trusiak_fig4

Figure 4.  The Arctic is warming twice as fast as the rest of the planet. 

trusiak_fig3

Figure 3. Soil waters had to be filtered in a oxygen-free glove bag back in the lab at Toolik Field Station to avoid oxidation of reduced iron before the start of experiments.

trusiak_fig2

Researchers at Toolik Lake

trusiak_fig1

Figure 1. Red-orange oxidized iron precipitates across the arctic landscapes.

rastetter-et-al

Climate models of changes in ecosystem carbon and nitrogen with increases in temperature. Black, dotted line represents a model where vole effects are “Aggregated” with other biogeochemical processes. Red dashed line represents a model with constant vole density (100 voles per hectare). Blue solid line represents a model with a simulated “Vole cycle,” in which vole abundance fluctuates with peaks every 3-4 years based on demographic patterns observed in wild populations. When voles aren’t explicitly accounted for (aggregated, dotted black line), the model underestimates shifts in carbon and nitrogen stocks.

vole

Frances_Trevor_Arctic LTER

Streams LTER Research Assistant Frances Iannucci (a coauthor on the study) recording dissolved oxygen in a watershed associated with the Arctic LTER. Credit: Jay Zarnetske

Muskox_JStuart

The elusive muskox stands atop a hill before approaching our truck on the nearby road. Julia Stuart (CC BY 4.0)

FlatTire_JStuart

Field technician Emily Brooke leads the charge in changing our second flat tire on the Dalton Highway, just another adventure in field work. Julia Stuart (CC BY 4.0) Julia Stuart (CC BY 4.0)

MichellePlucking_SMiller

Dr. Michelle Mack identifies a plant root as she nears the end of plucking her sample. Samantha Miller (CC BY 4.0)