Schmucker, 1970 (Scripps) - MTNet
Schmucker, 1970 (Scripps) - MTNet
Schmucker, 1970 (Scripps) - MTNet
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
126 Bulletin, <strong>Scripps</strong> Institution of Oceanography<br />
g. Induction program SHELCO (sec. 5.8).<br />
Evaluation of (5. 60)to determine the ratio of internal to external parts<br />
above a conductive shell and a layered core.<br />
h. Induction program NONUNI for nonuniform thin sheets above perfect<br />
conductor (sec. 6.3).<br />
Relaxation process to determine the anomalous current distribution<br />
within and the anomalous field distribution above a total conductivity profile,<br />
given at n :;:: 100 equidistant points. The total conductivity merges near the<br />
ends of the profiles into constant values which are not necessarily equal(sec.<br />
7.3). The numerical integrations of (6.8-11) are performed by the subroutines<br />
PRICE, CORE, and KERTZ. Various options exist to simulate the<br />
distant field distribution by suitable "analytical tails. "<br />
i. Internal field-line program LAPLAC (sec. 6.6).<br />
Downward extension of a given 2 -dimensional field distribution, given<br />
at n :;:: 720 equidistant points, according to (6.20). The field is developed into<br />
a series of m :;:: 24 spatial harmonics (subr. HARMOA), which after multiplication<br />
with the exponential depth factor for a certain subsurface level are<br />
converted again into the field distribution at that level (subr. SYNTHE).<br />
j. Conformal mapping programs MODEL 1, 2, 3 (sec. 6.7).<br />
Transformation of rectangular grids from the z-plane into the w-plane<br />
according to the mapping functions (6.23, 24, 26); to be used in conjunction<br />
with the programs FLDMD 1, 2, 3 to determine the transfer values hH' zH<br />
in the w-plane according to (6.22).
Change language