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There is a persistent area of low pressure near Iceland known as the Icelandic Low, found between Iceland and Greenland. This area affects the amount of air brought into the Arctic to the east, and the amount coming out of the Arctic to the west. [11] It is part of a greater pressure system known as the North Atlantic Oscillation (NAO). [12]
Thunderstorms, however, are very rare in Iceland, and there are less than five of them per year. [5] In June, Iceland's average daily temperatures range from 8 °C (46 °F) to 16 °C (61 °F). [9] Summer conditions vary in Norway depending on location. The Norwegian coast has cooler summers than areas further inland.
Because the Gulf Stream has a moderating effect, portions of Iceland have an Oceanic climate (subpolar variety) (Köppen climate classification: Cfc).But most of the ecoregion is Tundra climate (Köppen climate classification: ET), a local climate in which at least one month has an average temperature high enough to melt snow (0 °C (32 °F)), but no month with an average temperature in excess ...
Snæfellsjökull (Icelandic pronunciation: [ˈs(t)naiːˌfɛlsˌjœːkʏtl̥] ⓘ, snow-fell glacier) is a 700,000-year-old glacier-capped stratovolcano in western Iceland. [3] It is situated on the westernmost part of the Snæfellsnes peninsula. Sometimes it may be seen from the city of Reykjavík over Faxa Bay, at a distance of 120 km (75 mi).
An unusually chilly spring is about to turn even more shocking as cold air, moisture and a visit from the polar vortex team up to trigger way out-of-season conditions for mid-May across portions ...
The Southern Peninsula, also known as the Reykjanes Peninsula, is located in the southwestern corner of Iceland. The area contains little vegetation because of active volcanism and large lava fields. There are hot springs and sulphur springs in the southern portion of the peninsula, in the Kleifarvatn lake and the Krýsuvík geothermal area.
There is a pervasive danger of glacial outburst floods, or "glacier runs," at times of eruptions and volcanic activity. The radiating heat causes the underside of glaciers to melt, creating large pockets of water that accumulate until they burst. This phenomenon is unique to Iceland and is internationally known by the Icelandic term jökulhlaup ...
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