Buffam, Ishi
- University of Cincinnati
Sammanfattning
Evapotranspiration rates (ET) from contrasting Wisconsin bogs (one forested bog, one open bog) were compared over 4 years by analyzing diel oscillations of their water tables. Daily rates of ET from peatlands were also compared to rates of evaporation (E) from encircled bog ponds. We hypothesized that ET would be higher in the forested bog due to the greater leaf area index of forest canopy relative to moss and ericaceous shrubs. We also hypothesized that ET in peatlands would exceed the physical process of E from encircled ponds. Field data supported the first hypothesis, but the second only proved true for the forested peatland. Daily estimates of peatland ET varied widely, ranging from similar to 1 to > 10 mm/d; but average ET was higher in the forested peatland (4.04 vs. 3.09 mm/d; p < .01). Average ET in the forested peatland was also higher than E during summer (4.04 vs. 3.31 mm/d; p
Nyckelord
evaporation; evapotranspiration; northern peatlands; water table fluctuations
Publicerad i
Ecohydrology
2017, volym: 10, nummer: 4, artikelnummer: e1834
Utgivare: WILEY
SLU författare
UKÄ forskningsämne
Ekologi
Publikationens identifierare
- DOI: https://doi.org/10.1002/eco.1834
Permanent länk till denna sida (URI)
https://res.slu.se/id/publ/109556