Air masses moving in the northern hemisphere are turned westward from there original paths in the Westernlies.
Not necessarily. While cold air masses in the northern hemisphere often originate farther north than the areas they move into, they most often move westward, as they are usually brought in by westward-moving systems that rotate counterclockwise. In the southern hemisphere the air masses originate in the south and are associated with clockwise-rotating systems.
In the Northern Hemisphere, the original path of air masses typically begins over large land or ocean areas. For instance, polar air masses originate from polar regions, while tropical air masses form over warm tropical oceans. These air masses can move due to prevailing winds, such as the westerlies, and are influenced by the Coriolis effect, which causes them to curve as they travel. Consequently, their paths can vary significantly depending on factors like season and geographic features.
Continental polar air masses originate over cold, dry regions in the northern hemisphere, such as northern Canada and Siberia. These air masses form when cold air masses move southward from the polar regions and become isolated over land, leading to cooling and drying.
In the northern hemisphere, air masses typically move from west to east due to the predominant westerly winds and the Coriolis effect, which causes moving air to be deflected to the right. In contrast, in the southern hemisphere, air masses also move from west to east, but the Coriolis effect deflects them to the left. Additionally, the distribution of land and ocean influences the patterns and characteristics of air mass movement in both hemispheres. Overall, while the movement direction is similar, the specific dynamics can vary due to geographical and environmental factors.
moves most of them from the sw to ne. (always curving right in the northern hemisphere.)
Answer : Coriols effect
The Coriolis Force
In the Northern Hemisphere, air masses moving are turned westward from their original paths due to the Coriolis effect, which is caused by the rotation of the Earth. This deflection results in a general movement of air masses toward the right of their initial trajectory. Consequently, air masses originating from the tropics tend to shift westward, while polar air masses can also be influenced to move in a similar westward direction along certain latitudinal bands. This phenomenon plays a significant role in the formation of weather patterns and systems.
Not necessarily. While cold air masses in the northern hemisphere often originate farther north than the areas they move into, they most often move westward, as they are usually brought in by westward-moving systems that rotate counterclockwise. In the southern hemisphere the air masses originate in the south and are associated with clockwise-rotating systems.
In the Northern Hemisphere, the original path of air masses typically begins over large land or ocean areas. For instance, polar air masses originate from polar regions, while tropical air masses form over warm tropical oceans. These air masses can move due to prevailing winds, such as the westerlies, and are influenced by the Coriolis effect, which causes them to curve as they travel. Consequently, their paths can vary significantly depending on factors like season and geographic features.
The Southern Hemisphere generally has warmer average temperatures compared to the Northern Hemisphere due to greater amounts of ocean coverage and southward distribution of land masses.
Yes, approximately 68% of the Earth's land area is located in the northern hemisphere. The northern hemisphere contains the largest landmasses, including North America, Europe, and Asia.
The Coriolis Effect.
The Arctic is located in the northern hemisphere. It consists of the Arctic Ocean and the surrounding land masses of countries such as Canada, Russia, the United States, and others.
The Southern Hemisphere westerlies are more persistent and stronger than in the Northern Hemisphere because there are fewer land masses to disrupt their flow. In the Southern Hemisphere, the westerlies can travel more freely over the vast expanse of ocean, allowing them to maintain their strength and consistency. In contrast, in the Northern Hemisphere, the westerlies are slowed down and disrupted by land masses like North America and Eurasia.
Approximately 68.4% of the Earth's landmass is located in the northern hemisphere, while about 31.6% is in the southern hemisphere. The distribution of land between the two hemispheres is not equal due to the uneven arrangements of continents and land masses on Earth.
Both halves were effected, but most land masses are in the northern hemisphere so the effects were greater there.