# Alaska grid

## Description

This projection was developed to provide a conformal map of Alaska with less scale distortion than other conformal projections. A set of mathematical formulas defines a conformal transformation between two surfaces (Snyder 1993).

## Projection method

Modified planar. This is a sixth-order equation modification of an oblique stereographic conformal projection on the Clarke 1866 spheroid. The origin is at 64° N, 152° W.

## Point of tangency

Conceptual point of tangency at 64° N, 152° W

## Linear graticules

None

## Properties

### Shape

Perfectly conformal

### Area

Varies approximately 1.2 percent over Alaska

### Direction

Local angles are correct everywhere.

### Distance

The minimum scale factor is 0.997 at approximately 62°30' N, 156° W. Scale increases outward from this point. Most of Alaska and the Aleutian Islands, excluding the panhandle, are bounded by a line of true scale. The scale factor ranges from 0.997 to 1.003 for Alaska, which is one-fourth the range for a corresponding conic projection (Snyder 1987).

## Limitations

Distortion becomes severe away from Alaska.

## Uses and applications

- Conformal mapping of Alaska as a complete state on the Clarke 1866 spheroid or NAD27
- Not optimized for use with other datums and spheroids

## Parameters

Supported in ArcInfo Workstation only. Projection-specific parameters are set by the software.