Latitudinal variations of joule heating due to the auroral electrojets

Journal Article · Sun Jan 01 04:00:00 EST 1984 · J. Geophys. Res.; (United States)

DOI:https://doi.org/10.1029/JA089iA01p00245· OSTI ID:6883031

Duboin, M; Kamide, Y

Empirical scaling factors between the height-integrated joule heating rate deduced from measurements of the Chatanika incoherent scatter radar and the square of magnetic perturbation at College are derived. These relationships, calculated for different situations (the eastward and westward electrojects and daytime) are then used to estimate the joule heating rate along the latitudinal extent of the auroral oval on the basis of magnetometer data from the IMS Alaska meridian chain of observations. The total heat input for a disturbed day (April 12, 1978) is estimated to be 2.8 x 10/sup 15/ J.

• Research Organization: CNET/Centre de Recherches en Physique de l'Environnement Terrestre et Planetaire
• OSTI ID: 6883031
• Journal Information: J. Geophys. Res.; (United States), Journal Name: J. Geophys. Res.; (United States) Vol. 89:A1; ISSN JGREA
• Country of Publication: United States
• Language: English

Related Subjects

640201* -- Atmospheric Physics-- Auroral
Ionospheric
& Magetospheric Phenomena
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
AURORAL OVAL
CURRENTS
ELECTRIC CURRENTS
ELECTRIC FIELDS
ELECTRIC HEATING
ELECTROJETS
GEOGRAPHICAL VARIATIONS
HEATING
INCOHERENT SCATTERING
JOULE HEATING
LATITUDE EFFECT
PLASMA HEATING
POLAR CUSP
RESISTANCE HEATING
SCATTERING
VARIATIONS