HR: 0800h
AN: B51C-0608 [Abstracts]
TI: Effects of Deeper Snow on Ecosystem CO2 Fluxes in Tussock Tundra in Northern Alaska
AU: * Taneva, L
EM: lina.taneva@gmail.com
AF: University of Alaska Anchorage, Environment and Natural Resources Institute
707 A Street, Anchorage, AK 99501, United States
AU: Sullivan, P F
EM: paddy@uaa.alaska.edu
AF: University of Alaska Anchorage, Department of Biological Sciences, Anchorage, AK 99508, United States
AU: Sveinbjornsson, B
EM: afbs@uaa.alaska.edu
AF: University of Alaska Anchorage, Department of Biological Sciences, Anchorage, AK 99508, United States
AU: Welker, J M
EM: afjmw1@uaa.alaska.edu
AF: University of Alaska Anchorage, Environment and Natural Resources Institute
707 A Street, Anchorage, AK 99501, United States
AB:
Climate warming in northern latitudes is projected to lead to increased precipitation and, therefore, increased
snow depth in arctic ecosystems. Deeper snow in winter can affect these ecosystems by leading to warmer
soils, shorter growing seasons, and increased water availability to plants after snow melt, with subsequent
implications to ecosystem biogeochemical cycling. Increases in snow depth in the arctic have been reported to
lead to changes in plant community composition and, particularly, increases in shrub abundance in tundra
ecosystems. Because of the confounded effects of greater snow depth on arctic ecosystems, it is unclear what
the mechanisms underlying observed shrub cover changes are. In this study, we investigated the differential
effects of greater snow depth on ecosystem CO2 exchange in tussock tundra near Toolik Lake, Alaska. We
measured CO2 uptake and ecosystem respiration throughout the growing season after the first winter of
snow depth manipulation and compared these results to CO2 exchange in plots under long-term (14 years)
snow depth increase. Our initial findings indicate that long-term increases in snow result in greater relative
increases in respiration as opposed to ecosystem photosynthesis, leading to greater net CO2 efflux.
However, in the first year of snow additions, these differences were not observed, nor were there any differential
effects of winter warming only, or winter warming with added water on CO2 exchange.
DE: 4806 Carbon cycling (0428)
DE: 4815 Ecosystems, structure, dynamics, and modeling (0439)
SC: Biogeosciences [B]
MN: 2007 Fall Meeting