B41K-0209:
Greater deciduous shrub abundance extends the annual period of maximum tundra greenness and increases modeled net CO2 uptake

Thursday, 18 December 2014
Shannan K Sweet1,2, Kevin L Griffin1,2, Heidi Steltzer3, Laura Gough4 and Natalie Boelman1,2, (1)Columbia University of New York, Palisades, NY, United States, (2)Lamont-Doherty Earth Observ., Palisades, NY, United States, (3)Fort Lewis College, Durango, CO, United States, (4)University of Texas at Arlington, Arlington, TX, United States
Abstract:
Satellite studies of the terrestrial Arctic report increased summer greening and longer green seasons over the past several decades, which may increase productivity and lengthen the period of carbon uptake. These trends have been attributed largely to increasing air temperatures and reduced snow cover duration. However, deciduous shrubs are concurrently becoming increasingly abundant in tundra landscapes, which may also impact canopy phenology and productivity. Our aim in this research was to determine the influence of greater deciduous shrub abundance on tundra canopy phenology and subsequent impacts on net ecosystem carbon exchange (NEE) over the growing season in the northern foothills of the Brooks Range, Alaska (68º38’ N, 149º34’ W). We compared deciduous shrub-dominated and evergreen/graminoid-dominated community-level canopy phenology using the normalized difference vegetation index (NDVI) and piecewise linear regression modeling. We used a tundra plant-community specific leaf area index (LAI) model to estimate LAI throughout the season. We then used a tundra specific NEE model to estimate the impact of greater deciduous shrub abundance and associated shifts in leaf area and canopy phenology on tundra carbon flux. We found that deciduous shrub canopies reached the onset of maximum greenness significantly earlier than evergreen/graminoid canopies, but both communities reached the onset of senescence at similar times, resulting in a net extension of the peak green season in deciduous shrub communities compared to evergreen/graminoid communities. The combined effect of a longer peak green season and greater leaf area of deciduous shrub canopies increased the net carbon uptake in deciduous shrub communities compared to evergreen/graminoid communities. However, the longer peak season alone significantly increased carbon uptake in deciduous shrub communities, suggesting that greater deciduous shrub abundance increases carbon uptake not only due to greater leaf area, but also due to an extension of the period of maximum greenness and thus the period of peak carbon uptake.