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Thermodynamics and electrodynamics of the auroral E-region during the D salvo of the MAP/WINE campaign
Institution:1. Universidade do Vale do Paraíba – Univap, São José dos Campos – SP, Brazil;2. Instituto Federal do Maranhão – IFMA, Alcântara, MA, Brazil;3. Instituto Nacional de Pesquisas Espaciais – INPE, São José dos Campos-SP, Brazil;4. State Key Laboratory of Space Weather, Beijing, China;1. Centro de Instrumentación Científica, Universidad Adventista de Chile, Chillán, Chile;2. Centro Interuniversitario de Física de La Alta Atmósfera, Chile;3. State Key Laboratory of Space Weather, NSSC/CAS, Beijing, China;4. National Institute for Space Research-INPE, São José dos Campos, SP, Brazil;5. Universidad del Bío-Bío, Concepción, Chile;1. Universidade do Vale do Paraíba, Instituto de Pesquisa e Desenvolvimento, São José dos Campos-SP 12.244-000, Brazil;2. Instituto Federal do Maranhão, Departamento de Ensino de Física, Bacabal, MA 65.700-000, Brazil;3. State Key Laboratory of Space Weather, 100190 Beijing, China;4. Instituto Nacional de Pesquisas Espaciais, Divisão de Aeronomia, São José dos Campos-SP, 12.227-010, Brazil
Abstract:With the help of incoherent scatter (EISCAT) data the thermodynamics and electrodynamics of the auroral E-region north east of Andøya Rocket Range has been investigated between 1740 UT and 2040 UT on 31 January 1984. This time period covers the D salvo of MAP/WINE and the EISCAT incoherent scatter data comprise a useful supplement to interpret the rocket data. Good agreement has been found between the EISCAT temperatures and those derived from mass spectrometer data. Neutral wind velocity estimates from EISCAT and from a falling sphere rocket experiment are in satisfactory agreement for the zonal wind component, but disagree for the meridional component.
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