The two factors that determine the strength of the Coriolis effect are the rotation speed of the Earth and the latitude of the location. The effect is strongest at the poles and weakest at the equator due to the Earth's rotational speed and curvature.
The main factors that determine how much the wind bends are the wind speed, the density of the air, the presence of obstacles in the wind's path, and the Coriolis effect caused by the Earth's rotation. These factors can cause the wind to curve and change direction as it moves through the atmosphere.
Surface currents are primarily caused by the wind. As wind blows across the surface of the ocean, it creates friction and imparts energy to the water, causing it to move in the same direction as the wind. Other factors, such as the Coriolis effect and differences in water density, can also influence the direction and strength of surface currents.
it will bend to the west
The location, size, shape, and direction of surface current gyres are primarily determined by Earth's rotation, prevailing wind patterns, and the distribution of land masses and ocean basins. Coriolis effect, frictional drag on the ocean surface, and differences in temperature and salinity also play a role in shaping these gyres.
The Coriolis Effect is named after the French mathematician and engineer Gaspard-Gustave de Coriolis. He first described the effect in 1835, which explains the deflection of moving objects on the Earth's surface due to its rotation.
the Coriolis effect
The prevailing winds are set up by the Earth's rotation and the distribution of heat from the sun. Factors that influence their direction and strength include the Coriolis effect, pressure gradients, and the distribution of land and water on the Earth's surface.
Coriolis effect
The main factors that determine how much the wind bends are the wind speed, the density of the air, the presence of obstacles in the wind's path, and the Coriolis effect caused by the Earth's rotation. These factors can cause the wind to curve and change direction as it moves through the atmosphere.
continental deflections,global winds, coriolis effect
pressure differences, coriolis effect, friction
The Coriolis effect causes the polar easterlies to deflect to the west near the poles due to the Earth's rotation. This results in the wind flow from east to west in the upper atmosphere. The Coriolis effect influences the direction and strength of the polar easterlies, contributing to their characteristic eastward flow.
The three factors that control the path of a surface current are wind direction, the Earth's rotation (Coriolis effect), and the shape of the coastline or the presence of land masses. These factors influence the direction and strength of surface currents in the ocean.
It Flows with the coriolis effect. It Flows with the coriolis effect.
global winds, Coriolis effect, and continental deflection
Continental deflections,the Coriolis effect and global winds all effect surface ocean currents.
Surface currents are primarily caused by the wind. As wind blows across the surface of the ocean, it creates friction and imparts energy to the water, causing it to move in the same direction as the wind. Other factors, such as the Coriolis effect and differences in water density, can also influence the direction and strength of surface currents.