Open AccessRemote sensing space weather events: Antarctic‐Arctic Radiation‐belt (Dynamic) Deposition‐VLF Atmospheric Research Konsortium network
Author(s) -
Clilverd Mark A.,
Rodger Craig J.,
Thomson Neil R.,
Brundell James B.,
Ulich Thomas,
Lichtenberger János,
Cobbett Neil,
Collier Andrew B.,
Menk Frederick W.,
Seppälä Annika,
Verronen Pekka T.,
Turunen Esa
Publication year - 2009
Publication title -
space weather
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.254
H-Index - 56
ISSN - 1542-7390
DOI - 10.1029/2008sw000412
Subject(s) - space weather , environmental science , ionosphere , space physics , atmosphere (unit) , coronal mass ejection , meteorology , van allen radiation belt , atmospheric sciences , physics , geophysics , magnetosphere , solar wind , plasma , quantum mechanics , magnetic field
The Antarctic‐Arctic Radiation‐belt (Dynamic) Deposition‐VLF Atmospheric Research Konsortium (AARDDVARK) provides a network of continuous long‐range observations of the lower ionosphere in the polar regions. Our ultimate aim is to develop the network of sensors to detect changes in ionization levels from ∼30–90 km altitude, globally, continuously, and with high time resolution, with the goal of increasing the understanding of energy coupling between the Earth's atmosphere, the Sun, and space. This science area impacts our knowledge of space weather processes, global atmospheric change, communications, and navigation. The joint New Zealand‐United Kingdom AARDDVARK is a new extension of a well‐established experimental technique, allowing long‐range probing of ionization changes at comparatively low altitudes. Most other instruments which can probe the same altitudes are limited to essentially overhead measurements. At this stage AARDDVARK is essentially unique, as similar systems are only deployed at a regional level. The AARDDVARK network has contributed to the scientific understanding of a growing list of space weather science topics including solar proton events, the descent of NO x into the middle atmosphere, substorms, precipitation of energetic electrons by plasmaspheric hiss and electromagnetic ion cyclotron waves, the impact of coronal mass ejections upon the radiation belts, and relativistic electron microbursts. Future additions to the receiver network will increase the science potential and provide global coverage of space weather event signatures.