Dependence of spectral width of ionosphericFregion HF echoes on electric field

Author:

Kozlovsky A.1,Shalimov S.23,Koustov A. V.4,Lukianova R.35,Turunen T.1

Affiliation:

1. Sodankylä Geophysical Observatory; Sodankylä Finland

2. Institute of Physics of the Earth; Moscow Russia

3. Space Research Institute; Moscow Russia

4. Department of Physics and Engineering Physics; University of Saskatchewan; Saskatoon, Saskatchewan Canada

5. Arctic and Antarctic Research Institute; St. Petersburg Russia

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference22 articles.

1. HF radar signatures of the cusp and low-latitude boundary layer;Baker;J. Geophys. Res.,1995

2. A statistical comparison of SuperDARN spectral width boundaries and DMSP particle precipitation boundaries in the nightside ionosphere;Chisham;Geophys. Res. Lett.,2004

3. A statistical comparison of SuperDARN spectral width boundaries and DMSP particle precipitation boundaries in the morning sector ionosphere;Chisham;Ann. Geophys.,2005

4. Statistical analysis of echo power, Doppler velocity and spectral width obtained with the Syowa South HF radar;Fukumoto;Adv. Polar Upper Atmos. Res.,1999

5. DARN/SuperDARN: A global view of the dynamics of high-latitude convection;Greenwald;Space Sci. Rev.,1995

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