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Location Information | Location Notes |
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U.S. Forest Service - Pacific Southwest Research Station (USFS - PSW) | Pat Manley - U.S. Forest Service - Pacific Southwest Research Station (USFS - PSW) | |||
University of California, Davis (UC Davis) | Kat McIntyre - Tahoe Regional Planning Agency (TRPA) |
No expected performance measures set for this project.
No annual performance measure accomplishments entered for this project.
Total | |||
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Unknown or Unassigned | $152,443 | $152,443 | $0 |
Grand Total | $152,443 | $152,443 | $0 |
Total | 2011 | 2010 | 2009 | 2008 | |
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Southern Nevada Public Land Management Act (Pacifi... | $152,443 | $38,111 | $38,111 | $38,111 | $38,110 |
Grand Total | $152,443 | $38,111 | $38,111 | $38,111 | $38,110 |
No watersheds set for this project.
No Local and Regional Plans set for this project.
No Related Projects set for this project.
No external links entered.
10/27/2017 2:02 PM | Matt Driscoll | Match Funding: $40,972 | ||
07/17/2017 2:56 PM | Kiara Cuerpo-Hadsall | Objectives: This study examines the groundwater system supporting Grass Lake, the largest peatland in the Sierra Nevada Mountains and how climate change might affect the Lake, located south of Lake Tahoe, California. |
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07/17/2017 2:56 PM | Kiara Cuerpo-Hadsall | Findings: • The average seasonal stream flow (ASSF) values for 2011 are 1.9 (First Creek) to 2.7 times (West Freel Meadows Creek, Freel Meadows Creek, Waterhouse Creek) higher the 2010 values. • The ASSF out of Grass Lake in 2011 was 2.2 times higher than the 2010 value. • In 2010 stream flow for the four streams entering Grass Lake proper fell below 1.0 cfs between late June (Waterhouse Creek) and late July (Freel Meadows Creek). • In 2011 stream flow for the four streams entering Grass Lake fell below 1.0 cfs between late July (West Freel Meadows Creek and Waterhouse Creek) and mid-August (Freel Meadows Creek). |
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07/17/2017 2:53 PM | Kiara Cuerpo-Hadsall | Management Implications: • This study suggests a rain dominated precipitation regime may lead to desaturation of the Grass Lake peatland. • The most significant drying is expected to occur in the eastern and western portions of the peatland, resulting in approximately half of the peatland experiencing saturation levels 70% or less of total saturation by the end of the water year. This is expected to lead to increased aerobic decomposition near the edges of the peatland. • The predicted increase in temperature is expected to further increase the rate of peat decomposition. The center of the peatland maintains saturation levels above 80% of total saturation in all simulations, suggesting this area is least susceptible to aerobic decomposition and may contain the longest history of peat accumulation despite changes in the precipitation regime. |
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07/17/2017 2:52 PM | Kiara Cuerpo-Hadsall | Publications: Christensen, W. (2013). Hydrologic characterization and modeling of a montane peatland, Lake Tahoe Basin, California. ProQuest, UMI Dissertations Publishing. |