Evaporation dominates evapotranspiration on Alaska’s Arctic Coastal Plain

• Published in: Arctic, Antarctic, and Alpine Research
• Main Authors: Jessica M. Young-Robertson, Naama Raz-Yaseef, Lily R. Cohen, Brent Newman, Thom Rahn, Victoria Sloan, Cathy Wilson, Stan D. Wullschleger
• Format: Article in Journal/Newspaper
• Language: English
• Published: Taylor & Francis Group 2018
• Subjects: polygonal ground; permafrost; ice wedge; plant functional type; evapotranspiration partitioning; Environmental sciences; GE1-350; Ecology; QH540-549.5; Arctic; Antarctic and Alpine Research; Ice; wedge*
• Online Access: https://doi.org/10.1080/15230430.2018.1435931; https://doaj.org/article/2276b0fdbddd4a9ebb235f984ac887f1

The dynamics of evapotranspiration (ET), such as the partitioning to evaporation and transpiration, of polygonal ground on the Arctic Coastal Plain are not well understood. We assessed ET dynamics, including evaporation and transpiration partitioning, created by microtopographic features associated with high- and low-centered polygons. Chamber ET and leaf-level transpiration measurements were conducted in one-week field campaigns in two growing seasons with contrasting weather conditions. We found that ET was greater in the drier and warmer sampling period (2013) compared to the colder and wetter one (2014). Evaporation dominated ET, particularly in the wetter and colder sampling period (>90% in 2014 vs. 80% in 2013). In the 2013 sampling period, wetter and warmer conditions increased ET and the contribution of transpiration to ET. If the soils warm with degrading permafrost, ET and the fraction contributed by transpiration may increase to a certain threshold, when moisture must increase with rising temperatures to further increase these fluxes. While the fraction of transpiration may rise with warmer soils, it is unlikely that transpiration will completely dominate ET. This work highlights the complexities of understanding ET in this dynamic environment and the importance of understanding differences across polygonal ground.