
NSF Org: |
OPP Office of Polar Programs (OPP) |
Recipient: |
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Initial Amendment Date: | March 14, 2006 |
Latest Amendment Date: | March 29, 2010 |
Award Number: | 0520546 |
Award Instrument: | Continuing Grant |
Program Manager: |
Renee Crain
rcrain@nsf.gov (703)292-4482 OPP Office of Polar Programs (OPP) GEO Directorate for Geosciences |
Start Date: | March 15, 2006 |
End Date: | February 29, 2012 (Estimated) |
Total Intended Award Amount: | $1,015,026.00 |
Total Awarded Amount to Date: | $1,034,970.00 |
Funds Obligated to Date: |
FY 2007 = $197,388.00 FY 2008 = $202,486.00 FY 2009 = $209,240.00 FY 2010 = $241,363.00 |
History of Investigator: |
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Recipient Sponsored Research Office: |
2145 N TANANA LOOP FAIRBANKS AK US 99775-0001 (907)474-7301 |
Sponsor Congressional District: |
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Primary Place of Performance: |
2145 N TANANA LOOP FAIRBANKS AK US 99775-0001 |
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): |
Upper Atmospheric Facilities, ANT Astrophys & Geospace Sci, ARC Rsch Support & Logistics |
Primary Program Source: |
app-0107 01000809DB NSF RESEARCH & RELATED ACTIVIT 01000910DB NSF RESEARCH & RELATED ACTIVIT 01001011DB NSF RESEARCH & RELATED ACTIVIT 0100CYXXDB 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): | 47.078 |
ABSTRACT
The overall goal of this project is to continue the operations of the Kodiak SuperDARN Radar.
The Super Dual Auroral Radar Network, or SuperDARN, is an international collaborative
experiment for observations of plasma motions in Earth's upper atmosphere. By observing ionospheric plasma motions, a multitude of geophysical processes can be studied. These
processes range from E-region plasma instabilities, to the relationships between auroral
luminosity and electric fields, to the global-scale convective response to changes in the solar
wind and interplanetary magnetic field. Each of these areas of study contributes to the overall
goals of space physics: developing an understanding of the coupling of energy from the solar
wind into Earth's upper atmosphere and its effects on man or manmade systems. The Kodiak radar is particularly well suited for studies of he general areas to be addressed are convection observations, substorm processes, dayside transients, reconnection features at the cusp, mesospheric winds observed in meteor scatter, gravity waves, and thermosphere-ionosphere interactions, and these will be supported by this award.
The SuperDARN network comprises nine radars in the northern hemisphere, and seven radars in
the southern hemisphere, each operated independently by the member institutions, and supported
by the national agencies in their countries of residence. As is the nature of such networks, data from the SuperDARN network are used in such a wide variety of studies by such a wide range of scientists that it is prohibitive to produce a comprehensive list of the topics.
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.
Over the time period covered by this grant a number of exciting and important results were obtained. In addition, a number of students worked on the project in ways that contributed significantly to their educations.
Major findings:
The first major study examined average flow patterns for ten substorm intervals in an attempt to identify common features. The features that could be identified were: 1) An increase of the zonal convection speed in the pre-midnight region equatorward of the convection reversal boundary associated with a southward turning of the IMF becoming effective at the dayside magnetosphere, 2) A further enhancement of the zonal convection speed about 8 minutes prior to expansion onset, and 3) An abrupt and significant decrease of convection speed at the onset time accompanied by a rotation of the near-midnight flow from zonal to meridional out of the polar cap. These features are consistent with features identified in previous case studies of convection patterns during substorms.
Another study examined the characteristics of radar scatter and optical emissions from the ionospheric volume heated by high-power RF. It was found that there was a significant change in both of these quantities when the heating frequency passed through the second gyroharmonic. Optical emissions increased while HF backscatter decreased. The observations were compared to expectations from theory and were found to agree substantially.
Another study was published that reviewed a number of the developments and findings from the first decade of SuperDARN.
Another study examined the altitude distribution of optical emissions generated in HF ionospheric heating. Kodiak radar observations were used in conjunction with the optical observations to indicate the presence of ionospheric irregularities.
Another paper presented a methodology for the remote sensing of magnetic reconnection in the magnetosphere from the ionosphere. This method combines measurements of ionospheric plasma convection and the ionospheric footprint of the reconnection separatrix.
A study was undertaken with the goals of determining the level of fluctuation due to internal magnetospheric processes, and to examine the probability of observing a significant velocity fluctuation within any given time interval. The study included 6 years of observations from periods when the interplanetary magnetic field (IMF) was moderately southward and steady.
A study used SuperDARN data to study high-latitude ionospheric convection over a three hour period (starting at 22:00 UT on 2 January 2003), during which the Interplanetary Magnetic Field (IMF) flipped between two states, one with By>>|Bz| and one with Bz>0, both with negative Bx. We found that day side ionospheric convection was controlled by the IMF in both hemispheres.
Another study used the Super Dual Auroral Radar Network (SuperDARN) convection database in conjunction with a list of substorm onsets determined from the IMAGE satellite to examine the relationship between substorm onset locations and features of the convection pattern.
In addition to the publications a large number of conference presentations were made and data were supplied to a large number of users for studies in which nobody supported by this grant was named as co-author.
Student training:
Beginning in the first year of the grant three students carried out projects which ultimately led to their Master’s theses. A UAF engineering student supported under this grant wrote driver software for the digital receivers used by many of the radars. Writing the driver software constituted a portion of the student’s thesis work.
A second student developed a techni...
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