Global oscillations at low frequency from the SOHO mission (GOLF)

被引:241
作者
Gabriel, AH
Grec, G
Charra, J
Robillot, JM
Cortes, TR
TurckChieze, S
Bocchia, R
Boumier, P
Cantin, M
Cespedes, E
Cougrand, B
Cretolle, J
Dame, L
Decaudin, M
Delache, P
Denis, N
Duc, R
Dzitko, H
Fossat, E
Fourmond, JJ
Garcia, RA
Gough, D
Grivel, C
Herreros, JM
Lagardere, H
Moalic, JP
Palle, PL
Petrou, N
Sanchez, M
Ulrich, R
VanderRaay, HB
机构
[1] UNIV NICE, DEPT ASTROPHYS, CNRS URA 709, F-06034 NICE, FRANCE
[2] OBSERV UNIV BORDEAUX 1, F-33270 FLOIRAC, FRANCE
[3] INST ASTROFIS CANARIAS, E-38205 LA LAGUNA, SPAIN
[4] CE SACLAY, DAPNIA, DSM, SERV ASTROPHYS, F-91191 GIF SUR YVETTE, FRANCE
[5] SERV AERON, F-91371 VERRIERES LE BUISSON, FRANCE
[6] OBSERV COTE AZUR, LAB CASSINI, CNRS URA1362, F-06304 NICE, FRANCE
[7] UNIV CAMBRIDGE, DEPT APPL MATH & THEORET PHYS, CAMBRIDGE, ENGLAND
[8] UNIV CALIF LOS ANGELES, DEPT ASTRON, LOS ANGELES, CA 90024 USA
[9] UNIV BIRMINGHAM, DEPT PHYS, BIRMINGHAM B15 2TT, W MIDLANDS, ENGLAND
关键词
sun; helioseismology;
D O I
10.1007/BF00733427
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The GOLF experiment on the SOHO mission aims to study the internal structure of the sun by measuring the spectrum of global oscillations in the frequency range 10(-7) to 10(-2) Hz. Both p and g mode oscillations will be investigated, with the emphasis on the low order long period waves which penetrate the solar core. The instrument employs an extension to space of the proven ground-based technique for measuring the mean line-of-sight velocity of the viewed solar surface. By avoiding the atmospheric disturbances experienced from the ground, and choosing a non-eclipsing orbit, GOLF aims to improve the instrumental sensitivity limit by an order of magnitude to 1 mm s(-1) over 20 days for frequencies higher than 2.10(-4) Hz. A sodium vapour resonance cell is used in a longitudinal magnetic field to sample the two wings of the solar absorption line. The addition of a small modulating field component enables the slope of the wings to be measured. This provides not only an internal calibration of the instrument sensitivity, but also offers a further possibility to recognise, and correct for, the solar background signal produced by the effects of solar magnetically active regions. The use of an additional rotating polariser enables measurement of the mean solar line-of-sight magnetic field, as a secondary objective.
引用
收藏
页码:61 / 99
页数:39
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