A survey of plasma irregularities as seen by the midlatitude Blackstone SuperDARN radar

[1] The Super Dual Auroral Radar Network (SuperDARN) is a chain of HF radars that monitor plasma dynamics in the ionosphere. In recent years, SuperDARN has expanded to midlatitudes in order to provide enhanced coverage during geomagnetically active periods. A new type of backscatter from F region plasma irregularities with low Doppler velocity has been frequently observed on the nightside during quiescent conditions. Using three years of data from the Blackstone, VA radar, we have implemented a method for extracting this new type of backscatter from routine observations. We have statistically characterized the occurrence properties of the Sub Auroral Ionospheric Scatter (SAIS) events, including the latitudinal relationships to the equatorward edge of the auroral oval and the ionospheric projection of the plasmapause. We find that the backscatter is confined to local night, occurs on ≈70% of nights, is fixed in geomagnetic latitude, and is equatorward of both the auroral region and the plasmapause boundary. We conclude that SAIS irregularities are observed within a range of latitudes that is conjugate to the inner magnetosphere (plasmasphere).

[1]  Mark B. Moldwin,et al.  A new model of the location of the plasmapause: CRRES results , 2002 .

[2]  J. C. Samson,et al.  Goose Bay radar observations of Earth‐reflected, atmospheric gravity waves in the high‐latitude ionosphere , 1990 .

[3]  R. A. Greenwald,et al.  A case study of plasma processes in the dayside cleft , 1986 .

[4]  K. Baker,et al.  Probabilistic identification of high‐frequency radar backscatter from the ground and ionosphere based on spectral characteristics , 2009 .

[5]  Marc R. Hairston,et al.  Comparison of DMSP cross-track ion drifts and SuperDARN line-of-sight velocities , 2005 .

[6]  D. L. Carpenter WHISTLER STUDIES OF THE PLASMAPAUSE IN THE MAGNETOSPHERE. 1. TEMPORAL VARIATIONS IN THE POSITION OF THE KNEE AND SOME EVIDENCE ON PLASMA MOTIONS NEAR THE KNEE , 1966 .

[7]  Frank D. Lind,et al.  Identification of the temperature gradient instability as the source of decameter‐scale ionospheric irregularities on plasmapause field lines , 2006 .

[8]  Michael C. Kelley,et al.  The temperature gradient drift instability at the equatorward edge of the ionospheric plasma trough , 1976 .

[9]  Russell B. Cosgrove,et al.  Instability of the E‐F coupled nighttime midlatitude ionosphere , 2003 .

[10]  S. Fukao,et al.  Turbulent upwelling of the mid‐latitude ionosphere: 2. Theoretical framework , 1991 .

[11]  Joseph P. Skura,et al.  OVATION: Oval variation, assessment, tracking, intensity, and online nowcasting , 2002 .

[12]  Michael C. Kelley,et al.  On the origin of mesoscale TIDs at midlatitudes , 2011 .

[13]  Jeffrey P. Thayer,et al.  SuperDARN convection and Sondrestrom plasma drift , 2001 .

[14]  Timothy K. Yeoman,et al.  A comparison of veloCity measurements from the CUTLASS Finland radar and the EISCAT UHF system , 1999 .

[15]  Donald Danskin,et al.  Seasonal variation of HF radar F region echo occurrence in the midnight sector , 2004 .

[16]  John W. MacDougall,et al.  Super Dual Auroral Radar Network observations of meteor echoes , 1997 .

[17]  Tsunoda,et al.  High-latitude F-region irregularities: a review and synthesis. Technical report, 1 January 1986-1 July 1987 , 1988 .

[18]  B. M. Shevtsov,et al.  Coordinated observations of nighttime medium‐scale traveling ionospheric disturbances in 630‐nm airglow and HF radar echoes at midlatitudes , 2009 .

[19]  Keisuke Hosokawa,et al.  Plasma irregularities in the duskside subauroral ionosphere as observed with midlatitude SuperDARN radar in Hokkaido, Japan , 2010 .

[20]  Raymond A. Greenwald,et al.  Rates of scattering occurrence in routine HF radar observations during solar cycle maximum , 1997 .

[21]  J. M. Ruohoniemi,et al.  Coherent HF radar backscatter from small-scale irregularities in the dusk sector of the subauroral ionosphere , 1988 .

[22]  J. M. Ruohoniemi,et al.  Drift motions of small‐scale irregularities in the high‐latitude F region: An experimental comparison with plasma drift motions , 1987 .

[23]  Toshihiko Iyemori,et al.  Simultaneous measurement of duskside subauroral irregularities from the CUTLASS Finland radar and EISCAT UHF system , 2002 .

[24]  Toshihiko Iyemori,et al.  Source of field‐aligned irregularities in the subauroral F region as observed by the SuperDARN radars , 2001 .

[25]  Clark A. Miller Electrodynamics of midlatitude spread F 2. A new theory of gravity wave electric fields , 1997 .

[26]  Clark A. Miller,et al.  Electrodynamics of midlatitude spread F 3. Electrohydrodynamic waves? A new look at the role of electric fields in thermospheric wave dynamics , 1997 .

[27]  Jackie A. Davies,et al.  A comparison of EISCAT and SuperDARN F-region measurements with consideration of the refractive index in the scattering volume , 2010 .

[28]  M. J. Keskinen,et al.  Theories of high-latitude ionospheric irregularities: A review , 1982 .

[29]  F. Perkins,et al.  Spread F and ionospheric currents , 1973 .

[30]  Peter. Dyson,et al.  A decade of the Super Dual Auroral Radar Network (SuperDARN): scientific achievements, new techniques and future directions , 2007 .

[31]  Raymond A. Greenwald,et al.  A new approach for identifying ionospheric backscatter in midlatitude SuperDARN HF radar observations , 2011 .

[32]  Keisuke Hosokawa,et al.  Medium-scale traveling ionospheric disturbances observed with the SuperDARN Hokkaido radar, all-sky imager, and GPS network and their relation to concurrent sporadic E irregularities , 2009 .

[33]  Larry J. Paxton,et al.  Observations of ionospheric convection from the Wallops SuperDARN radar at middle latitudes , 2007 .

[34]  B. Fejer,et al.  Correction [to “Ionospheric irregularities”] , 1981 .

[35]  Larry J. Paxton,et al.  First observations of the temporal/spatial variation of the sub‐auroral polarization stream from the SuperDARN Wallops HF radar , 2006 .