Lake floor morphology and sediment architecture of lake torneträsk, northern sweden

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Lake floor morphology and sediment architecture of lake torneträsk, northern sweden

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http://www.wikidata.org/entity/Q58106107

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wetenschappelijk artikel

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наукова стаття, опублікована в червні 2013

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Lake floor morphology and sediment architecture of lake torneträsk, northern sweden

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Lake floor morphology and sediment architecture of lake torneträsk, northern sweden

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Lake floor morphology and sediment architecture of lake torneträsk, northern sweden

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Lake floor morphology and sediment architecture of lake torneträsk, northern sweden

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Lake floor morphology and sediment architecture of lake torneträsk, northern sweden

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Lake floor morphology and sediment architecture of lake torneträsk, northern sweden

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P1476

Lake floor morphology and sediment architecture of lake torneträsk, northern sweden

@en

P2093

Bernd Wagner

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Peter Rosén

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P2860

Thawing permafrost and thicker active layers in sub-arctic Sweden

What determines the current presence or absence of permafrost in the Torneträsk region, a sub-arctic landscape in northern Sweden?

Climate driven release of carbon and mercury from permafrost mires increases mercury loading to sub-arctic lakes.

Effects of a warmer climate on seed germination in the subarctic.

A catchment-scale carbon and greenhouse gas budget of a subarctic landscape.

Light limitation of nutrient-poor lake ecosystems.

Patterns of Quaternary ice sheet erosion and deposition in Fennoscandia and a theoretical framework for explanation

Preglacial surface remnants and Quaternary glacial regimes in northwestern Sweden

Quantifying the relative importance of lake emissions in the carbon budget of a subarctic catchment

The relationship between subsurface hydrology and dissolved carbon fluxes for a sub-arctic catchment

P304

159-170

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P31

scholarly article

P356

10.1111/GEOA.12006

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P433

http://www.w3.org/2001/XMLSchema#string

P478

http://www.w3.org/2001/XMLSchema#string

P50

Hendrik Vogel

P577

2013-06-01T00:00:00Z

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