Statistical evidence for O + energization and outflow caused by wave-particle interaction in the high altitude cusp and mantle
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Statistical evidence for O + energization and outflow caused by wave-particle interaction in the high altitude cusp and mantle ; volume:29 ; number:5 ; year:2011 ; pages:945-954
Annales geophysicae ; 29, Heft 5 (2011), 945-954
- Creator
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Waara, M.
Slapak, R.
Nilsson, H.
Stenberg, G.
André, M.
Barghouthi, I. A.
- DOI
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10.5194/angeo-29-945-2011
- URN
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urn:nbn:de:101:1-201710269561
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:35 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Waara, M.
- Slapak, R.
- Nilsson, H.
- Stenberg, G.
- André, M.
- Barghouthi, I. A.
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Four point measurements of electrons using PEACE in the high-altitude cusp
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Cluster observations of a complex high-altitude cusp passage during highly variable IMF
Wave particle interactions in the high-altitude polar cusp: a Cluster case study
Estimating the fate of oxygen ion outflow from the high altitude cusp
Oxygen ion energization by waves in the high altitude cusp and mantle
O + heating associated with strong wave activity in the high altitude cusp and mantle
Auroral ion outflow: low altitude energization
Spatial and temporal variations of the high-altitude cusp precipitation
Cluster observations of magnetic field fluctuations in the high-altitude cusp
On the structure of field-aligned currents in the mid-altitude cusp
Four point measurements of electrons using PEACE in the high-altitude cusp
Cluster survey of the mid-altitude cusp: 1. size, location, and dynamics
On the altitude dependence of transversely heated O + distributions in the cusp/cleft
Cluster observations of a complex high-altitude cusp passage during highly variable IMF