The climate is changing in many temperate forests with the amount of
forest area dominated by sugar maple experiencing an insulating
snowpack expected to shrink between 49 and 95% compared to 1951-2005
values. A reduced snowpack and increased depth and duration of soil
frost can injure fine roots, which are essential for plant water
uptake. Water uptake is a crucial component of ecosystem functioning
because this process strongly impacts other biological processes, such
as primary productivity and nutrient uptake. We evaluated the effects
of changing winter climate, including snow and soil frost dynamics, by
measuring sap flow rates in the Soil Freezing Study plots at the
Hubbard Brook Experimental Forest.
These data were gathered as part of the Hubbard Brook Ecosystem Study
(HBES). The HBES is a collaborative effort at the Hubbard Brook
Experimental Forest, which is operated and maintained by the USDA
Forest Service, Northern Research Station.
Analysis of these data are published in: Harrison, J.L., Reinmann,
A.B., Maloney, A.S. et al. Transpiration of
Dominant Tree Species Varies in Response to Projected Changes in
Climate: Implications for Composition and Water Balance of Temperate
Forest Ecosystems. Ecosystems (2020).
https://doi.org/10.1007/s10021-020-00490-y