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Fraser Experimental Forest
The 23,000 acre Fraser Experimental Forest was established
in 1937 as a representative site for conducting studies in the
alpine/subalpine environment of the central Rockies. It is
located on the Sulfur District, Arapaho National Forest,
approximately 70 miles west of Denver, on the west side
of the continental divide.
Most early research was oriented toward timber or water
production resulting from forest management. To this end there
are numerous long term study plots in both lodgepole pine and
englemann spruce as well as 9 gaged watersheds and attendant
meteorological installations and snow courses. Some of the
records now exceed 50 years in length. Research on
forest/wildlife interactions began in the 1950's.
Biogeochemical studies began in the 1960's, were
restarted in the 70's, and have been continuous since 1982.
Much of this work is done in cooperation with the National
Park Service.
Today, most of the new research addresses questions that deal with stand and landscape diversity or specific plant allocation and water processes that better define ecosystem function. Fraser is unique in that it has relatively long term record, pristine atmospheric input, and significant areas that have not been impacted by management or non-conforming uses.
In addition to several RMRS projects that conduct research at Fraser, North Central Station and faculty and graduate students from 6 universities also participate. Scientists from Europe, Asia, and Canada spend extended periods there as well.
Climate
Elevation ranges from 2,680 to 3,900 m, and about onethird
of the forest is above timberline at 3,350 m.
Climate is strongly correlated with elevation, with snow
increasing and temperatures decreasing with elevation.
Overall, the climate is cool and humid, with long cold
winters and short cool summers. Average annual
temperature at Fraser headquarters (2,745 m) is 0.5 °C,
and frost can occur any month of the year. At
headquarters, the mean monthly temperature is -10 °C
for January and 12.7 °C for July. Annual precipitation
averages 584 mm (range, 432 to 711 mm), and average
annual precipitation over the entire forest is 737 mm.
Nearly two-thirds of the precipitation falls as snow from
October to May.
Soils
Soils are generally derived from gneiss and schist. Typical
soils contain angular gravel and stone with little silt and
clay. These soils are permeable and can store considerable
water during snowmelt. At high elevations, especially on
the west side, soils are derived from sandstones. These
soils are shallow, have large amounts of stone, and have
fine sand or sand textures. Alluvial soils occur along main
streams, with parent material a mixture of glacial till,
glacial outwash, and recent valley fill.
Vegetation
The Fraser includes subalpine forests and alpine tundra
typical of the central Rocky Mountains. In the forested
areas below the timberline, Engelmann spruce and
subalpine fir are the predominant trees at higher
elevations, or north slopes, and along streams; lodgepole
pine is the predominant tree at lower elevations and on
drier upper slopes. The majority of the forest regenerated
naturally (sometimes slowly) after a stand-replacing fire
in 1685. There are pockets of older trees in draws and at
higher elevations. The flat, low-elevation portion of the
forest was logged in the early 1900s.
Long-Term Data Bases
The primary research focus on the Fraser has been the
effect of management practices on water yield and
quality. Snow depth and water content are collected on
five watersheds, with records dating to 1941 for one of
them. Streamflow is monitored on seven watersheds, and
a continuous record of streamflow for the oldest
watersheds dates from 1941-43. Sediment transport and
bedload are measured periodically. Precipitation and
temperature are measured at more than eight locations
and records are available from 1969 (one location from
1939). An NSF Long-Term Ecological Research quality
environmental monitoring system was installed in 2001.
Precipitation, streamflow, and snowpack chemistry have
been monitored weekly since 1982. Tree growth, seed
production, and tree mortality have been recorded at the
Fraser since in 1938. Climate and streamflow data are
available at
http://www.fs.fed.us/rm/fraser/fefdatabase.htm.
Research, Past and Present
Most early research on the Fraser was oriented toward
timber or water production and effects resulting from
forest management. Additionally, much research focused
on the effect of forest structure and species water use,
snow distribution, and water yield. A number of
integrated studies examined management impacts on
ecosystem processes and animal populations for a
landscape. Much early research is summarized in RMGTR-
118, available on the web. Current research
addresses questions about links between forests, riparian
areas, and streams, and aims to better understand
mechanisms important in nutrient cycling, snow
hydrology, and ecosystem carbon storage. More than 30
individual studies are in progress in addition to the
continued long-term monitoring of climate, streamflow,
and water chemistry.
Major Research Accomplishments
and Effects on Management
Research at Fraser has provided significant advances in
our understanding of subalpine forest ecology and
hydrology, and most of the silvicultural and hydrological
practices used in managing subalpine forests in the
central Rocky Mountains are derived from research done
here. Improvements in understanding the factors that
control snow distribution and water yields across
heterogeneous landscapes have been incorporated into
water-yield models and applied widely. Studies of tree
water use and ecophysiology have provided a better
understanding of the growth dynamics of forests and
transpiration water loss, and have been incorporated into
mechanistic models of ecosystem function used to
predict the impact of changing climate on forest
production and carbon storage. Long-term studies of
manipulated forest stands indicate that recovery requires
substantially longer than originally hypothesized. Aquatic
and terrestrial biogeochemistry have been studied in
manipulated and control catchments, providing a greater
understanding of the processes that control stream-water
quality.
Collaborators
Research collaborators working at the Fraser have come
from the USDI Geological Survey, US Forest Service
Rocky Mountain and North Central Research Stations,
Colorado State University, University of Colorado, State
University of New York, and Texas Tech University.
Research Opportunities
The Fraser is ideal for research that extrapolates from the
plot to the watershed for hydrology, biogeochemistry,
and vegetation. Outstanding opportunities are available
to examine issues of landscape-scaling by expanding the
Fraser's GIS to cover biogeochemistry (carbon storage
and flux; nitrogen cycling, and retention) and forest
structure and dynamics. Additionally, the dramatically
increasing recreation use offers an opportunity to assess
the effects of recreation. We welcome and encourage
research at Fraser, and especially encourage research that
takes advantage of the long-term records.
Facilities
The Fraser Experimental Forest is easily accessible (less
than 2 hours from Denver), has lodging for 20 to 25
people (main lodge, two cabins, bunkhouse, lounge, and
washroom), a new biogeochemistry and ecophysiology
laboratory and meeting/office space, and extensive shop
and storage facilities. Lodging is available for researchers
and their field crews for a nominal fee. Although well
roaded, less than 25 percent of the area has been affected
by research.
Lat. 39°54'25" N, long. 105°52'58" W
Contact Information
Fraser Experimental Forest
US Forest Service
Rocky Mountain Research Station
240 West Prospect Road
Fort Collins, CO 80526
Tel: (970) 498-1255
Or
Manager, Fraser Experimental Forest
US Forest Service
4947 County Road 73
PO Box 117
Fraser, CO 80442
Tel: (970) 726-5220
Forest website
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