Uncertainty in the impacts of projected climate change on the hydrology of a subarctic environment: Liard River Basin
Like many high latitude areas, the mountainous region of subarctic Canada has experienced recent warming and is an area of large inter-annual temperature variations, most notably during the winter. Quantifying how climate tendencies affect streamflow, especially in the spring melt season, is critica...
| Published in: | Hydrology and Earth System Sciences |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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Copernicus Publications
2011
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| Online Access: | https://doi.org/10.5194/hess-15-1483-2011 https://noa.gwlb.de/receive/cop_mods_00027428 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00027383/hess-15-1483-2011.pdf https://hess.copernicus.org/articles/15/1483/2011/hess-15-1483-2011.pdf |
| Summary: | Like many high latitude areas, the mountainous region of subarctic Canada has experienced recent warming and is an area of large inter-annual temperature variations, most notably during the winter. Quantifying how climate tendencies affect streamflow, especially in the spring melt season, is critical not only to regional water resource management, but to understanding the influence of freshwater on the Arctic sea-ice cover and global climate system. The impact of projected atmospheric warming on the discharge of the Liard River is unclear. Here, uncertainty in climate projections associated with GCM structure (2 °C prescribed warming) and magnitude of increases in global mean air temperature (1 to 6 °C) on the river discharge are assessed using a well-tested, semi-distributed hydrological model. Analyses have shown that the hydrological impacts are highly dependant on the GCM scenario. Uncertainties between the GCM scenarios are driven by the inconsistencies in projected spatial variability and magnitude of precipitation, rather than warming temperatures. Despite these uncertainties, the entire scenario simulations project that the subarctic nival regime will be preserved in the future, but the magnitude of change in river discharge is highly uncertain. Generally, spring freshet will arrive earlier, autumn to spring discharge will increase whereas summer flow will decrease, leading to an overall increase in annual discharge. |
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