
NSF Org: |
AGS Division of Atmospheric and Geospace Sciences |
Recipient: |
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Initial Amendment Date: | November 6, 2008 |
Latest Amendment Date: | December 8, 2010 |
Award Number: | 0819662 |
Award Instrument: | Continuing Grant |
Program Manager: |
Paul Bellaire
AGS Division of Atmospheric and Geospace Sciences GEO Directorate for Geosciences |
Start Date: | January 1, 2009 |
End Date: | December 31, 2011 (Estimated) |
Total Intended Award Amount: | $142,242.00 |
Total Awarded Amount to Date: | $142,242.00 |
Funds Obligated to Date: |
FY 2010 = $47,397.00 FY 2011 = $48,923.00 |
History of Investigator: |
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Recipient Sponsored Research Office: |
323 DR MARTIN LUTHER KING JR BLVD NEWARK NJ US 07102-1824 (973)596-5275 |
Sponsor Congressional District: |
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Primary Place of Performance: |
323 DR MARTIN LUTHER KING JR BLVD NEWARK NJ US 07102-1824 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): |
SOLAR-TERRESTRIAL, Upper Atmospheric Facilities |
Primary Program Source: |
01001011DB NSF RESEARCH & RELATED ACTIVIT 01001112DB NSF RESEARCH & RELATED ACTIVIT |
Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
The Principal Investigator will study magnetic reconnection and the associated flare energy release in the form of accelerated electrons, particularly in sigmoidal solar active regions. The proposing team will carry out a comprehensive investigation of solar flare and CME events using newly improved hard X-ray (HXR) imaging and spectroscopy techniques. They will further examine the association of ribbon-like HXR sources with sigmoid eruptions, while quantitatively analyzing the spatial distribution of accelerated electrons and its evolution in the flaring process, in order to establish the most realistic 3D magnetic reconnection scenario.
The PI plans to investigate flare ribbon dynamics, paying special attention to the early phase of solar flare and CME eruptions. Using multi-wavelength data, the proposers will examine the physics of interrelated flaring phenomena, such as contracting-to-separation development and strong-to-weak shear change in H-alpha and EUV/UV, footpoint-to-ribbon evolution in HXR, and sigmoid-to-arcade transformation in EUV and soft X-ray (SXR). The PI will also use the HXR spectral index as a probe to diagnose electron acceleration during flares. The team will study the temporal and spatial relationship between the electric field in reconnecting current sheets and the spectral index of detected HXRs, in order to better understand the electron acceleration mechanism.
Given that sigmoidal structures are among the most important signatures for impending space weather events, this study will contribute significantly to the National Space Weather Program (NSWP) goal of mitigating the adverse effects of space weather on society's technological infrastructure. The PI's status as a beginning postdoctoral researcher constitutes this project's education and training component.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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PROJECT OUTCOMES REPORT
Disclaimer
This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.
Solar flares are energetic eruptive events closely related to space weather. This project aims directly at the flare source region and studies how the magnetic fields in the solar corona can rearrange (i.e., break and reconnect) to release energy, the impact of such reconnection on the lower solar atmosphere, and the associated acceleration of electrons. Observations from both the space-based (such as the recently launched NASA's Solar Dynamics Observatory) and ground-based (such as the renowned Big Bear Solar Observatory in California) instruments are analyzed and jointly studied with theoretical models of coronal magnetic fields.
Our most prominent findings include that (1) we verifies, for the first time, that two oppositely oriented J-shaped loops can reconnect to form continuous, eruptive S-shaped loops (called sigmoids), which have long been regarded as an important signature in space weather forecasts. (2) We present the first unambiguous observation of the rapid and permanent changes of magnetic fields on the solar surface directly associated with the sigmoid eruption. Specifically, the surface fields must become more horizontal after flares. These help to settle a long debate in the solar physics. (3) We firstly demonstrate that while the sigmoids erupt outward, the coronal magnetic fields lying below could collapse downward toward the solar surface. This may hint that outward solar eruptions could be closely related to the downward disturbance such as sunquakes (analogous to earthquakes). (4) We obtain the clearest direct observational evidence of electron acceleration by the reconnection electric field in solar flares. (5) We originally propose in an exploratory way that flare emissions in the solar atmosphere could progress towards regions where the overlying magnetic fields provide less confinement.
Other important findings include that (6) we evidence that multiple solar eruptions can occur within a single but extended flare source region, a phenomenon similar to a "domino" effect. (7) We firstly verify that an eruption mechanism deduced from major flares, in which the removal of confining fields causes the eruption of the twisted core fields, could also apply to the very small-scale flaring activities on the Sun. (8) We reveal that coronal magnetic fields could inflate for many hours before their final eruption, which provides a critical complement to the standard theory for solar eruptions. (9) We show that even a moderate flare can have manifestation as brightenings deep down to the solar surface, which advances the classical view.
The observational outcomes resulted from this project have strong impacts on modeling of solar eruptive events in realization of the goal to mitigate the adverse effects of space weather. This project supports the education and training of a beginning postdoctoral researcher, who has been promoted to a research professor. Our research results have also been used to teach graduate and undergraduate students. A number of them have been involved in solar physics research in the Space Weather Research Laboratory of New Jersey Institute of Technology.
Last Modified: 12/30/2011
Modified by: Chang Liu