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Open AccessJournal ArticleDOI

Cusp aurora dependence on interplanetary magnetic field Bz

TLDR
In this paper, the Imager for Magnetopause to Aurora Global Exploration (IMAGE) Spectrographic Imager (SI12) detects Doppler-shifted Lyman alpha emissions created by charge exchange and de-excitation of precipitating protons in the atmosphere.
Abstract
[1] The Imager for Magnetopause to Aurora Global Exploration (IMAGE) Spectrographic Imager (SI12) detects Doppler-shifted Lyman alpha emissions created by charge exchange and de-excitation of precipitating protons in the atmosphere. At high latitudes near local noon, emissions consistent with the location of the cusp foot point have distinct interplanetary magnetic field (IMF) dependence. For northward IMF a spot of emissions is observed poleward of the dayside auroral oval. By tracing the magnetic field lines from this spot using a model magnetosphere it is shown that the cusp foot point maps to a narrow region on the high-latitude magnetopause where antiparallel magnetic reconnection may be occurring. As the IMF turns southward, the spot merges into the auroral oval, producing a broad region of intense emissions centered near local noon. By tracing the magnetic field lines from this broad region using a model magnetosphere it is shown that the cusp foot point maps to a relatively broad region on the dayside magnetopause where component magnetic reconnection may be occurring.

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A magnetic reconnection X-line extending more than 390 Earth radii in the solar wind

TL;DR: Three-spacecraft observations of accelerated flow associated with reconnection in a current sheet embedded in the solar wind flow imply that reconnection is fundamentally a large-scale process and reveal, surprisingly, that reconnections can operate in a quasi-steady-state manner even when undriven by the external flow.
Journal ArticleDOI

Magnetospheric Multiscale Science Mission Profile and Operations

TL;DR: The magnetospheric multiscale (MMS) mission and operations are designed to provide the maximum reconnection science as mentioned in this paper, where the mission phases are chosen to investigate reconnection at the dayside magnetopause and in the magnetotail.
Journal ArticleDOI

Probing the boundary between antiparallel and component reconnection during southward interplanetary magnetic field conditions

TL;DR: In this article, a method using three-dimensional plasma observations from the Toroidal Imaging Mass-Angle Spectrograph instrument on the Polar spacecraft as it passes through the northern magnetospheric cusp was used to calculate the distance to the reconnection line and subsequently trace the distance along model magnetic field lines back to the magnetopause.
References
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Journal ArticleDOI

The WIND magnetic field investigation

TL;DR: The magnetic field experiment on WIND will provide data for studies of a broad range of scales of structures and fluctuation characteristics of the interplanetary magnetic field throughout the mission, and, where appropriate, relate them to the statics and dynamics of the magnetosphere.
Journal ArticleDOI

Swe, a comprehensive plasma instrument for the wind spacecraft

TL;DR: The solar wind experiment (SWE) on the WIND spacecraft is a comprehensive, integrated set of sensors which is designed to investigate outstanding problems in solar wind physics as discussed by the authors, which consists of two Faraday cup (FC) sensors; a vector electron and ion spectrometer (VEIS); a strahl sensor, which is especially configured to study the electron ‘strahl’ close to the magnetic field direction; and an on-board calibration system.
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Modeling the Earth's magnetospheric magnetic field confined within a realistic magnetopause

TL;DR: In this paper, the authors describe a new approach to the problem of fitting the magnetosphereic magnetic field to spacecraft data, based on fits to a large number of observed crossing (allowing a parametrization by the solar wind pressure).
Journal ArticleDOI

Evidence for magnetic field reconnection at the Earth's magnetopause

TL;DR: In this article, 11 passes of the ISEE satellites through the frontside terrestrial magnetopause were identified, where the plasma velocity in the magnetic field and boundary layer was substantially larger than in the magnetosheath, with a view to determining whether the velocity enhancements can be explained by magnetic field reconnection.
Journal ArticleDOI

The GEOTAIL Magnetic Field Experiment.

TL;DR: The Geotail spacecraft carries a high-resolution Magnetic Field Experiment to provide magnetic field data in the frequency range below 50 Hz as mentioned in this paper, which includes dual fluxgate magnetometers and a search coil magnetometer.
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