As you move from the equator towards the poles, Earth's surface temperature generally decreases. This is primarily due to the curvature of the Earth, which causes sunlight to be more concentrated at the equator and more dispersed at higher latitudes. Additionally, the angle of sunlight strikes the surface at different latitudes, leading to variations in heating. Consequently, regions closer to the poles experience colder temperatures compared to those near the equator.
The distance between the longitudes decreases towards the poles. This is because the lines of longitude converge towards the poles, resulting in shorter distances between them as you move towards the North or South Pole.
The spacing of parallels decreases as you move towards the poles. This is because the lines of latitude converge towards the poles since the Earth's circumference decreases as you move away from the equator.
Latitude lines, which run parallel to the equator, represent circles around the Earth. As you move toward the poles, these circles become smaller due to the Earth's spherical shape. Consequently, the distance between each degree of latitude decreases, resulting in shorter lengths at higher latitudes compared to those near the equator. This geometric characteristic is fundamental to the Earth's curvature.
The Coriolis effect is caused by the rotation of the Earth. As the Earth rotates, objects traveling on its surface appear to be deflected due to the difference in speed of rotation at different latitudes. This effect is strongest at the poles and decreases towards the equator.
Latitudes are parallel lines that run east-west around the Earth, maintaining a constant distance from each other. However, they are not of the same size because the circumference of the Earth decreases as one moves from the equator towards the poles. At the equator, the latitude lines are the longest, while the lines near the poles become shorter until they converge at the poles themselves. This geometric relationship results in parallel lines that vary in length.
The deflection of wind due to the Coriolis effect is strongest at the poles and decreases towards the equator. This is because the Coriolis effect is most pronounced at higher latitudes where the rotational speed of the Earth is greatest.
As you move from the equator towards the poles, Earth's surface temperature generally decreases. This is primarily due to the curvature of the Earth, which causes sunlight to be more concentrated at the equator and more dispersed at higher latitudes. Additionally, the angle of sunlight strikes the surface at different latitudes, leading to variations in heating. Consequently, regions closer to the poles experience colder temperatures compared to those near the equator.
The distance between the longitudes decreases towards the poles. This is because the lines of longitude converge towards the poles, resulting in shorter distances between them as you move towards the North or South Pole.
high latitude is more towards the poles of the world such as north and south pole.
The spacing of parallels decreases as you move towards the poles. This is because the lines of latitude converge towards the poles since the Earth's circumference decreases as you move away from the equator.
Latitude lines, which run parallel to the equator, represent circles around the Earth. As you move toward the poles, these circles become smaller due to the Earth's spherical shape. Consequently, the distance between each degree of latitude decreases, resulting in shorter lengths at higher latitudes compared to those near the equator. This geometric characteristic is fundamental to the Earth's curvature.
The Coriolis effect is caused by the rotation of the Earth. As the Earth rotates, objects traveling on its surface appear to be deflected due to the difference in speed of rotation at different latitudes. This effect is strongest at the poles and decreases towards the equator.
The Coriolis effect increases with increasing latitude because the speed of rotation of the Earth is greatest at the equator and decreases towards the poles. This variation in rotational speed causes a greater deflection of moving objects at higher latitudes, resulting in a stronger Coriolis effect.
areas near the poles receive less solar energy per unit area.
As latitude increases, the temperature tends to decrease. This is because the amount of solar energy received decreases as you move away from the equator towards the poles. The angle at which sunlight hits the Earth's surface becomes more oblique at higher latitudes, resulting in less direct heating.
Biodiversity generally decreases with increasing latitude, as the number of species tends to decline towards the poles. In contrast, biodiversity increases with larger areas as larger habitats can support more diverse ecosystems and species. This is due to the availability of more niches and resources in larger areas.