2010
DOI: 10.1029/2009ja015013
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Evidence that crater flux transfer events are initial stages of typical flux transfer events

Abstract: Bipolar magnetic perturbations along the normal to the local magnetopause associated with field magnitude enhancements are signatures of typical flux transfer events (T‐FTEs) and are interpreted as evidence of encounters with magnetic flux ropes with strong core fields. If the field magnitude dips at the center of the signature, we identify the event as a crater FTE (C‐FTE). In the multiple‐spacecraft data of the Time History of Events and Macroscale Interactions During Substorms (THEMIS) between 1 May and 31 … Show more

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Cited by 43 publications
(87 citation statements)
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“…Since the tangential plasma flow in the magnetosheath is typical in the range v t = 200-400 km/s [Paschmann et al, 1982;Coroniti, 1985;Zhang et al, 2010;H. Since the tangential plasma flow in the magnetosheath is typical in the range v t = 200-400 km/s [Paschmann et al, 1982;Coroniti, 1985;Zhang et al, 2010;H.…”
Section: Summary and Discussionmentioning
confidence: 99%
“…Since the tangential plasma flow in the magnetosheath is typical in the range v t = 200-400 km/s [Paschmann et al, 1982;Coroniti, 1985;Zhang et al, 2010;H. Since the tangential plasma flow in the magnetosheath is typical in the range v t = 200-400 km/s [Paschmann et al, 1982;Coroniti, 1985;Zhang et al, 2010;H.…”
Section: Summary and Discussionmentioning
confidence: 99%
“…Because of the flow reversal observed within the structure, we interpret the THE signature as that of an FRE, an in vivo flux rope (see Figures 2d and 2e). The dip in the field magnitude B T near the center of the signature at THE suggests that the form of the flux rope was that of a crater FTE, a flux rope in an early stage of formation [ Zhang et al , 2010]. When the structure reached THD, it had evolved into a typical FTE with a strong core field.…”
Section: Themis Observationsmentioning
confidence: 99%
“…There are also some flux ropes with a decrease in magnetic field strength in the center, which are referred to as crater flux ropes (e.g., Farrugia et al, 1988;Sibeck et al, 2008). Zhang et al (2010) proposed that these crater flux ropes are initial stages of typical flux ropes, and they would evolve into typical flux ropes with a reduction of central plasma pressure resulting from the transport of plasma along their axes. Therefore, they are modeled as a non-force-free structure .…”
Section: Introductionmentioning
confidence: 99%