Wetland and Lake Evaporation in the Low Arctic
- 1 May 1986
- journal article
- research article
- Published by Taylor & Francis in Arctic and Alpine Research
- Vol. 18 (2), 195-200
- https://doi.org/10.2307/1551129
Abstract
Evaporation from wetland and lake surfaces in the continuous permafrost region of the Low Arctic was studied using an energy balance Bowen ratio approach and lysimeter measurements respectively. Daily evaporation was also estimated using the Priestley-Taylor model. Over the summer, mean evaporation from the wetland and lake were similar, but day-to-day variation was large at times. Differences of available energy and surface roughness between the lake and wetland surface produce a larger Priestly-Taylor .alpha. value for wetland evaporation. The approach presented in this paper can be used to estimate evaporation for wetland and lake surfaces in the low arctic region.This publication has 4 references indexed in Scilit:
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- Evaporation from a sphagnum moss surfaceJournal of Hydrology, 1980
- Evaporation in high latitudesWater Resources Research, 1977
- Evaluation of an evapotranspirometer for peat bogsWater Resources Research, 1966