation
radiation belt
Recovery
Space density
Storms
ULF waves
Wave power
title The March 2015 Superstorm Revisited: Phase Space Density Profiles and Fast ULF Wave Diffusive Transport
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