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Multispacecraft observations and modeling of the 22/23 June 2015 geomagnetic storm

dc.contributor.authorReiff, P. H.
dc.contributor.authorDaou, A. G.
dc.contributor.authorSazykin, S. Y.
dc.contributor.authorNakamura, R.
dc.contributor.authorHairston, M. R.
dc.contributor.authorCoffey, V.
dc.contributor.authorChandler, M. O.
dc.contributor.authorAnderson, B. J.
dc.contributor.authorRussell, C. T.
dc.contributor.authorWelling, D.
dc.contributor.authorFuselier, S. A.
dc.contributor.authorGenestreti, K. J.
dc.date.accessioned2016-10-17T21:17:28Z
dc.date.available2017-09-06T14:20:20Zen
dc.date.issued2016-07-28
dc.identifier.citationReiff, P. H.; Daou, A. G.; Sazykin, S. Y.; Nakamura, R.; Hairston, M. R.; Coffey, V.; Chandler, M. O.; Anderson, B. J.; Russell, C. T.; Welling, D.; Fuselier, S. A.; Genestreti, K. J. (2016). "Multispacecraft observations and modeling of the 22/23 June 2015 geomagnetic storm." Geophysical Research Letters 43(14): 7311-7318.
dc.identifier.issn0094-8276
dc.identifier.issn1944-8007
dc.identifier.urihttps://hdl.handle.net/2027.42/134114
dc.description.abstractThe magnetic storm of 22–23 June 2015 was one of the largest in the current solar cycle. We present in situ observations from the Magnetospheric Multiscale Mission (MMS) and the Van Allen Probes (VAP) in the magnetotail, field‐aligned currents from AMPERE (Active Magnetosphere and Planetary Electrodynamics Response), and ionospheric flow data from Defense Meteorological Satellite Program (DMSP). Our real‐time space weather alert system sent out a “red alert,” correctly predicting Kp indices greater than 8. We show strong outflow of ionospheric oxygen, dipolarizations in the MMS magnetometer data, and dropouts in the particle fluxes seen by the MMS Fast Plasma Instrument suite. At ionospheric altitudes, the AMPERE data show highly variable currents exceeding 20 MA. We present numerical simulations with the Block Adaptive Tree‐Solarwind ‐ Roe ‐ Upwind Scheme (BATS‐R‐US) global magnetohydrodynamic model linked with the Rice Convection Model. The model predicted the magnitude of the dipolarizations, and varying polar cap convection patterns, which were confirmed by DMSP measurements.Key PointsMHD models can reproduce well the dipolarizations seen at MMS and VAP. Space weather forecasting can predict Kp variations within 0.5 stepBeams of O+ flowing downstream appear to cross the separatrix and become a second energized population of the tail plasma sheetMHD models successfully reproduced the polar cap convection patterns and cross‐polar cap potential drops for a range of IMF conditions
dc.publisherWiley Periodicals, Inc.
dc.subject.otherprediction
dc.subject.othergeomagnetic storm
dc.subject.otherMMS
dc.subject.othersimulation
dc.subject.otherdipolarization
dc.subject.otherspace weather
dc.titleMultispacecraft observations and modeling of the 22/23 June 2015 geomagnetic storm
dc.typeArticleen_US
dc.rights.robotsIndexNoFollow
dc.subject.hlbsecondlevelGeological Sciences
dc.subject.hlbtoplevelScience
dc.description.peerreviewedPeer Reviewed
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/134114/1/grl54522_am.pdf
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/134114/2/grl54522-sup-0002-FigureS1.pdf
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/134114/3/grl54522.pdf
dc.identifier.doi10.1002/2016GL069154
dc.identifier.sourceGeophysical Research Letters
dc.identifier.citedreferenceLiao, J., L. M. Kistler, C. G. Mouikis, B. Klecker, and I. Dandouras ( 2012 ), Solar cycle dependence of the cusp O + access to the near‐Earth magnetotail, J. Geophys. Res., 117, A10220, doi: 10.1029/2012JA017819.
dc.identifier.citedreferenceCrooker, N. U. ( 1992 ), Reverse convection, J. Geophys. Res., 97, 19,363 – 19,372, doi: 10.1029/92JA01532.
dc.identifier.citedreferenceCoxon, J. C., S. E. Milan, L. B. N. Clausen, B. J. Anderson, and H. Korth ( 2014 ), The magnitudes of the regions 1 and 2 Birkeland currents observed by AMPERE and their role in solar wind‐magnetosphere‐ionosphere coupling, J. Geophys. Res. Space Physics, 119, 9804 – 9815, doi: 10.1002/2014JA020138.
dc.identifier.citedreferenceBurch, J. L., T. E. Moore, R. B. Torbert, and B. L. Giles ( 2016 ), Magnetospheric multiscale overview and science objectives, Space Sci. Rev., doi: 10.1007/s11214-015-0164-9.
dc.identifier.citedreferenceBaker, D. N., et al. ( 2016 ), A telescopic and microscopic examination of acceleration in the June 2015 geomagnetic storm: Magnetospheric Multiscale and Van Allen Probes study of substorm particle injection, Geophys. Res. Lett., 43, 6051 – 6059, doi: 10.1002/2016GL069643.
dc.identifier.citedreferenceBala, R., and P. H. Reiff ( 2012 ), Improvements in short‐term of geomagnetic Activity, Space Weather, 10, S06001, doi: 10.1029/2012SW000779.
dc.identifier.citedreferenceBala, R., and P. H. Reiff ( 2014 ), Validating the Rice neural network and the Wing Kp realtime models, Space Weather, 12, 417 – 425, doi: 10.1002/2014SW001075.
dc.identifier.citedreferenceReiff, P. H., and J. L. Burch ( 1985 ), By‐dependent plasma flow and Birkeland currents in the dayside magnetosphere: 2. A global model for southward and northward IMF, J. Geophys. Res., 90, 1595 – 1609, doi: 10.1029/JA090iA02p01595.
dc.identifier.citedreferencePowell, K. G., P. L. Roe, T. J. Linde, T. I. Gombosi, and D. L. De Zeeuw ( 1999 ), A solution‐adaptive upwind scheme for ideal magnetohydrodynamics, J. Comput. Phys., 154, 284 – 309.
dc.identifier.citedreferencePollock, C., et al. ( 2016 ), Fast Plasma Investigation for magnetospheric multiscale, Space Sci. Rev., doi: 10.1007/s11214-016-0245-4.
dc.identifier.citedreferenceSmith, C. W., J. L’Heureux, N. F. Ness, M. H. Acuña, L. F. Burlaga, and J. Scheifele ( 1998 ), The ACE magnetic fields experiment, Space Sci. Rev., 86, 613, doi: 10.1023/A:1005092216668.
dc.identifier.citedreferenceTóth, G., et al. ( 2005 ), Space Weather Modeling Framework: A new tool for the space science community, J. Geophys. Res., 110, A12226, doi: 10.1029/2005JA011126.
dc.identifier.citedreferenceNakamura, R., et al. ( 2016 ), Transient, small‐scale field‐aligned currents in the plasma sheet boundary layer during storm time substorms, Geophys. Res. Lett., 43, 4841 – 4849, doi: 10.1002/2016GL068768.
dc.identifier.citedreferenceMcComas, D. J., S. J. Bame, P. Barker, S. C. Feldman, J. L. Phillips, P. Riley, and J. W. Griffee ( 1998 ), Solar Wind Electron Proton Alpha Monitor (SWEPAM) for the Advanced Composition Explorer, Space Sci. Rev., 86, 613, doi: 10.1023/A:1005040232597.
dc.identifier.citedreferenceLu, G., P. H. Reiff, T. E. Moore, and R. A. Heelis ( 1992 ), Upflowing ionospheric ions in the auroral region, J. Geophys. Res., 97, 16,855 – 16,863, doi: 10.1029/92JA01435.
dc.identifier.citedreferenceLiao, J., L. M. Kistler, C. G. Mouikis, B. Klecker, I. Dandouras, and J.‐C. Zhang ( 2010 ), Statistical study of O + transport from the cusp to the lobes with Cluster CODIF data, J. Geophys. Res., 115, A00J15, doi: 10.1029/2010JA015613.
dc.identifier.citedreferenceYoung, D. T., et al. ( 2016 ), Hot plasma composition analyzer for the magnetospheric multiscale mission, Space Sci. Rev., doi: 10.1007/s11214-014-0119-6.
dc.identifier.citedreferenceTóth, G., et al. ( 2012 ), Adaptive numerical algorithms in space weather modeling, J. Comput. Phys., 231, 870 – 903, doi: 10.1016/j.jcp.2011.02.006.
dc.identifier.citedreferenceRussell, C. T., et al. ( 2016 ), The magnetospheric multiscale magnetometers, Space Sci. Rev., doi: 10.1007/s11214-014-0057-3.
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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