Use for cylindrical radius, to distinguish it from spherical radius . In cylindrical coordinates , the azimuthal angle is measured from positive in the horizontal plane:
Here and .
In spherical polar coordinates , take as the polar angle from positive and use the same azimuthal angle :
The ranges are , and . The radial direction has horizontal projection of length , which explains the extra factor in . The azimuth is undefined on the polar axis, and both angles are nonunique at the origin; these are coordinate degeneracies rather than geometric singularities.
Figure 1.
Cylindrical and spherical polar coordinates; the spherical polar angle is measured from positive z.
The same point and its projection onto the horizontal plane are shown in both panels. The cylindrical radius is the projection length; the spherical radius is the distance from the origin. Details.
On the unit upper hemisphere, use spherical coordinates with and . The surface mass density is , while the surface area element is . Thus the total mass is
The answer is in the mass units implicit in the specified unit radius and density law. A useful geometric check is that on the unit hemisphere equals the area element of its vertical projection onto the horizontal unit disc, whose area is .
This is a scalar surface integral, not an oriented flux. Split the whole closed surface into the bottom disc, curved side and tilted top; shared edge curves have zero surface area.
On the bottom, and the integrand is . Its integral over the symmetric disc vanishes by oddness:
On the top, , so . The graph has , , giving . Hence
For the side, let and parametrize by , with . The surface area element is . Thus
Adding all three pieces gives
The tilted top remains above the bottom everywhere because . The calculation is an instance of a scalar surface integral over a cylinder with one tilted cap; reversing a surface orientation would not change any of its terms.

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