During southward interplanetary magnetic field (IMF), the electron and ion boundary are separated near the dayside boundary layer. Here we show observations at the high latitude magnetosphere tailward of the cusp during northward IMF. We find that the ion edge is observed firstly and then the electron edge is found by Cluster. Detailed analysis indicates that this is caused by the reconnection at the high latitude. The relationship between the observations and the aurora data is also discussed. A global simulation shows that these observations in different regions might be closely related to each other. ? 2011 IEEE.EI
International audienceThis paper reviews Cluster observations of the high altitude and exterior (out...
[1] On 21–22 March 2001, four cusp-like regions were observed consecutively in about five hours by a...
Spectrographic Imager (SI12) detects Doppler-shifted Lyman alpha emissions created by charge exchang...
Cluster four spacecraft data is used to study the spatial-temporal characteristics in/near the high ...
abstract SM22B-04On some occasions, Cluster data in the mid-altitude cusp reveal overlapping ion pop...
International audienceHigh-latitude auroral arcs are a typical feature of periods of northward IMF. ...
International audienceThe nature of particle precipitations at dayside mid-altitudes can be interpre...
The low- and high-latitude boundary layers of the earth's magnetosphere [low-latitude boundary layer...
Launched on an elliptical high inclination orbit (apogee: 19.6 RE) since January 2001 the Cluste...
[1] Various boundary crossings in the vicinity of the high-altitude cusp region were experienced by ...
Abstract SM51A-06The polar cusps are two regions of the magnetosphere where the influence of the int...
We present multi-instrument observations using the meridian scanning photometer (MSP) at Ny Alesund,...
The HF radar Doppler spectral width boundary (SWB) in the cusp represents a very good proxy for th...
We report specific changes in the dayside auroral morphology in the winter hemisphere which occur in...
International audienceWe present multi-instrument observations using the meridian scanning photomete...
International audienceThis paper reviews Cluster observations of the high altitude and exterior (out...
[1] On 21–22 March 2001, four cusp-like regions were observed consecutively in about five hours by a...
Spectrographic Imager (SI12) detects Doppler-shifted Lyman alpha emissions created by charge exchang...
Cluster four spacecraft data is used to study the spatial-temporal characteristics in/near the high ...
abstract SM22B-04On some occasions, Cluster data in the mid-altitude cusp reveal overlapping ion pop...
International audienceHigh-latitude auroral arcs are a typical feature of periods of northward IMF. ...
International audienceThe nature of particle precipitations at dayside mid-altitudes can be interpre...
The low- and high-latitude boundary layers of the earth's magnetosphere [low-latitude boundary layer...
Launched on an elliptical high inclination orbit (apogee: 19.6 RE) since January 2001 the Cluste...
[1] Various boundary crossings in the vicinity of the high-altitude cusp region were experienced by ...
Abstract SM51A-06The polar cusps are two regions of the magnetosphere where the influence of the int...
We present multi-instrument observations using the meridian scanning photometer (MSP) at Ny Alesund,...
The HF radar Doppler spectral width boundary (SWB) in the cusp represents a very good proxy for th...
We report specific changes in the dayside auroral morphology in the winter hemisphere which occur in...
International audienceWe present multi-instrument observations using the meridian scanning photomete...
International audienceThis paper reviews Cluster observations of the high altitude and exterior (out...
[1] On 21–22 March 2001, four cusp-like regions were observed consecutively in about five hours by a...
Spectrographic Imager (SI12) detects Doppler-shifted Lyman alpha emissions created by charge exchang...