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Hydrologic studies of four small runoff plots were conducted in the continuous permafrost zone of north-central Banks Island between 1977 and 1979. One plot was located on an jnterfluve while the other three where on slopes where snowbanks develop. The plots ranged in size from 27 to 525 m2. For two...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.528.8542 http://pubs.aina.ucalgary.ca/cpc/CPC4-151.pdf |
| Summary: | Hydrologic studies of four small runoff plots were conducted in the continuous permafrost zone of north-central Banks Island between 1977 and 1979. One plot was located on an jnterfluve while the other three where on slopes where snowbanks develop. The plots ranged in size from 27 to 525 m2. For two to three months of each summer field season, all the major inputs and outputs of the hydrologic cycle were measured at each plot. The results of the study indicate a high degree of variability in the proportions of water losses from the plots, attributable to surface and subsurface flow. This variability is evident both in inter-year comparisons for a single site and inter-site comparisons for a single year. Inter-year variability is controlled largely by the winter snow distribution and by meteorological conditions during the melt season. Inter-site variability is influenced by snowbank size, with the largest snow accumulation site exhibiting the highest percentage loss to surface flow, and the smallest loss to subsurface flow and evapotranspiration. Surface-flow hydrographs of snowmelt runoff recorded at the plots are explicable within the context of accepted snowmelt theory. Surface flow generated by rainfall was much less important and occurred only twice in the three years of measurement. On these occasions, only areas downslope of existing snowbanks, or those areas from which snow had recently disappeared, pro-duced surface flow. These observations support the validity of the partial and variable concepts of runoff generation in the high Arctic. Areas producing surface flow are dependent on topograph-ically controlled snowbank distribution, rather than, as in temperate areas, on the location of streams. |
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