Geoscience Reference
In-Depth Information
Accordingly, this may be written
OC AB =DC ABB 0 A 0 A .
(4-44)
Thus, the orthometric correction from A to B equals the dynamic correc-
tion over the loop ABB 0 A 0 A , a curious, but practically completely useless
relation equivalent to (4-41). ( Question: Why is this independent of γ 0 ?)
From (4-18), we find
= B
A
dn = B
g
γ 0
γ 0
g
γ 0
γ 0
DC AB
δn ,
A
DC A 0 A = A
A 0
g − γ 0
γ 0
dH = g A − γ 0
γ 0
(4-45)
H A ,
DC B 0 B = B
B 0
g
γ 0
γ 0
dH = g B
γ 0
H B ,
γ 0
where g A and g B are the mean values of gravity along the plumb lines of A
and B . Thus, the orthometric correction (4-41) becomes
OC AB = B
g
γ 0
γ 0
δn + g A
γ 0
g B
γ 0
H A
H B .
(4-46)
γ 0
γ 0
A
Here again we need the mean values of gravity along the plumb lines, g A and
g B ; γ 0 is an arbitrary constant for which we always take normal gravity at
45 latitude.
Accuracy
Let us first evaluate the effect on H of an error in the mean gravity g .From
H = C/g , we obtain by differentiation
C
g 2 δg =
H
g
δH =
δg.
(4-47)
Since g is about 1000 gal, we have, neglecting the minus sign, the simple
formula
= δg [mgal] H [km] ,
δH [mm]
(4-48)
the subscripts denoting the units; δH is the error in H ,causedbyanerror
δg in g .
For H =1km,
= δg [mgal] ,
δH [mm]
(4-49)
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