MODEL ATMOSPHERE CALCULATION OF SOLAR OBLATENESS

被引:19
作者
DURNEY, BR
ROXBURGH, IW
机构
[1] High Altitude Observatory, Boulder, CO
[2] Department of Mathematics, Queen Mary College
关键词
D O I
10.1038/221646b0
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Dicke and Goldenberg1 measured the difference between the polar and the equatorial flux coming from the limb of the Sun (ΔF), and inferred that the surface of equal potential at the limb is oblate by 35 km. The Sun thus has a quadrupole moment due to a rapidly rotating interior, producing a perihelion shift of Mercury of 3.4 s of arc century-1. Agreement between the value predicted by general relativity and the observed perihelion shift of Mercury is thus destroyed. One of us2 has criticized the Dicke and Goldenberg interpretation and has suggested that the flux difference is due to a stronger stabilization of convection, by rotation, at the pole. © 1969 Nature Publishing Group.
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页码:646 / &
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