Nature, Volume 429Sir Norman Lockyer Macmillan Journals Limited, 2004 - Electronic journals |
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Page 169
... core through Earth's history1 - 5 . Here we use a set of numerical dynamo models to derive scaling relations between the core's characteristic dissipation time and the core's magnetic and hydrodynamic Reynolds numbers- dimensionless ...
... core through Earth's history1 - 5 . Here we use a set of numerical dynamo models to derive scaling relations between the core's characteristic dissipation time and the core's magnetic and hydrodynamic Reynolds numbers- dimensionless ...
Page 171
... core conditions reason- ably well . In order to calculate the dissipation of the geodynamo , we must know Rm and the total magnetic energy in the core . We use the dependence of the secular variation on Rm in our dynamo models to ...
... core conditions reason- ably well . In order to calculate the dissipation of the geodynamo , we must know Rm and the total magnetic energy in the core . We use the dependence of the secular variation on Rm in our dynamo models to ...
Page 596
... core ever retrieved . The ice was drilled at Dome C in the East Antarctic ice sheet by a consortium called the European Project for Ice Coring in Antarc- tica ( EPICA ) . It has nearly doubled the age record for an ice core previously ...
... core ever retrieved . The ice was drilled at Dome C in the East Antarctic ice sheet by a consortium called the European Project for Ice Coring in Antarc- tica ( EPICA ) . It has nearly doubled the age record for an ice core previously ...
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