Difference between revisions of "FG: Dayside FACs and Energy Deposition"
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'''Chairs: Delores Knipp, Geoff Crowley, Stefan Eriksson, and Ramon Lopez''' | '''Chairs: Delores Knipp, Geoff Crowley, Stefan Eriksson, and Ramon Lopez''' | ||
− | '' | + | ===GOAL=== |
+ | |||
+ | ''Explain the relation between enhanced dayside field-aligned currents, their sources in the solar wind and the impacts in the ionosphere-thermosphere system.'' | ||
+ | |||
+ | ---- | ||
+ | |||
+ | ===Description=== | ||
+ | |||
+ | Recent efforts to improve satellite drag prediction have revealed a set of events with anomalous thermospheric density signatures (B. Bowman, personal comm.). These events are associated with interplanetary shocks and large in-the-ecliptic interplanetary magnetic field (IMF) values, often, but not exclusively, while the IMF BZ is positive (Knipp et al., GEM Meeting 2009). Crowley et al. (2010) used the Assimilative Mapping of Ionospheric Electrodynamics (AMIE) procedure to verify extreme values of Joule heating at the foot points of the near-cusp and polar cap field lines during such events and associate them with unmodeled density enhancements. A new Poynting flux data set from the DMSP F-15 satellite confirms the localized dayside energy input (Knipp et al., Work In Progress (WIP), 2010) and further links these events with instances of strong upward ion flow. Although we cite mostly northward IMF literature below, such events also occur with neutral and slightly southward IMF in the presence of a large IMF BY component. | ||
+ | |||
+ | ===Expected Activities and Research Topics=== | ||
+ | |||
+ | We propose to investigate the disturbances described above. There is a significant likelihood that such events direct energy into the dayside thermosphere with little energy input to the magnetotail. Thus the Dst index, could remain unperturbed or even show storm recovery while the coupled dayside high-latitude region is greatly disturbed. We anticipate the following will be fruitful research topics. | ||
+ | |||
+ | *Dayside energy sources and transport for events with large IMF By and Bx (with Bz +/-) | ||
+ | |||
+ | *Dayside field-aligned current systems for large in-the-ecliptic IMF (By and Bx with Bz +/-) | ||
+ | |||
+ | *The location and nature of Poynting and particle energy deposition for IMF Bz>0 and large BY | ||
+ | |||
+ | *The role of enhanced solar wind density and speed during such events | ||
+ | |||
+ | *The relation of such events to cusp region thermospheric density anomalies | ||
+ | |||
+ | *Overall energy contributions to the coupled magnetosphere-ionosphere-thermosphere | ||
+ | |||
+ | *Methods for detecting such disturbances; indices vs. space based monitors | ||
+ | |||
+ | *More realistic MHD modeling of such disturbances | ||
+ | |||
+ | *Overall magnetospheric structure during such disturbances | ||
+ | |||
+ | *Daily and seasonal conductivity effects of high-latitude Joule heating events | ||
+ | |||
[[Image:FG_proposal_Dayside_Energy_Deposition-upload.pdf|thumb]] | [[Image:FG_proposal_Dayside_Energy_Deposition-upload.pdf|thumb]] |
Revision as of 12:55, 28 April 2010
Chairs: Delores Knipp, Geoff Crowley, Stefan Eriksson, and Ramon Lopez
GOAL
Explain the relation between enhanced dayside field-aligned currents, their sources in the solar wind and the impacts in the ionosphere-thermosphere system.
Description
Recent efforts to improve satellite drag prediction have revealed a set of events with anomalous thermospheric density signatures (B. Bowman, personal comm.). These events are associated with interplanetary shocks and large in-the-ecliptic interplanetary magnetic field (IMF) values, often, but not exclusively, while the IMF BZ is positive (Knipp et al., GEM Meeting 2009). Crowley et al. (2010) used the Assimilative Mapping of Ionospheric Electrodynamics (AMIE) procedure to verify extreme values of Joule heating at the foot points of the near-cusp and polar cap field lines during such events and associate them with unmodeled density enhancements. A new Poynting flux data set from the DMSP F-15 satellite confirms the localized dayside energy input (Knipp et al., Work In Progress (WIP), 2010) and further links these events with instances of strong upward ion flow. Although we cite mostly northward IMF literature below, such events also occur with neutral and slightly southward IMF in the presence of a large IMF BY component.
Expected Activities and Research Topics
We propose to investigate the disturbances described above. There is a significant likelihood that such events direct energy into the dayside thermosphere with little energy input to the magnetotail. Thus the Dst index, could remain unperturbed or even show storm recovery while the coupled dayside high-latitude region is greatly disturbed. We anticipate the following will be fruitful research topics.
- Dayside energy sources and transport for events with large IMF By and Bx (with Bz +/-)
- Dayside field-aligned current systems for large in-the-ecliptic IMF (By and Bx with Bz +/-)
- The location and nature of Poynting and particle energy deposition for IMF Bz>0 and large BY
- The role of enhanced solar wind density and speed during such events
- The relation of such events to cusp region thermospheric density anomalies
- Overall energy contributions to the coupled magnetosphere-ionosphere-thermosphere
- Methods for detecting such disturbances; indices vs. space based monitors
- More realistic MHD modeling of such disturbances
- Overall magnetospheric structure during such disturbances
- Daily and seasonal conductivity effects of high-latitude Joule heating events