Overview of Changes and Developments in the SuperDARN Upper Atmosphere Facility - PowerPoint PPT Presentation

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Overview of Changes and Developments in the SuperDARN Upper Atmosphere Facility

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Kapuskasing and Goose Bay: potential antenna deterioration ... Air Force infrastructure support for Goose Bay disappearing. Ionosonde no longer in operation ... – PowerPoint PPT presentation

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Title: Overview of Changes and Developments in the SuperDARN Upper Atmosphere Facility


1
Overview of Changes and Developments in the
SuperDARN Upper Atmosphere Facility
  • Raymond A. Greenwald, J. Michael Ruohoniemi,
    Joseph B. H. Baker
  • Bradley Department of Electrical and Computer
    Engineering
  • Virginia Tech
  • Elsayed Talaat and Robin Barnes
  • Johns Hopkins University Applied Physics
    Laboratory
  • Presented at the 2008 NSF Upper Atmosphere
    Facilities Workshop

1
Space _at_ Virginia Tech
2
Organizational Changes
  • Virginia Tech is now the Principal Investigator
    Institution of the U.S. SuperDARN Upper
    Atmosphere Facility.
  • Transition brought about by
  • Retirement of Ray Greenwald from JHU/APL.
  • Academic appointments of Mike Ruohoniemi and
    Joseph Baker at Virginia Tech.
  • JHU/APL remains a collaborating partner within
    the SuperDARN UAF.
  • Effort carried out by Elsayed Talaat and Robin
    Barnes.

3
Motivations for Change
  • Virginia Tech offers significantly greater
    opportunities for student training and
    development.
  • Virginia Tech has provided considerable
    institutional support for the development of the
    SuperDARN research effort.

4
New Organizational Staffing
  • Virginia Tech
  • J. Michael Ruohoniemi Associate Professor in
    Department of Electrical and Computer
    Engineering (ECE)
  • Joseph B. H. Baker Assistant Professor in ECE
  • Raymond A. Greenwald Part-time Research
    Professor in ECE
  • JHU/APL
  • Elsayed Talaat JHU/APL Science Lead
  • Robin Barnes Software Development

5
Organizational Responsibilities
  • Virginia Tech
  • Radar operations and maintenance
  • Scientific research
  • Community support
  • Education and outreach
  • JHU/APL
  • Scientific research
  • Software development
  • Community support
  • Outreach
  • Data distribution

6
Development of SuperDARNNorthern Hemisphere
Situation Today
Viewgraph from 2005 UAF Meeting
7
SuperDARN Northern HemisphereFuture Development
The right-hand map includes all of the radars
shown at the left plus eight radars extending
from the Azores to the Aleutians that constitute
an NSF MSI proposal and a single radar in violet
located in the U.K. Also, shown are additional
radars identified by faint dashed lines that have
been proposed by other countries to various
funding agencies.
8
Technology InnovationGreenwald Twin-Terminated
Folded Dipole Antenna
  • The TTFD antenna has proven to be a major
    improvement in SuperDARN antenna usage.
  • Reduced cost
  • Improved azimuthal coverage
  • Improved front-to-back ratio
  • More rugged due to fewer electrical connections
    and lower wind loading
  • Used at Wallops Island, Blackstone, Rankin Inlet,
    Inuvik, and Antarctica

9
TTFT Antenna Performance
10
Technology InnovationForward and Reverse Optimal
Golomb Sequences
  • In 1972, Farley was the first to apply the
    concept of Golomb rulers to radar measurements in
    the Earths ionosphere.
  • Within the radar community, this technique is
    commonly referred to as multipulse sequences.
  • Multipulse sequences provide a means of resolving
    the range-time ambiguities that are common to
    radar Doppler measurements when there are spread
    targets with significant Doppler velocities.
  • However, multipulse techniques are notorious for
    adding noise due to other transmitter pulses and
    their returns to the analysis process.
  • 6-pulse optimal ruler
  • Possible distances 54321 15
  • Length 17 Missing 10,15

7
4
2
3
1
11
Technology InnovationForward and Reverse Optimal
Golomb Sequences
  • The pattern above is a 13-pulse sequence
    consisting of a single pulse followed by forward
    and reverse 6-pulse optimal Golomb sequences.
  • This pattern is resistant to bad lags due to
    transmitter pulses and strong cross range noise.
  • In most instances there is at least one good
    option for each lag.

12
Technology InnovationForward and Reverse Optimal
Golomb Sequences
Sample types occurring during a 6-pulse Golomb
sequence preceded by a single pulse.
Range Gates 10-14 have gt10 db signal
13
Technology InnovationForward and Reverse Optimal
Golomb Sequences
14
Technology InnovationForward and Reverse Optimal
Golomb Sequences
15
Technology InnovationForward and Reverse Optimal
Golomb Sequences
Bad lags due to transmitter pulses for 13-pulse
forward and reverse sequence.
16
Technology InnovationForward and Reverse Optimal
Golomb Sequences
Bad lags due to Tx pulse and cross-range noise is
highly variable and depends on interplay between
two independent processes.
17
Improved Phase Vs. Lag Measurements Allow Doppler
Velocities to be Determined from Individual Pulse
Sequences
18
Doppler Velocity Vs. Time200 ms Temporal
Resolution
19
14-sec Doppler Velocity Pulsation Observed With
Wallops Island Radar (Greenwald et al., 2008)
Note Similar period on Ottawa magnetometer
20
Science Extended Observations of Sub-Auroral
Plasma Streams (Oksavik et al., 2006)
21
Science Identification of Temperature Gradient
Instability Onset (Greenwald et al., 2006)
22
THEMIS-SuperDARN Substorm Studies
  • During THEMIS tail conjunctions SuperDARN radars
    run a special THEMIS mode that increase temporal
    sensitivity to substorm dynamics
  • Dwell time reduced from 7 to 4 seconds.
  • SD radars returns to a designated camping-beam
    between each successive scan beam.

THEMIS Mode camping beams (Blue)
23
THEMIS-SuperDARN Substorm StudiesFebruary 22,
2008
Substorm expansion phase onset at approximately
0437 UT THEMIS spacecraft measure two bursts of
Earthward convection in the tail. Ground-based
magnetometers measure the onset of Pi2
oscillations. Blackstone Radar Measurements Pi2
oscillations measured on camping beam at
approximately location of plasmapause (Alfven
Waves?).
24
Science Upper Atmosphere Variability at
Mid-Latitudes
25
Education and TrainingAdvanced Degree Students _at_
Virginia Tech
  • Student Advanced Degree
  • Nathaniel Frissell PhD
  • Yin Yan PhD
  • Kevin Sterne MS
  • Frederick Wilder (Bob Clauer) PhD
  • Lyndell Hockersmith (Bob Clauer) MS

26
SuperDARN Issues and Concerns
  • The reconstitution of the JHU/APL SuperDARN
    activity at Virginia Tech and JHU/APL will still
    require some time to bring to completion. At
    Virginia Tech,
  • We have a good group of involved students.
  • We hope to add an engineer with SuperDARN
    experience.
  • Goose Bay and Kapuskasing have upgrade/
    maintenance needs
  • Kapuskasing digital receiver
  • Kapuskasing and Goose Bay new low-loss cables
  • Kapuskasing and Goose Bay potential antenna
    deterioration
  • Serious issues in obtaining maintenance support
    at Wallops

27
SuperDARN Issues and Concerns
  • Air Force infrastructure support for Goose Bay
    disappearing
  • Ionosonde no longer in operation
  • No Air Force funds for heat, electricity, or snow
    plowing
  • Death of Dr. Jean-Paul Villain raises concerns
    about future support for Stokkseryi radar
  • We are working with University of Leicester to
    identify magnitude of problem and possible
    solutions.
  • Full SuperDARN network can produce 4TB of data
    samples per year. How do we gather and
    disseminate data?
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