Titlebook: Jan Mayen Island in Scientific Focus; Stig Skreslet Conference proceedings 2004 Springer Science+Business Media New York 2004 Aerosol.Atmo

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Geology of Jan Mayen Island and Surroundings,st southward of the seismically active Jan Mayen Fracture Zone. Volcanic rocks of Quaternary age predominate on the island. Itsnorthern part (Nord-Jan) is formed by the large Beerenberg stratovolcano (2,277m). The oldest historical records of its activity are from 1732 and 1818 AD. In September 1970

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The Potential of the Beerenberg Glaciers for Climate Studies,ferent possible programs can be outlined. 1) Annual glacier front variations can give smoothed long-time information about the net mass balance of the glaciers. 2) Mass balance monitoring can be done as measurements of altitude variations of winter accumulation and summer melting and give informatio

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Meteorological Observations on Jan Mayen,average annual precipitation for 1921–1996 was 664.4mm, highest in December (64.8mm), lowest in June (31.5mm) The annual average number of overcast days was 242.0 and the average cloud cover 84.6% for 1922–1996. The annual frequency of fog was 13.7 for the 1956–1996 period. The lowest cloud height w

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On the Origin of Climatic Signals in the Nordic Seas,rcing impact like El Niño events can cause a heat flow pattern reconfiguration as in the Barents Sea so, perhaps, in whole Nordic Area. There is a good reason to assume that distant energetic connections in the sea-atmosphere climatic system are attributed to certain features of atmospheric circulat

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The Circulation of the Nordic Seas,ion and deep-water formation take place there. Barotropic and topographically steered, northward flow on the eastern side of the Nordic Seas carries warm and, salt Atlantic Water to the Arctic Ocean through the Barents Sea and the Fram Strait. On the other side, along the Greenland shelf, cold and f

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