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The Earth
Assumed to be a perfect sphere. Rotates east
Great Circle
A circle on the surface of a sphere whose centre and radius are those of the sphere itself. The plane of the great circle passes through the centre of the sphere and divides it into two equal parts.
Small circle
a circle on the surface of a sphere not coinciding with with the centre and radius of the sphere.
Meridian
Semi-great circles which join at the poles of the earth.
Parallel of latitude
Small circles on earth whose planes are parallel to the equator.
What are the units of Angular Measurement
Degrees, minutes, and seconds are units of angular measurement, both as angles at the centre of the circle and as length along the circumference. Each degree has 60 equal minutes divided into 60 equal seconds
Latitude
Angular distance between its place and the equator measured along a meridian
Facts about lines of latitude
Known as parallels
Run in an east-west direction
Measure distance north or south from equator
Are parallel to eachother
Cross the prime meridian at right angles
Lie in planes that cross the earth’s axis at right angles
Get shorter towards the poles with only the equator being a great circle
Longitude
Angular distance between a meridian and the prime meridian (Greenwich UK)
Facts about lines of longitude
Known as meridians
Run in a north-south direction
Measure distance east or west of prime meridian
Are furthest apart at the equator and meet at the poles
Cross the equator at right angles
Lie in planes that pass through the earth’s axis
Are equal in length
Are halves of great circles
Recording Lat and Long
Latitude coordinate in degrees and minutes is written first and is followed by longitude
Maps
A map is a small-scale flat surface representation of some portion of the earth’s surface.
The only true undistorted picture of the earth’s surface is to depict it on a globe
Qualities of Ideal Map
Conformality
Constant Scale
Correct Area
Orthomorphism
Rhumb lines as straight lines
Great circles as straight lines
Conformality
The correct representation of angles.
To possess conformality, a map must have: meridians and parallels intersecting at right angles, and scale expansion along the meridian equal to scale expansion along the parallel at any point
Constant scale
The correct scale at all points in all directions. This is impossible because of the basic difficulty of flattening a spherical surface.
Correct area
This can be achieved, but when areas are shown correctly, directions and shapes are distorted. Correct area also sacrifices conformality.
Orthomorphism
Correct shape. To be orthomorphic, a map would have to be conformal and have constant scale.
Rhumb lines as straight lines
Lines on a chart which intersect all meridians at the same angle, so parallels and meridians. To possess this property, a map must have meridians as parallel straight lines and at the same time be conformal. Mercator fulfills both.
Great circles as straight lines
Very desirable, great circle represents the shortest distance between two points.
Map Projections
The method by which the latitudes and longitudes of locations on the surface of a sphere are transferred to a plane (flat surface).
Always involves distortion.
Types of projections used in air navigation
Cylindrical and conic
Cylindrical Projections
Wrap a sheet of paper around the globe in a cylinder and transfer the geographic features onto it. To achieve projection, the graticule would be rectangular, the cylinder tangent to one line on the globe or intersects two lines of the globe.
Mercator Projection
A cylinder of paper around the equator of a globe map and projected the graticule of the earth onto the cylinder.
Large-scale expansion towards the poles
Has straight meridians and parallels that intersect at right angles
scales can be used to measure distances and are only true along equator or at two standard parallels equidistant at the equator.
Used for navigation for maps of equatorial regions.
Transverse Mercator
Rotated 90° so that it is tangential to the globe along a meridian instead of the equator
Any meridian may be the central meridian based on the area being mapped
The meridians and parallels intersect at right angles.
Scale is correct along the central meridian and is expanded elsewhere.
However, scale errors can be considered to be negligible on any one sheet.
Shapes are preserved, but areas are distorted; the degree of distortion increases with distance from the central meridian.
Great circles are approximate straight lines, and rhumb lines are curved concave to the nearer pole.
Adjoining north/south projections fit each other.
Lambert Conformal
is used in the preparation of ICAO (International Civil Aviation Organization) World Aeronautical Charts which are in common use by the Canadian Forces. This projection makes a good topographical or map-reading map for higher levels, where there is less detail but a much greater field of vision. The Lambert conformal is a modified conical projection which uses two standard parallels to reduce scale errors.
Map Scale
the ratio between a given length on the map and the actual distance on the earth
Three methods of showing scale
A statement in words
A representative fraction where one unit on the map is equivalent to a number of units on earth
A graduated line
Large Scale
Up to 1:250 000
Covers small areas in large amount of detail
Low-level navigation and target identification
Medium scale
1:500 000
Covers larger area with reasonable amount of detail
Medium-level navigation
Small Scale
1:1 000 000
Covers largest area with smallest amount of detail
Higher-level navigation
Map Relief
Representation of changes in elevation of the earth’s surface on a flat plane or map
Methods of showing map relief
Contour lines
Layer tinting
Spot heights
Hachures
Shading
Aeronautical Signs and Symbols
Aeronautical maps depict information to aircrew by the use of signs or symbols. The guide on the back or along the border of each map contains a complete explanation of all signs and symbols.