2008
DOI: 10.5194/angeo-26-3897-2008
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Balanced reconnection intervals: four case studies

Abstract: Abstract. During steady magnetospheric convection (SMC) events the magnetosphere is active, yet there are no data signatures of a large scale reconfiguration, such as a substorm. While this definition has been used for years it fails to elucidate the true physics that is occurring within the magnetosphere, which is that the dayside merging rate and the nightside reconnection rate balance. Thus, it is suggested that these events be renamed Balanced Reconnection Intervals (BRIs). This paper investigates four div… Show more

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Cited by 33 publications
(43 citation statements)
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“…Two methods of polar cap area calculation have been actively used in recent years. They are based on either electron-induced auroral emissions (thereafter referred to as F e , e.g., DeJong and Clauer, 2005;DeJong et al, 2007DeJong et al, , 2008 or protoninduced auroral emissions (thereafter referred to as F p , e.g., Hubert et al, 2006). Methods based on the electron-induced auroral emissions are expected to be more affected by dayglow contamination.…”
Section: Introductionmentioning
confidence: 99%
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“…Two methods of polar cap area calculation have been actively used in recent years. They are based on either electron-induced auroral emissions (thereafter referred to as F e , e.g., DeJong and Clauer, 2005;DeJong et al, 2007DeJong et al, , 2008 or protoninduced auroral emissions (thereafter referred to as F p , e.g., Hubert et al, 2006). Methods based on the electron-induced auroral emissions are expected to be more affected by dayglow contamination.…”
Section: Introductionmentioning
confidence: 99%
“…Global auroral images from DE1 and Viking made possible first individual ''measurements'' of the polar cap area and PC magnetic flux (e.g., Baker et al, 1994;Yahnin et al, 1994). Recently routine optical observation of the polar cap from the POLAR and IMAGE spacecraft during long periods became available at $ 122 min time resolution (Brittnacher et al, 1999;DeJong and Clauer, 2005;Hubert et al, 2006Hubert et al, , 2008Milan et al, 2007;DeJong et al, 2007DeJong et al, , 2008. However, these methods also have some uncertainties: the accuracy of the PC area determination depends on the accuracy of the PC boundaries identification, particularly on the chosen luminosity threshold level.…”
Section: Introductionmentioning
confidence: 99%
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“…The role of the magnetotail field as the main reservoir of energy dissipated during substorms have been questioned by Pulkkinen et al [2006]. Several examples of substorm onsets, not preceded by a pressure or magnetic flux increase in the magnetotail, have been presented [Petrukovich et al, 2000;Yahnin et al, 1994Yahnin et al, , 2001DeJong et al, 2008]. This has also been statistically confirmed by Dmitrieva et al [2004] who noticed that ∼1/3 out of 145 isolated substorm events in the midtail studied did not show any total pressure growth before unloading, whereas a classical growth phase was observed only in the other 1/3 of events (the remaining 1/3 showed a mixed behavior).…”
Section: Introductionmentioning
confidence: 99%
“…If this occurs globally and quasiperiodically then it is termed a global sawtooth oscillation, each unloading in the series is an individual sawtooth injection [ Reeves et al , 2002; Henderson , 2004]. If the energy is not stored and released, but rather continuously diverted, then convection is quasi‐steady, the dayside and nightside reconnection rates are balanced, and the magnetosphere has achieved a balanced reconnection interval (BRI), sometimes described as a steady magnetospheric convection (SMC) mode [ DeJong et al , 2008; Sergeev et al , 1996].…”
Section: Introductionmentioning
confidence: 99%