2016
DOI: 10.1051/swsc/2015041
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Ionosphere-thermosphere (IT) response to solar wind forcing during magnetic storms

Abstract: During magnetic storms, there is a strong response in the ionosphere and thermosphere which occurs at polar latitudes. Energy input in the form of Poynting flux and energetic particle precipitation, and energy output in the form of heated ions and neutrals have been detected at different altitudes and all local times. We have analyzed a number of storms, using satellite data from the Defense Meteorological Satellite Program (DMSP), the Gravity Recovery and Climate Experiment (GRACE), Gravity field and steady-s… Show more

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Cited by 26 publications
(45 citation statements)
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“…The role of energy deposition during geomagnetic storms has recently been studied using satellite observations of electromagnetic and neutral density perturbations (Huang et al 2014(Huang et al , 2016. Energy deposition in the polar cap, versus auroral latitudes, is found to be a significant and possibly dominant phenomenon during storms, with major implications for global thermosphere circulation patterns and the evolution of ionospheric storms.…”
Section: Discussionmentioning
confidence: 99%
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“…The role of energy deposition during geomagnetic storms has recently been studied using satellite observations of electromagnetic and neutral density perturbations (Huang et al 2014(Huang et al , 2016. Energy deposition in the polar cap, versus auroral latitudes, is found to be a significant and possibly dominant phenomenon during storms, with major implications for global thermosphere circulation patterns and the evolution of ionospheric storms.…”
Section: Discussionmentioning
confidence: 99%
“…As shown by Huang et al (2016), the thermospheric densities respond rapidly to the onset of magnetic activity. This response is exhibited as transient localized maxima in neutral density that we interpret as evidence of localized Joule heating.…”
Section: Energy Deposition At High Latitudesmentioning
confidence: 96%
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“…Moreover, there are numerous recent publications that use GOCE‐derived thermospheric neutral winds also referred in the literature as “crosswinds” and air density profiles for further understanding of thermospheric‐ionospheric studies as well as for model evaluation and assessment purposes (Doornbos et al, ; Drob et al, ; Lu et al, ). For the density retrieval and cross‐track neutral winds derived from previous dedicated gravity missions, namely CHAllenging Minisatellite Payload (CHAMP) and Gravity Recovery and Climate Experiment (GRACE), the reader is referred to Bruinsma and Biancale (), Bruinsma et al (), Doornbos et al (), Forbes et al (), Förster et al (), Huang et al (), Lühr et al (), and Sutton et al ().…”
Section: Introductionmentioning
confidence: 99%