Question

Почему над северным Ледовитым океаном образуются и континентальные,и морские воздушные массы?​

Answer 1

Ответ:

Потому, что морские воздушные массы формируются за счет испарения воды с поверхности океана. Северный Ледовитый океан почти весь покрыт льдом и, поэтому, вода с его поверхности не испаряется.

Answer 2

Formation of Continental and Maritime Air Masses over the Arctic Ocean

The formation of both continental and maritime air masses over the Arctic Ocean can be attributed to several factors.

1. Geographical Location: The Arctic Ocean is surrounded by landmasses, including the northern parts of North America, Europe, and Asia. This geographical configuration allows for the formation of both continental and maritime air masses.

2. Continental Air Masses: Continental air masses form over large land areas, such as the Arctic tundra and the Siberian and Canadian Arctic regions. These air masses are characterized by their dryness and low humidity. Continental air masses over the Arctic Ocean are influenced by the cold temperatures and the lack of moisture from the surrounding landmasses.

3. Maritime Air Masses: Maritime air masses form over large bodies of water, such as the Arctic Ocean. These air masses are characterized by their high humidity and relatively mild temperatures. Maritime air masses over the Arctic Ocean are influenced by the moisture and warmth from the ocean surface.

4. Air Mass Interactions: The interaction between continental and maritime air masses over the Arctic Ocean leads to the formation of both continental and maritime air masses. When cold continental air masses move over the relatively warmer ocean surface, they can pick up moisture and become maritime air masses. Conversely, when maritime air masses move over the colder landmasses, they can lose moisture and become continental air masses.

It is important to note that the formation of air masses is a complex process influenced by various factors, including temperature, humidity, wind patterns, and the characteristics of the surrounding land and water bodies. The specific details of air mass formation over the Arctic Ocean can vary depending on the time of year, prevailing weather patterns, and other atmospheric conditions.