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Melting glaciers in Svalbard deliver additional 13 km3 water each year

Amplified melting of small glaciers in the Arctic has largest impact on changing global sea level. Fresh calculations based on the latest glacier mass balance data from Svalbard show additional delivery of 13 km3 melt water to the ocean each year.

All predictions indicate further changes of climate in the Arctic. This would cause large amplification of glacier melting and increased global sea level. Arctic glaciers are particularly sensitive to even small change in air temperature and they react quickly. Therefore it is extremely important to maintain long-term glacier monitoring programme.

Glaciers in Svalbard and Alaska melt much quicker than glaciers in other Arctic regions. In fact Svalbard glaciers melt twice as fast as the ones in Canadian Arctic do.

Due to climate warming as much as 13 km3 of meltwater from Svalbard glaciers is delivered every year to the ocean. This amount is additional to what would be melting if the glaciers were in balance with climate. Meltwater from Svalbard glaciers alone rise sea level by 0.035 mm each year.

Glacier mass balance and dynamics research has been carried out on sevaral glaciers in various locations in Svalbard. This work is part of the large international project: GLACIODYN (GLACIODYN Norway website).

See also:
Svalbard-breene smelter dramatisk: 41/2 millioner tonn smeltevann i timen (article in University of Oslo research journal Apollon, in Norwegian only)

GLACIODYN at IASC Working Group on Arctic Glaciology

Contact: Jon Ove Hagen, University of Oslo (j.o.m.hagen@geo.uio.no)

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Small glaciers occupy only 0.5% of total glaciated area in the world, yet their contribution to sea level rise is 70% (Graph: Apollon, UiO)

Calving front of Körberbreen in Hornsund (photo: Marzena Kaczmarska)

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