Question

Beginning with the underlying cause, rank the factors that contribute to global air circulation from most to least significant: (a) pressure differences, (b) temperature differences, (c) Coriolis force, (and) frictional force. Rank from most to least. To rank items as equivalent, overlap them.

Answer 1

The factors contributing to global air circulation, ranked from most to least significant, are temperature differences, pressure differences, Coriolis force, and frictional force.

Step-by-step explanation:

The factors that contribute to global air circulation can be ranked from most to least significant as follows:

1. Temperature differences: Variations in temperature create pressure differences, which in turn drive air circulation. Cold air is more dense and has higher pressure than warm air, so it tends to flow into regions of lower pressure.
2. Pressure differences: Differences in atmospheric pressure create variations in air density, which cause air to move from areas of high pressure to areas of low pressure. This movement sets the stage for global air circulation patterns.
3. Coriolis force: The Earth's rotation causes moving air to be deflected, creating the Coriolis force. In the Northern Hemisphere, this force deflects winds to the right, while in the Southern Hemisphere, it deflects winds to the left.
4. Frictional force: Friction between the air and Earth's surface slows down winds at the surface. It is the least significant factor contributing to global air circulation.

Learn more about Global air circulation

Answer 2

The factors which causes or contribute to global air circulation from most to least factors include the following:

(b) temperature differences

(a) pressure differences

(c) Coriolis force, (and) frictional force

Step-by-step explanation:

In the above listed factors, they have a great contribution to the air circulation in the world. For example, the temperature differences is one of the contributing factor due to the fact that, the areas with high temperature leads to air circulation towards the area with low temperature.