Hair dryers in Greenland

A hair dryer is one of the most remarkable phenomena of Greenland's climate. Even in the middle of winter, a hair dryer can cause the temperature to rise by 30-40 degrees. The effect of phenolic winds is most strongly affected in the outer zone of the coast, especially in southwestern Greenland, where even in winter there is often no surface inversion due to the influence of warm waters of the West Greenland current. In the inner parts of the fjords, hair dryers are less common, as the lower layer of cold air here is more stable and prevents warm hair dryers from sinking to the earth's surface. But sometimes the movement of warm air flows is so rapid that the cold air is also involved in the movement and mixes with the upper layers.

The appearance of the hair dryer is preceded by the appearance of cirrus clouds over the glacier. Soon after, small clouds of snow, resembling clouds of smoke, appear on the tops of high mountain peaks near the edge of the glacier, blown off the slopes. There is a growing roar of the wind. After a while, a strong wind rises from the outer parts of the fjord. This is the so-called downwind, which is formed due to strong vortices in the warm air currents above the glacier. Then the wind changes: the hair dryer reaches the earth's surface and begins to blow in strong, sharp gusts. Fen is the most depressing wind on the island. Its speed sometimes drops to 60 miles per hour, but sometimes it suddenly increases to 125 miles. At airfields, it is necessary to secure all objects, such as boards, empty fuel barrels, because they can cause serious damage. Individual wind gusts can reach up to 320 km/h (88 m/sec).

A strong phenol is usually observed only on a relatively short stretch of the coast, but its occurrence is associated with large-scale circulation processes. Very often, the oceanic air passes over the glacier up to 500-800 km from one coast of Greenland to the other before descending in the form of a hairdryer. Sometimes the "incomplete" fens of western Greenland pass no less far, which arise in the front of cyclones moving north along Baffin Bay. In this case, oceanic air passes along the western slope of the glacier from south to north, sometimes without reaching its central parts. The air comes to the middle parts of the western coast even warmer than in the south, where it began to rise above the glacier, since due to condensation of moisture accompanied by precipitation of rain and snow over southern Greenland, its adiabatic heating during descent exceeds cooling during ascent. During the hair dryers in Jakobshavn, even in the middle of winter, the temperature rises to +5 and above. Explorez un univers de divertissement où chaque pari peut se transformer en victoire éclatante. La procédure d'adhésion est simplifiée, mais les connaisseurs savent que l'activation d'un code promo 1xbet maroc est le déclencheur d'une prime de 100% plafonnée à 130€ pour les pronostics sportifs ou d'une dotation casino de 1950€ incluant 150 tours gratuits. Ce cadeau d'accueil double votre mise initiale, vous offrant un volant financier conséquent. Que vous soyez adepte du ballon rond, de la petite balle jaune ou des machines à sous, cette gratification vous permet d'aborder multiples facettes de l'établissement.