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By K. Knott (auth.), K. Knott, A. Durney, K. Ogilvie (eds.)

ISBN-10: 940099527X

ISBN-13: 9789400995277

ISBN-10: 9400995296

ISBN-13: 9789400995291

(Opening deal with of thirteenth ESLAB Symposium) With GEOS and ISEE occupying an immense a part of the ESA medical programme it used to be transparent a number of years in the past 'natural' foundation for the 1978 ESLAB Annual Symposium may be the early facts from those spacecraft. in the course of the 1976 assembly of the eu Geophysical Society in Amsterdam it turned obvious to me a lot wider neighborhood used to be and that during specific operating staff 2 of COSPAR used to be contemplating a GEOS consultation in the course of its 1978 assembly the following in Innsbruck. This used to be after all because it needs to be simply because GEOS have been followed because the reference spacecraft for the foreign Magnetospheric research. After a few discussions with COSPAR and with the organizers of the STP Symposium which was once held right here final week we felt that during the curiosity of shopper kinfolk and following solid logic we should always hand over a few of our independence in 1978 and merge our Symposium with COSPAR. i'd gratefully recognize the co-operation of COSPAR's operating staff 2 chairman and vice-chairman, the lively help of the President of COSPAR and the 'gentleman's contract' with the STP programme committee which prepared that the hot ISEE and GEOS effects have been routed to this Symposium instead of to the STP. i've got pointed out how we got here to have this joint Symposium. probably I should still inform you too how we got here as regards to having no Symposium.

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And Smith, E. : 1970,1. Geophys. Res. 75, 755. , (to be published). Singer, H. , Russell, C. , Kivelson, M. , Greenstadt, E. , and Olson, J. : 1977, Geophys. Res. Letters 4, 377. Taylor, W. W. L. and Lyons, L. : 1976,1. Geophys. Res. 81, 6177. Taylor, W. W. , Parady, B. , L. : 1975, 1. Geophys. Res. 80, 1271. K. Abstract. This paper is concerned mainly with the information which can be extracted from frequency-time spectra in the VLF range. The instrument used is the correlator which has a good frequency resolution (50 Hz) and time resolution (30 ms) in one magnetic and one electric component simultaneously.

I • ~ B. 2 FS a: ~ 7. a: FIXED REFERENTIAL component RLZ) ~ 6. 0::: ~ 5. 5 ~ 4. J 3. 6 2. 1· O. 3 -1. -2. -3. -4. -5. (b) -6. 0 FREQUENCY (HZ) Fig. 1. Spectra of the three components of the ULF signal. 8°) along the spin axis. In spite of the despin system, the three components present a parasitic signal at the spin frequency F,. An emission at Fl appears on the B z component, whereas the energy in splitted into two signals at Fl ±F" on Bx and By. (b) Bv B R , and B z in a stationary frame of reference, BL and B R , being the circular components of opposite polarities.

L. and Heppner, J. :1977, 1. Geophys. Res. 32, 5155. Cummings, W. , DeFprest, S. , and McPherron, R. : 1978,1. Geophys. Res. 83, 697. , Young, D. , Wrenn, G. : 1978, Space Sci. Rev. 22,633. 25 346 A. PEDERSEN ET AL. : 1971, 'Problems of Electric Field Measurements from a Geostationary Satellite', ESRO SP-60, pp. 249-265. : 1972, Photon and Particle Interactions with Surfaces in Space, D. Reidel Pub!. , pp. 163-192. , McPherron, R. , and Russell, C. : 1976,1. Geophys. Res. 81, 5141. Lanzerotti, L.

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Advances in Magnetosperic Physics with GEOS-1 and ISEE by K. Knott (auth.), K. Knott, A. Durney, K. Ogilvie (eds.)

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