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Type: | Resource | |
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Created: | Jun 23, 2025 at 3:57 p.m. (UTC) | |
Last updated: | Jun 23, 2025 at 5:58 p.m. (UTC) | |
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Sharing Status: | Public |
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Abstract
High northern latitudes are experiencing dramatic changes in precipitation and air temperatures. These changes can impact river discharge and concentrations of bioreactive elements like carbon and nitrogen, but the pathways linking soil source pools to streams remain poorly constrained. Here we use high frequency water isotope and biogeochemical concentrations from a temperate forested watershed in Southeast Alaska to better understand how rainfall can influence water flow pathways, stream discharge, and concentrations of dissolved organic carbon (DOC) and total dissolved nitrogen (TDN). We found that shallow groundwater traveling through organic matter rich surface horizons dominates contributions to stream water discharge during both wet and dry periods. Additionally, DOC yields generally increase with heightened shallow groundwater contributions and greater discharge, while TDN is more disconnected from these hydrologic processes. However, increased future groundwater contributions from shallow flowpaths to streams, particularly during repeated storm events, in a warmer and wetter region could lead to temporary periods of DOC source limitations, but will have little impact on TDN. Further, our findings suggest that concentration-discharge relationships for TDN appear to be controlled primarily by reach-scale factors, which could also shift in the future due to changes like warming stream temperatures due to shrinking snow and glacial meltwater inputs to surface water. These stream DOC/TDN dynamics could also impact nutrient availability in coastal regions that have limited mixing with the open ocean.
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Credits
Funding Agencies
This resource was created using funding from the following sources:
Agency Name | Award Title | Award Number |
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National Science Foundation | Alaska EPSCoR | OIA-1757348; ORE-CZ (EAR-2227821) |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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