Pascal and Francis Bibliographic Databases

Help

Search results

Your search

au.\*:("TRIVEDI NB")

Document Type [dt]

A-Z Z-A Frequency ↓ Frequency ↑
Export in CSV

Publication Year[py]

A-Z Z-A Frequency ↓ Frequency ↑
Export in CSV

Discipline (document) [di]

A-Z Z-A Frequency ↓ Frequency ↑
Export in CSV

Results 1 to 14 of 14

  • Page / 1
Export

Selection :

  • and

COMPARISON OF EQUATORIAL ELECTROJET CHARACTERISTICS AT HUANCAYO AND EUSEBIO (FORTALEZA) IN THE SOUTH AMERICAN REGIONKANE RP; TRIVEDI NB.1982; JOURNAL OF ATMOSPHERIC AND TERRESTRIAL PHYSICS; ISSN 0021-9169; GBR; DA. 1982; VOL. 44; NO 9; PP. 785-793; BIBL. 15 REF.Article

IMPLICATION OF Z VARIATION DURING A NEAR NOON EQUATORIAL COUNTERELECTROJET ON MARCH 6, 1967 IN THE INDIAN ZONEKANE RP; TRIVEDI NB.1980; J. GEOPHYS. RES.; ISSN 0022-1406; USA; DA. 1980; VOL. 85; NO A9; PP. 4705-4710; BIBL. 9 REF.Article

HORIZONTAL GEOMAGNETIC FIELD VARIATIONS AT LOW LATITUDE IN SOUTH ATLANTIC MAGNETIC ANOMALYKAUSHIKA ND; TRIVEDI NB.1972; PURE APPL. GEOPHYS.; SWITZ.; DA. 1972; VOL. 99; NO 7; PP. 99-107; BIBL. 7 REF.Serial Issue

ESPECTRO DE POTENCIA DO CAMPO GEOMAGNETICO PELO METODO DA ENTROPIA MAXIMA = SPECTRE D'INTENSITE DU CHAMP GEOMAGNETIQUE PAR LA METHODE D'ENTROPIE MAXIMALEKANTOR IJ; TRIVEDI NB.1980; REV. BRAS. FIS.; ISSN 0374-4922; BRA; DA. 1980; VOL. 10; NO 3; PP. 569-595; ABS. ENG; BIBL. 2 P.Article

COMPARISON OF MAXIMUM ENTROPY SPECTRAL ANALYSIS (MESA) AND LEAST-SQUARES LINEAR PREDICTION (LSLP) METHODS FOR SOME ARTIFICIAL SAMPLES = COMPARAISON ENTRE L'ANALYSE SPECTRALE DE L'ENTROPIE MAXIMALE (MESA) ET LA METHODE DE PREVISION LINEAIRE PAR MOINDRES CARRES (LSLP) POUR QUELQUES ECHANTILLONS ARTIFICIELSKANE RP; TRIVEDI NB.1982; GEOPHYSICS; ISSN 0016-8033; USA; DA. 1982-12; VOL. 47; NO 12; PP. 1731-1736; BIBL. 18 REF.; 1 TAB. ; ILL.Article

CONFINEMENT OF EQUATORIAL COUNTER ELECTROJETS TO RESTRICTED LONGITUDESKANE RP; TRIVEDI NB.1981; J. GEOMAGN. GEOELECTR.; ISSN 0022-1392; JPN; DA. 1981; VOL. 33; NO 6; PP. 379-382; BIBL. 12 REF.Article

STUDIES OF SUDDEN CHANGES IN H AND Z AT EQUATORIAL STATIONS IN THE INDIAN ZONE.TRIVEDI NB; RASTOGI RG.1968; ANN. GEOPHYS.; FRA; 1968, VOL. 24, NUM. 0004, P. 1037 A 1043Miscellaneous

ARE THE EQUATORIAL ELECTROJET AND COUNTERELECTROJET CENTERED INVARIABLY ON THE DIP EQUATOR.KANE RP; TRIVEDI NB.1982; J. ATMOS. TERR. PHYS.; ISSN 0021-9169; GBR; DA. 1982; VOL. 44; NO 4; PP. 301-304; BIBL. 27 REF.Article

CENTRAL PLANE OF THE RING CURRENT RESPONSIBLE FOR GEOMAGNETIC DISTURBANCE IN THE SOUTH AMERICAN REGIONKANE RP; TRIVEDI NB.1981; ANN. GEOPHYS.; ISSN 0003-4029; FRA; DA. 1981; VOL. 37; NO 2; PP. 271-280; ABS. FRE; BIBL. 22 REF.Article

EQUATORIAL ENHANCEMENT OF DP2 FLUCTUATIONSKANE RP; TRIVEDI NB.1980; J. GEOMAGN. GEOELECTR.; ISSN 0022-1392; JPN; DA. 1980; VOL. 32; NO 11; PP. 683-690; BIBL. 12 REF.Article

INFLUENCE OF NORTHERN AND SOUTHERN HEMISPHERE SQ CURRENT SYSTEMS ON EQUATORIAL MAGNETIC VARIATIONSKANE RP; TRIVEDI NB.1980; J. ATMOSPH. TERRESTR. PHYS.; GBR; DA. 1980; VOL. 42; NO 4; PP. 303-305; BIBL. 15 REF.Article

ENHANCED ELECTRON PRECIPITATION IN BRAZILIAN MAGNETIC ANOMALY IN ASSOCIATION WITH SUDDEN COMMENCEMENTMARTIN IM; RAI DB; DA COSTA JM et al.1972; NATURE PHYS. SCI.; G.B.; DA. 1972; VOL. 240; NO 100; PP. 84-86; BIBL. 4REF.Serial Issue

MAGNETOTELLURIC MEASUREMENTS AT EUSEBIO, AN EQUATORIAL STATION = MESURES MAGNETOTELLURIQUES A EUSEBIO, UNE STATION EQUATORIALETRIVEDI NB; DE SOUZA EG; DE PAULA ER et al.1981; PHYS. EARTH PLANET. INTER.; ISSN 0031-9201; NLD; DA. 1981; VOL. 25; NO 3; PP. 241-244; BIBL. 9 REF.; ILL.Article

ENHANCED LOW-ENERGY GAMMA RAYS AT BALLOON ALTITUDE IN THE BRAZILIAN MAGNETIC ANOMALY.MARTIN IM; RAI DB; PALMEIRA RAR et al.1974; NATURE; G.B.; DA. 1974; VOL. 252; NO 5478; PP. 25-27; BIBL. 5 REF.Article

  • Page / 1