Lambert Conic Conformal (2SP Michigan)
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Lambert Conic Conformal (2SP Michigan) Open
Coordinate Operation Method Details [VALID]
Name: Lambert Conic Conformal (2SP Michigan)
Code: 1051
Operation is Reversible: Yes
Formula: Note: These formulas have been transcribed from EPSG Guidance Note #7-2. Users are encouraged to use that document rather than the text which follows as reference because limitations in the transcription will be avoided.

To derive the projected Easting and Northing coordinates of a point with geographical coordinates (lat,lon) the formulas for the one standard parallel case are:

E = EF + r sin(theta)
N = NF + rF - r cos(theta)
where
m = cos(lat)/(1 - e^2 sin^2(lat))^0.5 for m1, lat1, and m2, lat2 where lat1 and lat2 are the latitudes of the two standard parallels.
t = tan(pi/4 - lat/2)/[(1 - e sin(lat))/(1 + e sin(lat))]^(e/2) for t1, t2, tF and t using lat1, lat2, latF and lat respectively.
n = (loge(m1) - loge(m2))/(loge(t1) - loge(t2))
F = m1/(n t1^n)
r = a K F t^n for rF and r, where rF is the radius of the parallel of latitude of the false origin and K is the ellipsoid scaling factor.
theta = n(lon - lon0)

The reverse formulas to derive the latitude and longitude of a point from its Easting and Northing values are:

lat = pi/2 - 2atan{t'[(1 - esin(lat))/(1 + esin(lat))]^(e/2)}
lon = theta'/n +lon0
where
r' = +/-[(E - EF)^2 + {rF - (N - NF)}^2]^0.5 , taking the sign of n
t' = (r'/(aKF))^(1/n)
theta' = atan2 [(E- EF),(rF - (N- NF))] (see GN7-2 implementation notes in preface for atan2 convention)
and n, F, and rF are derived as for the forward calculation.

Note that the formula for lat requires iteration. First calculate t' and then a trial value for lat* using
lat = π/2-2atan(t'). Then use the full equation for lat substituting the trial value into the right hand side of the equation. Thus derive a new value for lat. Iterate the process until lat does not change significantly. The solution should quickly converge, in 3 or 4 iterations.
Example: For Projected Coordinate System NAD27 / Michigan Central

Parameters:
Ellipsoid Clarke 1866, a = 6378206.400 metres = 20925832.16 US survey feet
1/f = 294.97870
then e = 0.08227185 and e^2 = 0.00676866

First Standard Parallel = 44°11'00"N = 0.771144641 rad
Second Standard Parallel = 45°42'00"N = 0.797615468 rad
Latitude False Origin = 43°19'00"N = 0.756018454 rad
Longitude False Origin = 84°20'00"W = -1.471894336 rad
Easting at false origin = 2000000.00 US survey feet
Northing at false origin = 0.00 US survey feet
Ellipsoid scaling factor = 1.0000382

Forward calculation for:
Latitude = 43°45'00.00"N = 0.763581548 rad
Longitude = 83°10'00.00"W = -1.451532161 rad

first gives :
m1 = 0.718295175 m2 = 0.699629151
t = 0.429057680 tF = 0.433541026
t1 = 0.424588396 t2 = 0.409053868
n = 0.706407410 F = 1.862317735
r = 21436775.51 rF = 21594768.40
theta = 0.014383991

Then Easting X = 2308335.75 US survey feet
Northing Y = 160210.48 US survey feet

Reverse calculation for same easting and northing first gives:
theta' = 0.014383991 r' = 21436775.51
t' = 0.429057680

Then Latitude = 43°45'00.000"N
Longitude = 83°10'00.000"W
Method
Parameters:
Parameter Name Parameter Code Sign reversal Parameter Description
Latitude of false origin 8821 No The latitude of the point which is not the natural origin and at which grid coordinate values false easting and false northing are defined.
Longitude of false origin 8822 No The longitude of the point which is not the natural origin and at which grid coordinate values false easting and false northing are defined.
Latitude of 1st standard parallel 8823 No For a conic projection with two standard parallels, this is the latitude of one of the parallels of intersection of the cone with the ellipsoid. It is normally but not necessarily that nearest to the pole. Scale is true along this parallel.
Latitude of 2nd standard parallel 8824 No For a conic projection with two standard parallels, this is the latitude of one of the parallels at which the cone intersects with the ellipsoid. It is normally but not necessarily that nearest to the equator. Scale is true along this parallel.
Easting at false origin 8826 No The easting value assigned to the false origin.
Northing at false origin 8827 No The northing value assigned to the false origin.
Ellipsoid scaling factor 1038 No Ratio by which the ellipsoid is enlarged so that survey observations are reduced to a surface above the ellipsoid surface.