Super Dual Auroral Radar Network

The Super Dual Auroral Radar Network (SuperDARN) is an international scientific radar network[1][2] consisting of 35[3] high frequency (HF) radars located in both the Northern and Southern Hemispheres. SuperDARN radars are primarily used to map high-latitude plasma convection in the F region of the ionosphere, but the radars are also used to study a wider range of geospace phenomena including field aligned currents, magnetic reconnection, geomagnetic storms and substorms, magnetospheric MHD waves, mesospheric winds via meteor ionization trails, and interhemispheric plasma convection asymmetries.[2] The SuperDARN collaboration is composed of radars operated by JHU/APL, Virginia Tech, Dartmouth College, the Geophysical Institute at the University of Alaska Fairbanks, the Institute of Space and Atmospheric Studies at the University of Saskatchewan, the University of Leicester, Lancaster University, La Trobe University, and the Solar-Terrestrial Environment Laboratory at Nagoya University.

SuperDARN site in Holmwood SDA, Saskatoon

History

In the 1970s and 1980s, the Scandinavian Twin Auroral Radar Experiment (STARE) very high frequency (VHF) coherent scatter radars were used to study field aligned E region ionospheric irregularities. Using two radars with overlapping fields of view, it was possible to determine the 2D velocity vector of E region ionospheric plasma flow.[2] However, irregularities were only observed when the radar wavevector was perpendicular to the magnetic field in the scattering region.

This meant that there was a problem with operating at VHF since VHF frequencies don't allow for very much refraction of the transmitted radar wave vector; thus, the perpendicularity requirement could not be easily met at high latitudes. At HF frequencies, however, refraction of the radar wavevector is greater, and this allows for the perpendicularity requirement to be met at high latitudes. Refraction of radio waves in the ionosphere is a complicated non-linear phenomenon governed by the Appleton–Hartree equation.

In 1983, a steerable-beam HF radar with 16 log-periodic antennas began operations at Goose Bay, Labrador, Canada.[1] Comparing measurements of F region ionopheric plasma velocity from the Goose Bay radar with the Sondestrom Incoherent Scatter Radar revealed that the Goose Bay radar was capable of measuring the F region plasma convection velocity. A magnetically conjugate radar was constructed in Antarctica at Halley Research Station in 1988 as part of the Polar Anglo–American Conjugate Experiment (PACE). PACE provided simultaneous conjugate studies of ionospheric and magnetospheric phenomena.[2]

From PACE, which was only able to determine a single component of the 2D ionospheric velocity, it became apparent that determining the 2D ionospheric velocity would be advantageous. Combining velocity measurements from Goose Bay with a second coherent-scatter radar in Schefferville in 1989 allowed for a 2D determination of the F region ionospheric velocity.

This work led to SuperDARN, a network of HF radars with pairs of radars having overlapping fields of view. This arrangement allowed for the determination of the full 2D ionospheric plasma convection velocity. Due to the advancement of data assimilation models, radars recently added to the network do not necessarily have overlapping fields of view. Using data from all SuperDARN radars in the northern or southern hemisphere, an ionospheric plasma convection pattern—a map of high-latitude plasma velocity at F region altitudes (300 km)—can be determined.[2]

Primary Goals

The primary goals of SuperDARN are to determine or study:

  • Structure of global convection—to provide a global-scale view of the configuration of plasma convection in the high-latitude ionosphere;
  • Dynamics of global convection—to provide a global-scale view of the dynamics of plasma convection in the high-latitude ionosphere. (Previous studies of high-latitude convection had largely been statistical and time-averaged);
  • Substorms—to test various theories of polar cap expansion and contraction under changing IMF conditions and observe the large-scale response of the nightside; convection pattern to substorms:
  • Gravity waves,
  • High-latitude plasma structures, and
  • Ionospheric irregularities

Operations

SuperDARN radars operate in the HF band between 8.0 MHz (37m) and 22.0 MHz (14m).[2] In the standard operating mode each radar scans through 16 beams of azimuthal separation of ~3.24°, with a scan taking 1 min to complete (~3 seconds integration per beam).

Each beam is divided into 75 (or 100) range gates each 45 km in distance, and so in each full scan the radars each cover 52° in azimuth and over 3000 km in range; an area encompassing the order of 1 million square km.

The radars measure the Doppler velocity (and other related characteristics) of plasma density irregularities in the ionosphere.

Since Linux became popular, it has become the default operating system for the SuperDARN network. The operating system (superdarn-ros.3.6) is currently licensed under the LGPL).

SuperDARN sites

The following is a list of SuperDARN sites, based on a list maintained by Virginia Tech College of Engineering.[4] As of 2009, an expansion project was underway for expanding the network into the middle latitudes, including the addition of sites in Hays, Kansas (near Fort Hays State University), Oregon, and the Azores, in order to support mapping outside of the auroral regions during large magnetic storms.[5]

NameCodeLocationCoordinatesBoresight
Heading
Institute (website)Nationality
Northern Hemisphere
King SalmonksrKing Salmon, Alaska, United States58.6918°N 156.6588°W / 58.6918; -156.6588−20.0°National Institute of Information and Communications TechnologyJapan
Adak Island EastadeAdak Island, Alaska, United States51.8929°N 176.6285°W / 51.8929; -176.628546.0°University of Alaska FairbanksUnited States
Adak Island Westadw51.8931°N 176.6310°W / 51.8931; -176.6310−28.0°
KodiakkodKodiak, Alaska, United States57.6119°N 152.1914°W / 57.6119; -152.191430.0°
Prince GeorgepgrPrince George, British Columbia, Canada53.9812°N 122.5920°W / 53.9812; -122.5920−5.0°University of SaskatchewanCanada
SaskatoonsasSaskatoon, Saskatchewan, Canada52.1572°N 106.5305°W / 52.1572; -106.530523.1°
Rankin InletrknRankin Inlet, Nunavut, Canada62.8281°N 92.1130°W / 62.8281; -92.11305.7°
InuvikinvInuvik, Northwest Territories, Canada68.4129°N 133.7690°W / 68.4129; -133.769026.4°
Clyde RiverclyClyde River, Nunavut, Canada70.4867°N 68.5037°W / 70.4867; -68.5037−55.6°
BlackstonebksBlackstone, Virginia, USA37.1019°N 77.9502°W / 37.1019; -77.9502-40.0°Virginia Polytechnic Institute and State UniversityUnited States
Fort Hays EastfheHays, Kansas, United States38.8585°N 99.3886°W / 38.8585; -99.388645.0°
Fort Hays Westfhw38.8588°N 99.3904°W / 38.8588; -99.3904−25.0°
Goose BaygbrHappy Valley-Goose Bay,
Newfoundland and Labrador, Canada
53.3179°N 60.4642°W / 53.3179; -60.46425.0°
KapuskasingkapKapuskasing, Ontario, Canada49.3929°N 82.3219°W / 49.3929; -82.3219−12.0°
Wallops IslandwalWallops Island, Virginia, United States37.8576°N 75.5099°W / 37.8576; -75.509935.9°Johns Hopkins University Applied Physics LaboratoryUnited States
StokkseyristoStokkseyri, Iceland63.8603°N 21.0310°W / 63.8603; -21.0310−59.0°Lancaster UniversityUnited Kingdom
Þykkvibær
Cutlass/Iceland
pykÞykkvibær, Iceland63.7728°N 20.5445°W / 63.7728; -20.544530.0° University of Leicester
Hankasalmi
Cutlass/Finland
hanHankasalmi, Finland62.3140°N 26.6054°E / 62.3140; 26.6054−12.0°
LongyearbyenlyrLongyearbyen, Norway78.1535°N 16.0607°E / 78.1535; 16.060723.7°UNISNorway
Hokkaido EasthokHokkaido, Japan43.5318°N 143.6144°E / 43.5318; 143.614425.0°Nagoya UniversityJapan
Hokkaido Westhkw43.5372°N 143.6075°E / 43.5372; 143.6075−30.0°
Christmas
Valley East
cveChristmas Valley, Oregon, United States43.2703°N 120.3567°W / 43.2703; -120.356754.0°Dartmouth CollegeUnited States
Christmas
Valley West
cvw43.2707°N 120.3585°W / 43.2707; -120.3585−20.0°
Southern Hemisphere
NameCodeLocationCoordinatesBoresight
Heading
Institute (website)Nationality
Dome C EastdceConcordia Station, Antarctica75.090°S 123.350°E / -75.090; 123.350115.0°Institute for Space Astrophysics and PlanetologyItaly
Dome C Northdcn75.086°S 123.3597°E / -75.086; 123.3597-28.0°
Halley*halHalley Research Station, Antarctica75.6200°S 26.2192°W / -75.6200; -26.2192165.0°British Antarctic SurveyUnited Kingdom
McMurdomcmMcMurdo Station, Antarctica77.8376°S 166.6559°E / -77.8376; 166.6559300.0°University of Alaska FairbanksUnited States
South PolespsSouth Pole Station, Antarctica89.995°S 118.291°E / -89.995; 118.29175.7°
SANAE*sanSANAE IV, Vesleskarvet, Antarctica71.6769°S 2.8282°W / -71.6769; -2.8282173.2°South African National Space AgencySouth Africa
Syowa South*sysShowa Station, Antarctica69.0108°S 39.5900°E / -69.0108; 39.5900159.0°National Institute of Polar ResearchJapan
Syowa East*sye69.0085°S 39.6003°E / -69.0085; 39.6003106.5°
KerguelenkerKerguelen Islands49.3505°S 70.2664°E / -49.3505; 70.2664168.0°French National Centre for Scientific ResearchFrance
TIGERtigBruny Island, Tasmania, Australia43.3998°S 147.2162°E / -43.3998; 147.2162180.0°La Trobe UniversityAustralia
TIGER-UnwinunwAwarua, near Invercargill, New Zealand46.5131°S 168.3762°E / -46.5131; 168.3762227.9°
Buckland ParkbpkBuckland Park, South Australia, Australia34.6270°S 138.4658°E / -34.6270; 138.4658146.5°
ZhongshanzhoZhongshan Station, Antarctica69.3766°S 76.3681°E / -69.3766; 76.368172.5°Polar Research Institute of ChinaChina

*: Part of the Southern Hemisphere Auroral Radar Experiment

Coverage

Northern Hemisphere

  • Because the SuperDARN network evolved in the west during the late Cold War, coverage of Russia's arctic regions is poor.
  • Although there is no shortage of possible sites to cover Russia's Arctic regions from Northern Europe and Alaska, the coverage would probably not be of high quality.
  • Although Russian universities have worked with the University of Leicester and installed a HF radar in Siberia, national funding issues have limited the radar operations.
  • The Polar Research Institute of China has extended mid-latitude coverage, christening the extension to SuperDARN "AgileDARN" [6]

Southern Hemisphere

  • Although Antarctica is covered reasonably well, the Sub-Antarctic regions do not have uniform coverage due to the large expanse of ocean.
  • Java VM real time display software interoperability (where both poles could be observed at the same time) is still a work in progress.

Annual SuperDARN Workshops

Each year the SuperDARN scientific community gather to discuss SuperDARN science, operations, hardware, software and other SuperDARN related issues. Traditionally, this workshop has been hosted by one of the SuperDARN PI groups, often at their home institution, or at another location such as a site close to a radar installation. A list of the SuperDARN workshop locations and their host institutions is provided below:

YearVenueHost Institution
2019Fujiyoshida, Yamanashi, JapanNational Institute of Information and Communications Technology (NICT)
2018Banyuls-sur-Mer, FranceL'Institut de Recherche en Astrophysique et Planétologie (IRAP)
2017San Quirico D'Orcia, Siena, ItalyInstitute for Space Astrophysics and Planetology (IAPS) of the National Institute for Astrophysics (INAF)
2016Fairbanks, Alaska, USAGeophysical Institute, University of Alaska Fairbanks
2015Leicester, UKRadio and Space Plasma Physics Group (RSPP), University of Leicester
2014Longyearbyen, Svalbard, NorwayThe University Centre in Svalbard (UNIS)
2013Moose Jaw, Saskatchewan, CanadaUniversity of Saskatchewan
2012Shanghai, ChinaPolar Research Institute of China
2011Hanover, New Hampshire, USADartmouth College
2010Hermanus, South AfricaSANSA Space Science (previously the Hermanus Magnetic Observatory, HMO)
2009Cargèse, Corsica, FranceLe Centre national de la recherche scientifique (CNRS)
2008Newcastle, New South Wales, AustraliaSchool of Mathematical & Physical Sciences, Newscastle University
2007Abashiri, Hokkaido, JapanInstitute for Space-Earth Environmental Research, Nagoya University
2006Chincoteague, USAJohns Hopkins University, Applied Physics Laboratory (APL)
2005Cumbria, UKBritish Antarctic Survey (BAS)
2004Saskatoon, CanadaUniversity of Saskatchewan
2003Kiljava, Finland
2002Valdez, Alaska, USAGeophysical Institute, University of Alaska Fairbanks
2001Venice, Italy
2000Beechworth, Victoria, AustraliaLa Trobe University
1999Reykjavik, Iceland
1998Tokyo, JapanNational Institute of Polar Research (NIPR)
1997Ithala Game Reserve, South Africa
1996Ellicott City, MD, USA
1995Madingley Hall, Cambridge, UK

References

  1. Greenwald, R.A. (February 1, 1995). "DARN/SuperDARN". Space Science Reviews. 71 (1–4): 761–796. Bibcode:1995SSRv...71..761G. doi:10.1007/BF00751350.
  2. Chisham, G. (January 1, 2007). "A decade of the Super Dual Auroral Radar Network (SuperDARN): scientific achievements, new techniques and future directions". Surveys in Geophysics. 28 (1): 33–109. Bibcode:2007SGeo...28...33C. doi:10.1007/s10712-007-9017-8.
  3. Ruohoniemi, M.J. "VT SuperDARN Home: Virginia Tech SuperDARN". Retrieved February 23, 2015.
  4. "SuperDARN". Virginia Tech. Retrieved 2015-01-07.
  5. "APL Part of International Team Expanding Space Weather Radar Network". Johns Hopkins Applied Physics Laboratory. 2009-08-30. Retrieved 2015-01-07.
  6. "SuperDARN Workshop 2016". SuperDARN Workshop 2016. University of Alaska, Fairbanks. Retrieved 10 August 2016.

Research papers

Research papers related to SuperDARN and related technologies

Real time display of SuperDarn radar

Each participating university should be listed here. As these are ongoing research sites, these links are subject to change.

Northern Hemisphere Stations

Southern Hemisphere Stations

Media related to Unwin Radar at Wikimedia Commons

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