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The nitrogen cycle is the process where nitrogen transforms to its various chemical forms. This transformation can be carried out through both biological and physical processes. 78% of Earth's atmosphere is nitrogen.

In a tundra, snow controls the nitrogen cycle. Snow causes an abundance of nitrogen. This is because snow forms in the atmosphere, and since the atmosphere is 79% nitrogen, snow can absorb a fair amount of it.

Nitrogen from dead animals exists in the permafrost, which is a thick subsurface layer of soil that remains frozen throughout the year. When the permafrost thaws, it is released into the air causing an excess of nitrogen. Nitrogen cycles are inter linked to carbon cycles because the decomposition of carbon in organic soil by microbes and the photosynthetic uptake of atmospheric carbon dioxide by plants is depended on the nitrogen available in the area.

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