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Understanding Climate Recovery From Warming. 

 The Paleocene-Eocene Thermal Maximum (PETM) was a rapid warming event (hyperthermal) 56 million years ago. It is studied as an analogy of current climate warming, so that we understand what happens during increasing temperatures.. We are examining how the climate recovered several tens of thousands of years after the warming started. 

Latest Publication

Tracing silicate weathering processes in the permafrost-dominated Lena River watershed using lithium isotopes

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More Sampling

Water sampling. Measuring dissolved CO2 (alkalinity) in the waters by titration in the field. A measure of how much each river is affecting the climate by removing carbon dioxide Sampling and Filtering. Again. Apparently, there was a question...

Skogafoss

Camping at Skogafoss - slight change in plan as trekking across the to Landmannalaugar is not possible in the bad weather. So here is a view of the waterfall instead

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Why is the Earth Habitable?

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More Sampling

Water sampling. Measuring dissolved CO2 (alkalinity) in the waters by titration in the field. A measure of how much each river is affecting the climate by removing carbon dioxide Sampling and Filtering. Again. Apparently, there was a question...

Skogafoss

Camping at Skogafoss - slight change in plan as trekking across the to Landmannalaugar is not possible in the bad weather. So here is a view of the waterfall instead