Meridians are typically shown as straight lines radiating out from the center point of the polar projection map. They converge at the poles and represent lines of longitude, which help to indicate direction and location on the map. These meridians help users navigate and understand the spatial relationships on the polar projection.
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72 number of meridians can be drawn on the globe at 5 degree interval
Meridians on a cylindrical projection appear as straight vertical lines on the map, while meridians on a globe are smooth curves meeting at the poles. The distortion of meridians increases as you move away from the equator on a cylindrical projection, making them seem more elongated.
they appear as straight lines.i needed help w this (?] too shoooot.aha,
On a globe, parallels and meridians meet at right angles only at the equator and the poles. On a Mercator projection map, all meridians intersect the equator at right angles, while parallels intersect meridians at right angles throughout the map.
i don’t know
Meridians are lines of longitude that are drawn from the North to South poles.
72 number of meridians can be drawn on the globe at 5 degree interval
Meridians on a cylindrical projection appear as straight vertical lines on the map, while meridians on a globe are smooth curves meeting at the poles. The distortion of meridians increases as you move away from the equator on a cylindrical projection, making them seem more elongated.
On a Mercator projection, meridians appear as straight, parallel lines running from top to bottom of the map, spaced evenly apart. This is because the Mercator projection is a cylindrical map projection that preserves straight lines of constant bearing, resulting in meridians being stretched vertically towards the poles.
they appear as straight lines.i needed help w this (?] too shoooot.aha,
yes
On a globe, parallels and meridians meet at right angles only at the equator and the poles. On a Mercator projection map, all meridians intersect the equator at right angles, while parallels intersect meridians at right angles throughout the map.
A polar projection of the earth shows a pole (north or south, depending on the projection) at the center of a circular map. The equator is the circumference of the circle.
Meridians on a globe get closer and eventually merge at the North and South Poles. On a map (a flat plane) the meridians are drawn parallel and there is distortion at the poles, most noticeable on a world map.
The polar regions are often represented using the azimuthal polar projection. This projection centers on one of the poles, allowing for an accurate depiction of the area surrounding it. It is particularly useful for navigation and for representing phenomena such as weather patterns in polar areas. The azimuthal polar projection distorts shapes and sizes further from the center, but provides a clear view of the polar regions themselves.
A globe can have 36 meridians drawn at 10-degree intervals. This is because meridians are lines of longitude that extend from the North Pole to the South Pole, and they are measured from 0 degrees (the Prime Meridian) to 360 degrees. Dividing the 360 degrees by 10 degrees gives 36 meridians.