Subarctic phenomena

Arctic Phenomenon Aurora Aurora is very fascinated by people in the northern hemisphere. Aurora is influenced by many myths of northern culture. The first attempt to study the scientific origin of Aurora occurred in the 18th century when it was concluded that Aurora is related to magnetism. Aurora occurs at the high latitudes of the North Pole and the South Pole. The Arctic and Antarctic auroras are related and are named Aurora and Aurora. Aurora can be seen mainly in the high latitude area where the population of the northern hemisphere is small, but it can also be seen in the low latitude area.

The climate of the western Alaska relies heavily on the Bering Sea and Alaska Bay. The ocean climate of the South Arctic Arctic region and the North Arctic climate. Given the distance to the northern part of the area, the temperature is somewhat gentle. There are various rainfall in this area. The area from the north side of the Seward Peninsula to the Kobuk Valley (the area surrounding Kotzebue Sound) is technically a desert with annual rainfall less than 25 cm (10 inches). On the other hand, some places between Dillingham and Bethel have average rainfall of about 100 inches (250 cm).

In the subarctic climate there is little precipitation and the temperature of 1 to 3 months per year exceeds 10 ° C (50 ° F). Because of the cold winter, there are permafrost in most areas. Winter in the subarctic climate usually includes temperatures up to 6 months and the average temperature is less than 0 ° C (32 ° F). The desert is a form or region of a landscape with less precipitation. The deserts are usually maintained during daytime and nighttime and seasonal temperatures (depending on temperature during the day (maximum 45 ° C or 113 ° F for the summer) and temperatures at the lowest night (0 ° C or 32 ° F for the winter) The range becomes higher. It's because humidity is very low. Many deserts are formed by shadows of rain. Because the mountain hinders the moisture and precipitation path to the desert.