The Fernow Experimental Forest, West Virginia, USA: Insights,
datasets, and opportunities.
ii. Running head:
The Fernow Experimental Forest.
iii. Full Names of the Authors and iv. Institutions:
Luis Andrés Guillén * (Corresponding author), Division of
Forestry & Natural Resources, West Virginia University, 334 Percival
Hall, Morgantown, WV 26506, USA,
lg0018@mix.wvu.edu
Mary Beth Adams, PhD. Research Soil Scientist, USDA Forest Service
Northern Research Station.
Emily Elliot, PhD. Associate Professor, Department of Geology and
Environmental Science, University of Pittsburgh.
Jason Hubbart, PhD. Professor, Division of Plant and Soil Sciences &
Division of Forestry and Natural Resources, West Virginia University.
Charlene Kelly, PhD. Teaching Assistant Professor. Division of Forestry
& Natural Resources, West Virginia University.
Brenden McNeil, PhD. Associate Professor. Department of Geography, West
Virginia University.
William Peterjohn, PhD. Professor. Department of Biology, West Virginia
University.
Nicolas Zegre, PhD. Associate Professor. Division of Forestry & Natural
Resources, West Virginia University.
v. Acknowledgements:
An immeasurable debt of gratitude is due to the early USDA Forest
Service scientists who designed and implemented many of the studies at
the FEF - their names can be found in the list of references. Equally
important are the generations of field and lab technicians who assured
that this research was conducted carefully and consistently: Bud
Fridley, John Campbell, Doug Owens, Clifford Phillips, Melvin Owens,
Chris Cassidy, Emmett Fox, John Pierce, Cheryl Wiles, and Frederica
Wood, who has served as the data manager for the Fernow. Funding for
this research was provided, in part, by the Long Term Research in
Environmental Biology (LTREB) program at the National Science Foundation
(Grant Nos. DEB0417678 and DEB-1019522) to West Virginia University; and
by the National Science Foundation (Grant Nos OIA-148952) and the USDA
National Institute of Food and Agriculture Hatch project (Grant Nos
1004360), both to Zegre.
Keywords:
Long-term datasets, Forest Management, Fernow Experimental Forest,
Experimental Catchments, Hydrological Processes.
Abstract:
Long-term experimental watershed studies have significantly influenced
our global understanding of hydrological processes. The discovery and
characterization of how stream water quantity and quality respond to a
changing environment (e.g., land use change and acidic deposition) has
only been possible due to the establishment of catchments devoted to
long-term study. One such catchment is the Fernow Experimental Forest
(FEF) located in the headwaters of the Appalachian Mountains in West
Virginia, a region that provides essential freshwater ecosystem services
to eastern and mid-western USA communities. Established in 1934, the FEF
is among the earliest experimental watershed studies in the Eastern USA
that continues to address emergent challenges to forest ecosystems,
including climate change and other threats to forest health. This data
note summarizes some of the seminal findings from more than 50 years of
hydrologic research in the FEF. During the first few decades, research
at the FEF focused on the relationship between forest management and
hydrological processes – especially those related to the overall water
balance. Later, research efforts included the examination of
interactions between hydrology and soil erosion, biogeochemistry,
N-saturation, and acid deposition. Hydro-climatologic and water quality
datasets from long-term measurements and data from short-duration
studies are publicly available to provide new insights and foster
collaborations that will continue to advance our understanding of
hydrology in forested headwater catchments. As a result of its rich
history of research and abundance of long-term data, the FEF is uniquely
positioned to continue to advance understanding of forest ecosystems in
a time of unprecedented change.
Main text:
The Fernow Experimental Forest
Long-term research in small gauged forested watersheds within the USDA
Forest Service Experimental Forest and Range network (USDA-EFR) has
contributed substantially to current management of forests (Vose et al.,
2012). In 1934, the USDA Forest Service Fernow Experimental Forest (FEF)
was established to study mixed hardwood silviculture practices of the
Appalachian Mountain region. FEF is located in Tucker County, West
Virginia (39°03’N, 79°40’W) within the Monongahela National Forest.
Elevation ranges from 706 - 843 m. As part of the USDA-EFR network, FEF
has contributed to many comparative studies (e.g. Vose et al., 2012;
Amatya et al., 2016), and research from the FEF has produced numerous
publications that assess the impacts of forest management on ecosystem
processes (Hornbeck et al., 1993) and water quality. Additionally,
ecosystem responses to the chronic chemical stressors have been the
subject of both long-term acidification experiments (Adams et al., 2006)
and observational studies of ecosystem responses to nitrogen saturation
(Stoddard, 1994; Peterjohn et al., 1996; Rose et al., 2015). In this
data note, we summarize some of the seminal findings from 50+ years of
hydrological research at the FEF. Hydro-climatologic and water quality
datasets are presented that represent long-term monitoring and short
duration studies; we conclude with opportunities for scientific
collaboration and data sharing that will advance forest management and
hydrologic understanding.
FEF’s mean annual air temperature is 9.3 °C while mean monthly
temperatures range from -2.8 °C in January to 20.4 °C in July (Adams et
al., 2012). In the last 60 years the mean annual air temperature
increased 0.01 °C yr-1, with minimum temperature
increasing 0.02 °C yr-1 and the maximum temperature
remaining relatively constant (Young et al., 2019). Mean annual
precipitation is 1458 mm (Adams et al., 2012) and is distributed evenly
throughout the year. The precipitation regime has been relatively
constant during the last 60 years (Young et al., 2019). Growing season
precipitation is associated with convectional thunderstorms while
dormant season precipitation is associated with frontal systems (Adams
et al., 2012). Stream discharge (m3/s) is dominated by
baseflow with flashy storm flow occurring rapidly after precipitation
events. Mean annual runoff (mm) in the reference watershed (WS 4) is 642
mm and evapotranspiration averages 816 mm, indicating that 56% of the
rainfall in WS4 returns to the atmosphere as evapotranspiration.
Vegetation at the FEF is dominated by mixed mesophytic forest, including
over 500 hundred species of vascular plants (Madarish et al., 2002).
Common overstory species include red oak (Quercus rubra ), sugar
maple (Acer saccharum ), yellow poplar (Liriodendron
tulipifera ), black cherry (Prunus serotina ) and other broadleaf
Appalachian Forest species (Madarish et al., 2002). Soils are shallow
(<1 m), loamy-skeletal, and well-drained with steep slopes
averaging 16% (Adams et al. 2012). FEF has 10 gauged watersheds (Figure
1) including three reference (WS 4, 10 and 13 established in 1951, 1988,
and 1993 respectively), one conversion from broadleaved forest to a
Norway spruce (Picea abies ) stand in 1973 (WS 6), and one (WS 3)
that has been fertilized/acidified from 1989-2020. The remaining have
been disturbed by varying degrees of harvesting practices (WS 2, 5, 7).
Watershed 14 contains WS 6, 7 and 13 (Figure 1).
[Insert Figure 1 here]
FEF contributions to scientific understanding of hydrological
processes