Modeling the Thermal Balance Between Groundwater Springs and River Ice

We modeled the thermal balance between groundwater discharge and ice-free areas in the Tanana River near Fairbanks, Alaska, a region that is characterized by discontinuous permafrost. Under degrading permafrost conditions, these areas have been hypothesized to have increased winter discharge due to...

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Bibliographic Details
Format: Dataset
Language:unknown
Published: International Arctic Research Center (IARC) Data Archive
Subjects:
Ice
Online Access:https://search.dataone.org/view/dcx_517c5be1-7833-43c3-8cb6-91d752c7968b_0
Description
Summary:We modeled the thermal balance between groundwater discharge and ice-free areas in the Tanana River near Fairbanks, Alaska, a region that is characterized by discontinuous permafrost. Under degrading permafrost conditions, these areas have been hypothesized to have increased winter discharge due to increasing contributions from groundwater flow. In the winter, interior Alaskan rivers are fed almost entirely by groundwater, which also serves as an external source of heat energy to the system. Several reaches of the river fed by groundwater springs remain ice-free or have dangerously thin ice throughout the winter despite air temperatures that dip below -40° C. These areas are dangerous for winter travelers who regularly use Alaskan rivers for wintertime travel. Our model allows us to explore the relationship between seasonal groundwater flows and ice thickness under changing atmospheric conditions. Our model results explore how local and regional changes in groundwater flow can affect ice thickness by addressing two primary research questions: 1) What physical factors influence seasonal ice dynamics on the Tanana River? 2) How is the thermal balance maintained between changing groundwater flow and cold air temperatures? Our results indicate that under field conditions with our measured upwelling rate, heat flux due to upwelling may degrade river ice at up to 17 mm/day, but the potential ice melt is reduced by increased air temperature and water depth, but increased by increased hydraulic conductivity, groundwater upwelling, ice thickness, or snow depth. Increased air temperatures associated with climate change is expected to increase upwelling rates, decrease the temperature gradient, increase snow depths, and decrease ice thickness. Estimated future changes estimate that potential ice melt rates may increase by up to 18% under an altered climate. These results provide additional evidence that changing hydrologic conditions may affect inhabitants of northern latitudes under potential hydrologic scenarios in a changing climate.