Icelandic Low
In today's article, we are going to delve into the fascinating world of Icelandic Low. From its origins to its impact on today's society, we will explore the different aspects that make Icelandic Low relevant today. We will analyze its evolution over time, its influence in different areas and its role in daily life. With a broad and objective perspective, we will seek to approach Icelandic Low from various perspectives to understand its true meaning and scope in today's world. Join us on this journey through Icelandic Low and discover everything behind this exciting topic.
The Icelandic Low is a semi-permanent centre of low atmospheric pressure found between Iceland and southern Greenland and extending in the Northern Hemisphere winter into the Barents Sea. In the summer, it weakens and splits into two centres, one near Davis Strait, Labrador, and the other west of Iceland. It is a principal centre of action in the atmosphere circulation of the Northern Hemisphere, associated with frequent cyclone activity. It forms one pole of the North Atlantic oscillation, the other being the Azores High.
See also
References
- National Snow and Ice Data Center, retrieved 19 May 2005.
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