Geography Reference
In-Depth Information
β Φ + 3
256 E 4 (12 Φ − 8 sin 2 Φ + sin 4 Φ )+O( E 6 ) +
8 E 2 (2 Φ − sin 2 Φ )+ 15
×
(F.28)
ln 1+ E sin Φ
1
,
+ α
4 E
2 E sin Φ
E sin Φ +
E 2 sin 2 Φ
1
1
1
f ( Φ ) =
α + β
αy gL + βy gSF ,
f 1 ( Φ )=
α + β ( αy gL + βy gSF ) ,
(F.29)
cos Φ
y gL ( Φ )= A (1
E 2 )
(1 − E 2 sin 2 Φ ) 2 = A 1 N ( Φ ) M ( Φ )cos Φ,
E 2 )
A (1
y gSF ( Φ )=
E 2 sin 2 Φ ) 3 / 2 = M ( Φ ) ,
(F.30)
(1
1
f ( Φ ) =
x = x ( Λ, Φ )= N ( Φ ) M ( Φ )cos ΦΛ
N ( Φ ) M ( Φ )cos ΦΛ ( α + β )
αA 1 N ( Φ ) M ( Φ )cos Φ + βM ( Φ ) =
( α + β ) A cos Φ
α cos Φ + β 1
=
Λ.
(F.31)
E 2 sin 2 Φ
Thus,wehaveprovenLemma F.5 .
Lemma F.5 (Vertical mean of the generalized Lambert projection and of the generalized Sanson-
Flamsteed projection of the biaxial ellipsoid E
2 A,B ).
The vertical mean of the generalized Lambert projection and of the generalized Sanson-Flamsteed
projection of the biaxial ellipsoid leads to the equiareal mapping of pseudo-cylindrical type rep-
resented by ( F.32 ).
( α + β ) A cos Φ
α cos Φ + β 1
x = x ( Λ, Φ )=
Λ,
E 2 sin 2 Φ
E 2 )
α + β
A (1
y = y ( Φ )
×
(F.32)
β Φ + 3
8 sin 2 Φ + sin 4 Φ )+O( E 6 ) +
sin 2 Φ )+ 15
8 E 2 (2 Φ
256 E 4 (12 Φ
×
ln 1+ E sin Φ
1
.
+ α
4 E
2 E sin Φ
E sin Φ +
E 2 sin 2 Φ
1
End of Lemma.
The second variant of mixed equiareal mapping of the biaxial ellipsoid onto the plane is gen-
erated as weighted mean of the horizontal coordinates
{
x gL ,x gSF }
with respect to the gen-
eralized Lambert coordinate x gL (
( F.21 )) and the generalized Sanson-Flamsteed coordinate
x gSF (
( F.23 )). In contrast, the vertical coordinate y is constructed from the postulate of equiareal
pseudo-cylindrical mapping equations of the type ( F.20 ).
Definition F.6 (Equiareal mapping of pseudo-cylindrical type: horizontal coordinate mean).
An equiareal mapping of pseudo-cylindrical type of the biaxial ellipsoid is called horizontal coor-
dinate mean if ( F.33 )holdswhere α and β are weight coecients.
 
Search WWH ::




Custom Search