Thermal and hydrological conditions of the Goethe rock glacier, Central Sierra Nevada, California
The potential of rock glaciers in the Sierra Nevada to provide critical hydrological reservoirs and ecological habitats in a changing climate remains largely untested. In an effort to constrain the microclimatic contributions of buried ice, continuous temperatures were recorded in the near-surface d...
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| Format: | Text |
| Language: | English |
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Western CEDAR
2013
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| Online Access: | https://cedar.wwu.edu/wwuet/307 https://cedar.wwu.edu/cgi/viewcontent.cgi?article=1306&context=wwuet |
| Summary: | The potential of rock glaciers in the Sierra Nevada to provide critical hydrological reservoirs and ecological habitats in a changing climate remains largely untested. In an effort to constrain the microclimatic contributions of buried ice, continuous temperatures were recorded in the near-surface debris of a variety of ice-cored and associated landforms in the Goethe cirque from August 2011 and July 2012 (Goethe rock glacier=GRG, valley-wall rock glaciers=VRG, Recess Peak debris=RPD, talus=TAL, ranging from most ice to least ice). In addition, continuous meteorological conditions on the rock glacier and stage of the main meltwater outwash stream were recorded to assess temporal and spatial responses of hydrologic inputs and outputs to the rock glacier. The mean annual surface temperature (MAST) of the GRG is -2°C and the mean annual temperature at depth (MADT) is -2.5°C. The GRG has the steepest average annual temperature gradient of all the landforms with 0.44°C/m, indicating the presence of a large ice core. The MAST for RPD, VRG, and TAL are -0.5°C, -2°C, and -2.5°C, respectively, and their MADTs are -1°C, -3°C, and -3°C respectively. The mean annual air temperature (MAAT) from the on-site weather station in the cirque was -1.5°C, and the total cumulative precipitation was 552 mm. The modeled discharge varies from 0-1.6 cms, averaging 0.35 cms, and the stream temperatures vary from 0-3.85°C, averaging 0.53°C. According to Tritium signatures of stream water samples, the percent of ice-core melt versus snowmelt in the stream was 0% for the mid-summer of 2011, 5% for fall of 2011, and 13% for the early summer of 2012. The thermal and hydrological conditions in the Goethe cirque indicate a large sensitivity to meteorological conditions that is seasonally moderated by cold internal temperatures within the ice and debris of the landforms. The two contrasting summers during the yearlong study period exhibited different characteristics, particularly in discharge, stream temperature, and relative contribution of ... |
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