Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Measurement and modeling of bryophyte evaporation in a boreal forest chronosequence

Journal Article · · Ecohydrology, 4(1):26–35
DOI:https://doi.org/10.1002/eco.118· OSTI ID:1004014

The effects of changing climate and disturbance on forest water cycling are not well understood. In particular bryophytes contribute significantly to forest evapotranspiration (ET) in poorly-drained boreal forests, but few studies have directly measured this flux and how it changes with stand age and soil drainage. We used large chambers to measure bryophyte evaporation (E) in Canadian Picea mariana forests of varying ages and soil drainages, as well under controlled laboratory conditions, and modeled daily E using site-specific meteorological data to drive a Penman-Monteith-based model. Field measurements of E averaged 0.37 mm day-1, and ranged from 0.03 (Pleurozium schreberii in a 77-year-old dry stand) to 1.43 mm day-1 (Sphagnum riparium in a 43-year-old bog). canopy resistance ranged from ~0 (at 25 °C, some values were <0) to ~1500 s m-1 for dry, cold (5 °C) mosses. In the laboratory, moss canopy resistance was constant until a moss water content of ~6 g g-1 and then climbed sharply with further drying; no difference was observed between the three moss groups (feather mosses, hollow mosses, and hummock mosses) tested. Modeled annual E fluxes from bryophytes ranged from 0.4 mm day-1, in the well-drained stands, to ~1 mm day-1 in the 43-year-old bog, during the growing season. Eddy covariance data imply that bryophytes contributed 18-31% and 49-69% to the total ET flux, at the well- and poorly-drained stands respectively. Bryophyte E was greater in bogs than in upland stands, was driven by low-lying mosses, and did not vary with stand age; this suggests that shifts in forest age due to increasing fire will have little effect on the bryophyte contribution to ET.

Research Organization:
Pacific Northwest National Laboratory (PNNL), Richland, WA (US)
Sponsoring Organization:
USDOE
DOE Contract Number:
AC05-76RL01830
OSTI ID:
1004014
Report Number(s):
PNNL-SA-65105; 400408000
Journal Information:
Ecohydrology, 4(1):26–35, Journal Name: Ecohydrology, 4(1):26–35 Journal Issue: 1 Vol. 4
Country of Publication:
United States
Language:
English

Similar Records

Effects of fire on regional evapotranspiration in the central Canadian boreal forest
Journal Article · Wed Apr 08 00:00:00 EDT 2009 · Global Change Biology, 15(5):1242-1254 · OSTI ID:959148

Effects of bryophytes on succession from alkaline marsh to Sphagnum bog
Journal Article · Fri Oct 01 00:00:00 EDT 1982 · Am. Midl. Nat.; (United States) · OSTI ID:6542769

Comparison of tree transpiration under wet and dry canopy conditions in a Costa Rican premontane tropical forest
Journal Article · Sat Jul 16 00:00:00 EDT 2016 · Hydrological Processes · OSTI ID:1467619