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How do clouds influence the temperatures at the surface in the Arctic?
How is the extent of permafrost in the Arctic projected to change over the next century?
To a large extent, humans are responsible for excess greenhouse gases currently contributed to the atmosphere. What will the rates of Arctic warming be if we stabilize and reduce our emissions of greenhouse gases over the next century, versus, continuing with a business-as-usual scenario?
How do these different scenario/projections of warming differ from winter to summer seasons?
1) What is the variability of surface air temperature simulations across many climate models?
2) What is the variability of surface circulation features across many climate models?
How is the length of the growing season in the Arctic projected to change over the next century?