Process Synchrony a Key Control of Resilience in a Subarctic Freshwater System
Abstract Climate‐induced changes in streamflow and biogeochemistry are occurring across the northern circumpolar region but several key unknowns include (a) the mechanisms responsible among landscapes and permafrost conditions, (b) the resilience and precariousness of hydrological and biogeochemical...
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Wiley
2025-03-01
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| Series: | Earth's Future |
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| Online Access: | https://doi.org/10.1029/2024EF005518 |
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| author | C. Spence J. M. Galloway N. Hedstrom S. V. Kokelj S. A. Kokelj P. Muise B. W. Newton R. T. Patterson M. F. J. Pisaric G. T. Swindles |
| author_facet | C. Spence J. M. Galloway N. Hedstrom S. V. Kokelj S. A. Kokelj P. Muise B. W. Newton R. T. Patterson M. F. J. Pisaric G. T. Swindles |
| author_sort | C. Spence |
| collection | DOAJ |
| description | Abstract Climate‐induced changes in streamflow and biogeochemistry are occurring across the northern circumpolar region but several key unknowns include (a) the mechanisms responsible among landscapes and permafrost conditions, (b) the resilience and precariousness of hydrological and biogeochemical regimes. Even though it is among the largest physio‐climatic regions of the northern circumpolar, these knowledge gaps are acute in the Taiga Shield. This research aimed to determine if hydrology and biogeochemistry regimes of the Taiga Shield have been resilient to recent climate warming. We apply a recently developed framework of hydrological resilience that shows the first 20 years of the 21st century were the warmest and wettest of the previous 300 years. These conditions altered the catchment such that >50% of the water year streamflow now occurs during winter, shifting the catchment from a nival to a cold season pluvial hydrological regime. This regime shift has significantly changed the fraction of inorganic nitrogen export, but insufficiently to shift the biogeochemical regime. Sustained multi‐year physical process synchronization was the cause of these changes. This behavior is not well simulated by existing Earth system models. The tipping point in local mean annual air temperatures was crossed near the turn of the century well below the warming threshold of the Paris Accord. A one‐size‐fits‐all approach to mitigation targets is not effective at preventing all shifts in Earth systems. This is important to consider as regime changes in small hydrological systems have the potential to trigger cascading effects in the larger catchments to which they contribute. |
| format | Article |
| id | doaj-art-9bd24d2de64c4d3f8b0e3ce1e5d6d19f |
| institution | DOAJ |
| issn | 2328-4277 |
| language | English |
| publishDate | 2025-03-01 |
| publisher | Wiley |
| record_format | Article |
| series | Earth's Future |
| spelling | doaj-art-9bd24d2de64c4d3f8b0e3ce1e5d6d19f2025-08-20T03:17:57ZengWileyEarth's Future2328-42772025-03-01133n/an/a10.1029/2024EF005518Process Synchrony a Key Control of Resilience in a Subarctic Freshwater SystemC. Spence0J. M. Galloway1N. Hedstrom2S. V. Kokelj3S. A. Kokelj4P. Muise5B. W. Newton6R. T. Patterson7M. F. J. Pisaric8G. T. Swindles9Environment and Climate Change Canada Saskatoon SK CanadaGeological Survey of Canada/Commission géologique du Canada Calgary AB CanadaEnvironment and Climate Change Canada Saskatoon SK CanadaNorthwest Territories Geoscience Office Yellowknife NT CanadaEnvironment and Climate Change Government of the Northwest Territories Yellowknife NT CanadaDepartment of Geography and Tourism Studies Brock University St. Catharine's ON CanadaAlberta Environment and Protected Areas Calgary AB CanadaOttawa‐Carleton Geoscience Centre and Department of Earth Sciences Carleton University Ottawa ON CanadaDepartment of Geography and Tourism Studies Brock University St. Catharine's ON CanadaOttawa‐Carleton Geoscience Centre and Department of Earth Sciences Carleton University Ottawa ON CanadaAbstract Climate‐induced changes in streamflow and biogeochemistry are occurring across the northern circumpolar region but several key unknowns include (a) the mechanisms responsible among landscapes and permafrost conditions, (b) the resilience and precariousness of hydrological and biogeochemical regimes. Even though it is among the largest physio‐climatic regions of the northern circumpolar, these knowledge gaps are acute in the Taiga Shield. This research aimed to determine if hydrology and biogeochemistry regimes of the Taiga Shield have been resilient to recent climate warming. We apply a recently developed framework of hydrological resilience that shows the first 20 years of the 21st century were the warmest and wettest of the previous 300 years. These conditions altered the catchment such that >50% of the water year streamflow now occurs during winter, shifting the catchment from a nival to a cold season pluvial hydrological regime. This regime shift has significantly changed the fraction of inorganic nitrogen export, but insufficiently to shift the biogeochemical regime. Sustained multi‐year physical process synchronization was the cause of these changes. This behavior is not well simulated by existing Earth system models. The tipping point in local mean annual air temperatures was crossed near the turn of the century well below the warming threshold of the Paris Accord. A one‐size‐fits‐all approach to mitigation targets is not effective at preventing all shifts in Earth systems. This is important to consider as regime changes in small hydrological systems have the potential to trigger cascading effects in the larger catchments to which they contribute.https://doi.org/10.1029/2024EF005518streamflowbiogeochemistryCanadian Shieldclimate change mitigationregime shift |
| spellingShingle | C. Spence J. M. Galloway N. Hedstrom S. V. Kokelj S. A. Kokelj P. Muise B. W. Newton R. T. Patterson M. F. J. Pisaric G. T. Swindles Process Synchrony a Key Control of Resilience in a Subarctic Freshwater System Earth's Future streamflow biogeochemistry Canadian Shield climate change mitigation regime shift |
| title | Process Synchrony a Key Control of Resilience in a Subarctic Freshwater System |
| title_full | Process Synchrony a Key Control of Resilience in a Subarctic Freshwater System |
| title_fullStr | Process Synchrony a Key Control of Resilience in a Subarctic Freshwater System |
| title_full_unstemmed | Process Synchrony a Key Control of Resilience in a Subarctic Freshwater System |
| title_short | Process Synchrony a Key Control of Resilience in a Subarctic Freshwater System |
| title_sort | process synchrony a key control of resilience in a subarctic freshwater system |
| topic | streamflow biogeochemistry Canadian Shield climate change mitigation regime shift |
| url | https://doi.org/10.1029/2024EF005518 |
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