it will move westward because the Earth rotates east
The Earth's rotation turns the polar high pressure systems westward as they move from the poles (westerlies), and the subtropical high pressure systems eastward as they move toward the equator (tropical easterlies).
Geostrophic wind is not possible at the equator because the Coriolis force is negligible at the equator due to the Earth's rotation, resulting in a weak pressure gradient force dominating. This weak Coriolis force prevents the balance between pressure gradient force and Coriolis force required for geostrophic winds.
This is due to the Earth's rotation causing a Coriolis effect, which deflects the trajectory of moving objects. As the cannonball travels towards the equator from a northern latitude, it retains some of the eastward velocity from the Earth's rotation, causing it to land west of its intended longitude.
This is impossible. A cyclone cannot cross the equator. The reason why this cannot happen is because the Coriolis Force reduces to almost nothing at the equator. The effect on a cyclone would be to cause it to dissipate.
The Coriolis effect has the least effect on winds in equatorial regions and the most effect on winds in polar regions. Coriolis effect deflects winds to the right of their initial direction in the northern hemisphere and left of their initial direction in the southern hemisphere.
The Earth's rotation turns the polar high pressure systems westward as they move from the poles (westerlies), and the subtropical high pressure systems eastward as they move toward the equator (tropical easterlies).
The Coriolis effect is zero at the equator because the rotation of the Earth is perpendicular to the direction of motion at the equator, resulting in no deflection of moving objects.
Turn towards the right
Geostrophic wind is not possible at the equator because the Coriolis force is negligible at the equator due to the Earth's rotation, resulting in a weak pressure gradient force dominating. This weak Coriolis force prevents the balance between pressure gradient force and Coriolis force required for geostrophic winds.
Equator due to the trade winds pushing the surface waters westward. This creates the Equatorial Counter Current, which flows eastward at the surface.
The Coriolis effect is weakest at the equator because the effect is a result of the Earth's rotation, and the rotational speed is slower at the equator compared to higher latitudes. As a result, the Coriolis force is less pronounced near the equator.
The Coriolis Effect is strongest at the poles and weakest at the equator. This is because the effect is influenced by the rotation of the Earth, and the rotational speed is greatest at the poles and slowest at the equator.
westward
This is due to the Earth's rotation causing a Coriolis effect, which deflects the trajectory of moving objects. As the cannonball travels towards the equator from a northern latitude, it retains some of the eastward velocity from the Earth's rotation, causing it to land west of its intended longitude.
Hurricanes cannot form at the equator because the Coriolis effect, which is needed for their formation, is too weak in that region. The Coriolis effect is a force caused by the Earth's rotation that helps hurricanes spin and develop.
This is impossible. A cyclone cannot cross the equator. The reason why this cannot happen is because the Coriolis Force reduces to almost nothing at the equator. The effect on a cyclone would be to cause it to dissipate.
The Coriolis effect has the least effect on winds in equatorial regions and the most effect on winds in polar regions. Coriolis effect deflects winds to the right of their initial direction in the northern hemisphere and left of their initial direction in the southern hemisphere.