Recently Added

Posted: November 15, 2017
Meadows of the Golden Trout Wilderness (GTW) are an extremely valuable component of the landscape, providing numerous benefits to society. In 2012, the National Fish and Wildlife Foundation funded a partnership between CalTrout, Trout Unlimited, and American Rivers to evaluate meadow resources in the GTW and prioritize meadows for restoration. We hope the information we provide here will help partners and the US Forest Service work together to increase the pace and scale of meadow restoration in the GTW.

Posted: November 15, 2017
This report briefly describes the methods we developed and presents findings from applying the methods in the Yuba and Mokelumne River watersheds.The methods we developed and the on-the-ground data for the Yuba and Mokelumne watersheds supply a replicable template that may be applied in other watersheds to focus meadow restoration effort where it will provide the greatest value. The prioritized list of meadows we developed galvanized support of the top restoration candidate (see From Prioritization to Restoration, below) and, within six months, resulted in completed permits and three funding proposals.Our ultimate goal is to accelerate and improve meadow restoration. The steps we took in this project focus on providing the infrastructure necessary for meadow restoration to gain and sustain momentum into its next phase, where watershed-scale impacts are anticipated.

Posted: November 15, 2017
This report shares the results of a broadly collaborative effort to assess and prioritize meadows in the Pine Creek Basin for restoration. The purpose of this Pine Creek Meadow Assessment report is twofold. First, it provides condition data and explains why the Pine Creek CRMP chose the first set of meadows as the top priority for restoration. Second, it provides a basis and identifies next steps for partners to pursue in restoring meadows in the watershed.

Posted: February 22, 2017
Articulates methods for monitoring hydrologic and water quality impacts of meadow restoration in the Sierra Nevada. This includes recommended analyses and standard metrics that, if reported, will enable future regional studies to combine data across meadow restoration projects. These methods are not exhaustive, rather we identify the key indicators that should be monitored by all projects aiming to alter hydrology or water quality through meadow restoration. Data collected are grouped into five categories based on the objectives they support: 1) groundwater elevation; 2) stream flow; 3) water temperature; 4) sedimentation; and 5) overview data, such as photographs and maps that support multiple monitoring objectives. Table 1 summarizes which data are collected and how they are reported. Tables and figures from the text are referenced as examples of how data are reported.

Posted: February 15, 2017
Study Region: We analyzed the effects of groundwater pumping on a mountain wetland complex, Yosemite National Park, California, USA. Study Focus: Groundwater pumping from mountain meadows is common in many regions of the world. However, few quantitative analyses exist of the hydrologic or ecological effects of pumping. New Hydrological Insights for the Region: Daily hydraulic head and water table variations at sampling locations within 100. m of the pumping well were strongly correlated with the timing and duration of pumping. The effect of pumping varied by distance from the pumping well, depth of the water table when the pumping started, and that water year's snow water equivalent (SWE). Pumping in years with below average SWE and/or early melting snow pack, resulted in a water table decline to the base of the fen peat body by mid summer. Pumping in years with higher SWE and later melting snowpack, resulted in much less water level drawdown from the same pumping schedule. Predictive modeling scenarios showed that, even in a dry water year like 2004, distinct increases in fen water table elevation can be achieved with reductions in pumping. A high water table during summers following low snowpack water years had a more significant influence on vegetation composition than depth of water table in wet years or peat thickness, highlighting the impact of water level drawdown on vegetation.

Posted: February 15, 2017
Two pumiceous tephra layers, widespread in meadow topsoils of the southern Sierra Nevada, are correlated on the basis of radiocarbon dates and trace-element analyses with two eruptive centers at the northern and southern ends of the Mono Craters--Inyo craters volcanic chain in eastern California. Pumice and obsidian that were erupted in the northern part of the chain are uniform in trace-element content, whereas those erupted from the southern part are nonuniform and distinctly different, particularly in Sr content. Similar differences are recognized in the two most recent and widespread tephra layers originating from these sites. These tephra layers are the deposits of the most recent explosive eruptions of magma from the Mono Craters and the Inyo craters. Tephra 1, characterized by sanidine microphenocrysts and a Sr content of about 215 ppm, was erupted 720 {+/-} 60 yr B.P. Its distribution defines a south-trending lobe extending over the Sierra Nevada from the upper San Joaquin drainage area to the Little Kern drainage area. Sr, Rb, and Zr contents of the ash are similar to those of a tephra-ringed obsidian dome at the south end of the Inyo craters. Tephra 2, characterized by a lack of microphenocrysts and a Sr content of less than 20 ppm, was erupted 1190 {+/-} 80 yr B.P. It is encountered as a fine ash layer in the Sierra Nevada from northernmost Yosemite to Kings Canyon. Its low Sr content indicates geochemical affinity with the Mono Craters. Panum Crater, a tephra-ringed dome at the north end of the chain, appears to be its most likely source vent.

Posted: February 15, 2017
Valley-fill deposits, exposed by Twentieth-Century dissection of a number of meadows on the west slope of the southern Sierra Nevada, contain a stratigraphic record strongly affected by secular variations in watershed hydrology during the Holocence. Meadows are situated in low gradient reaches, adequately supported by seepage water, where fine textured materials accumulate under present hydrologic conditions. Meadows do not necessarily owe their origin to glacial modification of drainage. Many meadows have formed in both glaciated and unglaciated valleys by a water table rise in valley-fill deposits. Ground water in any meadow drainage basin is annually recharged by snowmelt. Significant evapotranspiration by meadow plants causes diurnal fluctuations of growing-season water tables on the order of 0.2 to 0.5 ft and seasonal fluctuations of 2 to 4 ft. Growing-season water-table depths are characteristically different for the two major plant communities, being usually shallower that 2 feet for meadows, and deeper than 4 ft for conifer forests. This relationship and a ground-water model are used to interpret paleohydrologic variations recorded in valley-fill stratigraphy. Stratigraphy, radiocarbon dating, and tephrachronology indicate the following sequence in upper tributary valleys of the montane belt. Pre-Holocene cobbly alluvium rests upon bedrock. A paleosol developed upon this alluvium between 10,200 and 8700 radiocarbon years B.P., records an early post-glacial climatic interval that established forests in the present upper montane belt. The overlying sequence of coarse loamy materials associated with in situ conifer stumps indicates one or more intervals of good soil drainage and dry valley-bottom conditions between 8700 and 1200 years B.P. At some sites there is an abrupt change from forest soils to overlying wet-meadow deposits dated 2500 years at some sites and 1200 years at others, suggesting many meadows originated coincidentally with neoglaciation in the Sierras. A water-table rise of a few feet, resulting from late melting snows, could cause the change from forest to meadow conditions. Meadow deposits are composed of organic-rich, sandy-loam, topsoil layers intercalcated with sheets of well-sorted sandy gravels deposited by flood flows with recurrence intervals greater than 50 years. A plot of upstream catchment area and valley gradient for dissected and undissected meadows indicates the geomorphic domain of unstable meadows subject to gully erosion under present hydrologic conditions on the Sierra west slope. Two pumiceous tephra layers, widespread in meadow topsoils of the southern Sierra, are radiocarbon dated and attributed to tephra-ringed eruptive centers at opposite ends of the Mono-Inyo Crater chain of eastern California. Tephra 1, characterized by sanidine microphenocrysts and Sr content of 215 ppm, erupted 720 years B.P. Distribution of this tephra in confined to a south trending lobe extending 120 miles over the Sierra from the upper San Joaquin drainage to the Little Kern drainage. Trace element analysis of tephra 1 best match those of the tephra-ringed obsidian flow just south of Deadman Creek in the Inyo Craters. Tephra 2, characterized by a lack of microphenocrysts and Sr contents less than 20 ppm erupted from on the northern Mono Craters eruptive centers. These two tephras appear to represent the most recent explosive eruptions of magma from this 40-km long chain of Holocene volcanoes.

Posted: February 13, 2017
A broad sample of 79 montane fens in the Sierra Nevada revealed that underlying geology and topography exert strong control over the distribution and vegetation of these ecosystems. Distinct granodiorite, metamorphic, volcanic, carbonate and serpentine bedrock geology resulted in very different water chemistry, which had significant effects on the particular plant species found at each site. Wide-ranging values of pH (4.28–8.00) and dissolved cation concentrations (1.6–62.0 mg L-1) spanned the categories of transitional poor– rich to extremely rich fens. The vegetation of a pair of fens on carbonate bedrock and two floating mat fens was markedly different from the vegetation recorded at any other study sites. Once these outlier fens were removed from the analyses, the environmental variables that correlated most closely with the vegetation data were pH, altitude, presence of volcanic bedrock and fen slope. The measured environmental parameters explained 9.7 % of the variability in the vegetation data. Species richness was primarily (and negatively) correlated with altitude. Peat thickness (15–253 cm) was constrained in smaller catchments and on steeper slopes, and was positively correlated with soil organic matter content (16–92 %). Of the four typical fen landforms (bedrock contact, slope, spring mound and basin), sloping fens were the most common (63 % of the 79-fen sample).

Posted: February 8, 2017
Greenhouse Gas Sampling Protocol for Mountain Meadows for use in ongoing studies that are part of the Sierra Meadows research

Posted: February 8, 2017
A USGS comprehensive national assessment of carbon (C) storage and flux (flow) and the fuxes of other greenhouse gases (GHGs, including carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O)). These carbon and GHG variables were examined in the Western United States for major terrestrial ecosystems (forests, grasslands/shrublands, agricultural lands, and wetlands) and aquatic ecosystems (rivers, streams, lakes, estuaries, and coastal waters) in two time periods: baseline (the first half of the 2000s) and future (projections from baseline to 2050).

Posted: January 18, 2017
All-hands, all-lands approach to increasing the pace, scale, and efficacy of meadow restoration and protection throughout the Greater Sierra Nevada. Articulates three overarching strategy approaches, 1) Restore and/or protect meadows to achieve desired conditions; 2) Enhance regulatory and institutional funding capacity and coordination; 3) Increase and diversify institutional and partnership capacity for meadow restoration and/or protection in the greater Sierra.

Posted: January 18, 2017
A new strategy summary report has been released highlighting approaches to restoring and/or protecting 30,000 meadow acres on all lands in the Sierra Nevada.

Posted: November 2, 2016
The Great Gray Owl (Strix nebulosa) is a California Endangered Species, with an estimated population size of only 100-200 pairs in the state. It is the largest owl in North America and one of the largest owls in the world. It is also one of the most reclusive bird species, which provides challenges in studying its life history.

Posted: March 14, 2016
Standard Operating Procedures (SOP) for the Collection of Field Data for Bioassessments of California Wadeable Streams: Benthic Macroinvertebrates, Algae, and Physical Habitat. March 2016 v2 (unformatted).

Posted: March 14, 2016
Aquatic macroinvertebrate sampling for restoration projects protocol and methodology. Description of methodology and sampling protocols.

Posted: March 14, 2016
A modified and simplified outline of steps required to sample aquatic benthic macroinvertebrates, based on SWAMP protocols. Short foreword by Natalie Stauffer-Olsen.

Posted: February 18, 2016
Natural Range of Variation (NRV) assessments (essentially equivalent to Historical Range of Variation [HRV] assessments) provide baseline information on ecosystem conditions (composition, structure, and function) that can be compared to current conditions to develop an idea of trend over time and an idea of the level of departure of altered ecosystems from their “natural” state (Morgan et al. 1984, Manley et al. 1995, Landres et al. 1999, Wiens et al. 2012; see Methods). These trend assessments form part of the basis for the assessment of ecological integrity that is required in the 2012 Forest Service Planning Rule. NRV assessments were carried out for 11 terrestrial ecosystems by the Pacific Southwest Region Ecology Program between October, 2012 and May, 2013, using historical information (primarily from the pre-Euroamerican period, 16th century to the mid-19th century) as well as information from modern-day reference ecosystems and other sources. This is the meadow NRV assessment.

Posted: February 11, 2016
Hydrogeomorphic typing of Van Norden Meadow, conducted by Dave Weixelman, Rachel Hutchinson, Sarah Yarnell, and Ryan Peek.

Posted: February 10, 2016
Measurements of groundwater–surface water exchange at three wetland stream sites were related to patterns in benthic productivity as part of the US Geological Survey’s Northern Temperate Lakes–Water, Energy and Biogeochemical Budgets (NTL–WEBB) project. The three sites included one high groundwater discharge (HGD) site, one weak groundwater discharge (WGD) site, and one groundwater recharge (GR) site. Large upward vertical gradients at the HGD site were associated with smallest variation in head below the stream and fewest gradient reversals between the stream and the groundwater beneath the stream, and the stream and the adjacent streambank. The WGD site had the highest number of gradient reversals reflecting the average condition being closest to zero vertical gradient. The duration of groundwater discharge events was related to the amount of discharge, where the HGD site had the longest strong-gradient durations for both horizontal and vertical groundwater flow. Strong groundwater discharge also controlled transient temperature and chemical hyporheic conditions by limiting the infiltration of surface water. Groundwater–surface water interactions were related to highly significant patterns in benthic invertebrate abundance, taxonomic richness, and periphyton respiration. The HGD site abundance was 35% greater than in the WGD site and 53% greater than the GR site; richness and periphyton respiration were also significantly greater (p%0.001, 31 and 44%, respectively) in the HGD site than in the GR site. The WGD site had greater abundance (27%), richness (19%) and periphyton respiration (39%) than the GR site. This work suggests groundwater–surface water interactions can strongly influence benthic productivity, thus emphasizing the importance of quantitative hydrology for management of wetland-stream ecosystems in the northern temperate regions.

Posted: April 16, 2015
In this project, we sought to identify putative climate change refugia and connectivity between meadows across the Sierra Nevada and to use data on persistence, stability, and genetic diversity of mammal populations to validate these hypotheses. We addressed California Landscape Conservation Cooperative priorities of scale by analyzing across the Sierra Nevada. We involved state and federal natural resource managers throughout the project; some are already beginning to incorporate results. Our products focused on maps and tools that are user-friendly and that allow managers to make decisions and set landscape conservation priorities. We are communicating project outcomes directly to CA LCC partners to aid in decisions from immediate, small-scale adaptation projects to region-wide changes in use, development, and planning for state and federal land management. Our results will help managers to prioritize areas and landscapes that are critical to maintaining biodiversity in the Sierra Nevada in the face of climate change and to focus limited resources for effective adaptation efforts.

Posted: February 12, 2015
This report brings together recent survey results from state and federal agencies and other groups, and provide an updated range map and population estimate for Willow Flycatcher in the Sierra Nevada.

Posted: February 11, 2014
The Institute for Bird Populations is teaming with the National Fish and Wildlife Foundation and numerous public and private land managers to develop, assess, and refine bird-friendly meadow restoration efforts. This report is provides information relating to the development of a monitoring protocol for assessing how bird populations respond to meadow restoration in the Sierra Nevada. Monitoring visits included point count surveys, area searches, and vegetation assessments. This report describes results of the pre- and post-restoration monitoring completed at 59 meadows (including restoration and reference meadows) during 2012.

Posted: February 10, 2014
The Center for Watershed Sciences authored a technical report, "Montane Meadows in the Sierra Nevada: Changing Hydroclimatic Conditions and Concepts for Vulnerability Assessment" to better prepare the meadows community for ecosystem monitoring and restoration planning under future hydroclimatic conditions.

Posted: February 5, 2014
Grazing photo examples by the Central Sierra Environmental Resource Center (CSERC), 2013

Posted: February 5, 2014
This reports describes Central Sierra Environmental Resource Center (CSERC) continued monitoring or meadow condition and the degree of grazing utilization at more than 60 mountain meadows on the Stanislaus National Forest.