SUR L'UNICITE DE LA DISTRIBUTION SPECTRALE DES VARIATIONS IRREGULIERES A LONGUE PERIODE DU CHAMP GEOMAGNETIQUEDUBROVSKIJ VG; KRAMARENKO SA.1975; IZVEST. AKAD. NAUK TURKM. S.S.R., FIZ.-TEKH. KHIM. GEOL. NAUK; S.S.S.R.; DA. 1975; NO 2; PP. 50-55; ABS. TURKM. ANGL.; BIBL. 11 REF.Article

ON THE RELATIONSHIP BETWEEN AURORAL ELECTROJET INTENSITY FLUCTUATION AND THE WIND FIELD NEAR THE MESOPAUSEBALSLEY BB; CARTER DA; ECKLUND WL et al.1982; GEOPHYS. RES. LETT.; ISSN 0094-8276; USA; DA. 1982; VOL. 9; NO 3; PP. 219-222; BIBL. 14 REF.Article

ALTITUDE DES AURORES RADIOELECTRIQUESTIMOFEEV EE; MIROSHNIKOV YU G; KHOR'KOVA TN et al.1982; GEOMAGN. AERON.; ISSN 0016-7940; SUN; DA. 1982; VOL. 22; NO 2; PP. 249-251; BIBL. 12 REF.Article

VARIATIONS DE LA LATITUDE ET DE L'INTENSITE DU COURANT DE L'ELECTROJET AURORALOL GI; SUVOROVA LA.1981; TR. ARKT. ANTARKT. NAUCNO-ISSLED. INST.; ISSN 500461; SUN; DA. 1981; VOL. 377; PP. 21-36; BIBL. 25 REF.Article

AURORAL ELECTROJET INDICES (AE) FOR JANUARY-JUNE 1978 AND JULY-DECEMBER 19781982; SOL. TERR. ENVIRON. RES. JPN; ISSN 0386-5444; JPN; DA. 1982; VOL. 6; PP. 34-35Article

INTERPRETATION OF AURORAL OVAL EQUIVALENT CURRENT FLOW NEAR DUSK USING INVERSION TECHNIQUESHUGHES TJ; OLDENBURG DW; ROSTOKER G et al.1979; J. GEOPHYS. RES.; USA; DA. 1979; VOL. 84; NO A2; PP. 450-456; BIBL. 1 P.Article

A TWO-DIMENSIONAL MAGNETOMETER ARRAY FOR GROUND-BASED OBSERVATIONS OF AURORAL ZONE ELECTRIC CURRENTS DURING THE INTERNATIONAL MAGNETOSPHERIC STUDY (IMS)KUEPPERS F; UNTIEDT J; BAUMJOHANN W et al.1979; J. GEOPHYS.; DEU; DA. 1979; VOL. 46; NO 4; PP. 429-450; BIBL. 2 P.Article

JOINT MAGNETOMETER ARRAY AND RADAR BACKSCATTER OBSERVATIONS OF AURORAL CURRENTS IN NORTHERN SCANDINAVIA.BAUMJOHANN W; GREENWALD RA; KUPPERS F et al.1978; J. GEOPHYS.; DEU; DA. 1978; VOL. 44; NO 4; PP. 373-383; BIBL. 15 REF.Article

AURORAL INFRASONIC WAVES OBSERVED AT WINDLESS BIGHT, ANTARCTICA.WILSON CR.1977; ANTARCT. J. U.S.; U.S.A.; DA. 1977; VOL. 12; NO 4; PP. 200-202; BIBL. 6 REF.Article

STRUCTURE A GRANDE ECHELLE DU CHAMP ELECTRIQUE DANS L'IONOSPHERE POLAIRE. IIIGUREVICH AV; KRYLOV AL.1974; GEOMAGNET. I AERONOM.; S.S.S.R.; DA. 1974; VOL. 14; NO 4; PP. 622-626; BIBL. 6 REF.Article

Effets magnétiques au sol, provoqués par l'électrojet de «polarisation»KUZNETSOV, B. M.Kosmičeskie issledovaniâ. 1986, Vol 24, Num 3, pp 474-476, issn 0023-4206Article

AURORAL INFRASONIC WAVES AND THE AURORAL ELECTROJETSUZUKI Y.1979; J. ATMOSPH. TERRESTR. PHYS.; GBR; DA. 1979; VOL. 41; NO 1; PP. 11-23; BIBL. 12 REF.Article

AURORAL ELECTROJET MAGNETIC ACTIVITY INDICES AE (11) FOR 1972.ALLEN JH; ABSTON CC; MORRIS LD et al.1975; WORLD DATA CENTER A SOLAR-TERRESTR. PHYS., REP. U.A.G.; U.S.A.; DA. 1975; NO 45; PP. 1-146; BIBL. 7 REF.Article

AURORAL INFRASONIC WAVE GENERATION MECHANISMWILSON CR.1972; A.G.A.R.D. CONF. PROC.; FR.; DA. 1972; NO 115; PP. 19P.; ABS. FR.; BIBL. 31REF.Serial Issue

RECONSTITUTION DE L'ELECTROJET AURORAL DURANT L'APPARITION D'UNE AURORE RADIOELECTRIQUEANTIPIN SV; VAKULIN YU I; VASIL'EV IN et al.1980; GEOMAGN. AERON.; ISSN 0016-7940; SUN; DA. 1980; VOL. 20; NO 5; PP. 961-963; BIBL. 5 REF.Article

DETECTION OF 2 HZ INFRASOUND PRODUCED BY MOVING AURORAL ELECTROJETSLISZKA L; WESTIN H.1972; K.G.O. REP.; SWEDEN; DA. 1972; NO 727; PP. 1-7; H.T. 14; BIBL. 11REF.Serial Issue

DETECTION OF 2 HZ INFRASOUND PRODUCED BY MOVING AURORAL ELECTROJETSLISZKA L; WESTIN H.1972; A.G.A.R.D. CONF. PROC.; FR.; DA. 1972; NO 115; PP. 11P.; ABS. FR.; BIBL. 11REF.Serial Issue

NOTES ON THE AURORAL ELECTROJET INDICESKAMIDE Y; AKASOFU SI.1983; REVIEWS OF GEOPHYSICS AND SPACE PHYSICS; ISSN 0034-6853; USA; DA. 1983; VOL. 21; NO 7; PP. 1647-1656; BIBL. 1 P.Article

CAMPOS ELETRICOS NA REGIAO IONIZADA DA ATMOSFERA = CHAMPS ELECTRIQUES DES REGIONS IONISEES DE L'ATMOSPHEREKIRCHHOFF VWJH.1981; REV. BRAS. FIS.; ISSN 0374-4922; BRA; DA. 1981; VOL. 11; NO 3; PP. 711-725; ABS. ENG; BIBL. 21 REF.Article

2 HZ INFRASOUND AND GEOMAGNETIC ACTIVITY.WESTIN H.1976; K.G.I. REP.; SWED.; DA. 1976; VOL. 76; NO 2; PP. 1-17; BIBL. 8 REF.Serial Issue

Comment on The poleward leap of the auroral electrojet as seen in auroral images by Edward W. Hones, Jr. ReplyROSTOKER, G; HONES, E. W. JR.JGR. Journal of geophysical research. Part A, Space physics. 1986, Vol 91, Num 5, pp 5879-5884Article

HEIGHT DEPENDENCE IN THE POWER SPECTRUM OF DIFFUSE RADAR AURORAUNWIN RS; JOHNSTON PV.1981; J. GEOPHYS. RES.; ISSN 0022-1406; USA; DA. 1981; VOL. 86; NO A7; PP. 5733-5745; BIBL. 23 REF.Article

COORDINATED MAGNETIC OBSERVATIONS OF MORNING SECTOR AURORAL ZONE CURRENTS WITH TRIAD AND THE SCANDINAVIAN MAGNETOMETER ARRAY: A CASE STUDYSULZBACHER H; BAUMJOHANN W; POTEMRA TA et al.1980; J. GEOPHYS.; DEU; DA. 1980; VOL. 48; NO 1; PP. 7-17; BIBL. 2 P.Article

CALCUL DE LA LARGEUR ET DE LA DENSITE DE COURANT DE L'ELECTROJETOL GI.1980; TRUDY ARKTICH. ANTARKTICH. NAUCHNO-ISSLEDOVAT. INST. LENINGRAD; SUN; DA. 1980; NO 366; PP. 105-110; BIBL. 5 REF.Article

ON AURORAL ELECTROJET CURVATURE AND THE INTERPRETATION OF AZIMUTH-SCAN, RADAR DOPPLER DATA.BREKKE A; TSUNODA RT; BARON MJ et al.1977; RADIO SCI.; U.S.A.; DA. 1977; VOL. 12; NO 1; PP. 141-149; BIBL. 28 REF.Article