Geomagnetic secular variation generated by a tangentially geostrophic flow under the frozen-flux assumption - II. Sufficient conditions

被引:7
作者
Chulliat, A [1 ]
机构
[1] Florida State Univ, Inst Geophys Fluid Dynam, Tallahassee, FL 32306 USA
关键词
core flow; frozen-flux; geomagnetism; geostrophic; secular variation;
D O I
10.1111/j.1365-246X.2004.02216.x
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Two assumptions are often made when computing Earth's core surface flows from geomagnetic data: the frozen- flux assumption and the tangentially geostrophic assumption. These assumptions impose some integral constraints on the geomagnetic field on secular timescales. It has been shown in the first paper of this series that all known integral constraints could actually be deduced from a single set of curvilinear integral constraints on the secular variation along level curves of zeta = B-r /cos theta at the core surface. In the present paper, these particular constraints are further proved to be sufficient conditions for the geomagnetic secular variation to be generated by a tangentially geostrophic flow under the frozen- flux assumption. This result means that no other independent constraint can be found and makes it possible to attempt building geomagnetic models consistent with both the frozen- flux and the tangentially geostrophic assumptions. Also, the complete set of tangentially geostrophic flow solutions of the induction equation under the frozen- flux assumption is exhibited. These solutions are amenable to direct numerical computation.
引用
收藏
页码:537 / 552
页数:16
相关论文
共 19 条
[1]   POLOIDAL AND TOROIDAL FIELDS IN GEOMAGNETIC-FIELD MODELING [J].
BACKUS, G .
REVIEWS OF GEOPHYSICS, 1986, 24 (01) :75-109
[3]   THE REGION ON THE CORE MANTLE BOUNDARY WHERE A GEOSTROPHIC VELOCITY-FIELD CAN BE DETERMINED FROM FROZEN-FLUX MAGNETIC DATA [J].
BACKUS, GE ;
LEMOUEL, JL .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1986, 85 (03) :617-628
[4]   GEOMAGNETIC-FIELD ANALYSIS .4. TESTING THE FROZEN-FLUX HYPOTHESIS [J].
BLOXHAM, J ;
GUBBINS, D .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1986, 84 (01) :139-152
[5]   TIME-DEPENDENT MAPPING OF THE MAGNETIC-FIELD AT THE CORE-MANTLE BOUNDARY [J].
BLOXHAM, J ;
JACKSON, A .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1992, 97 (B13) :19537-19563
[6]   Local computation of the geostrophic pressure at the top of the core [J].
Chulliat, A ;
Hulot, G .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 2000, 117 (1-4) :309-328
[7]   Geomagnetic secular variation generated by a tangentially geostrophic flow under the frozen-flux assumption - I. Necessary conditions [J].
Chulliat, A ;
Hulot, G .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2001, 147 (02) :237-246
[8]  
Gubbins D., 1987, GEOMAGN AERON, V2, P1
[9]  
Hills R.G., 1979, THESIS NEW MEXICO ST
[10]   Small-scale structure of the geodynamo inferred from Oersted and Magsat satellite data [J].
Hulot, G ;
Eymin, C ;
Langlais, B ;
Mandea, M ;
Olsen, N .
NATURE, 2002, 416 (6881) :620-623