The global increase in surface air temperature has produced an overall lengthening of the growing season by 3-5 days/decade in the Northern Hemisphere during the last 30 years. The direct impact of a longer growing season has not been well documented for Sphagnum moss communities in the Arctic. We hypothesized that an increase in the growing season length may be detrimental to Sphagnum growth as a result of photoinhibition caused by the plants emerging from snow near the seasonal peak of solar irradiance. We conducted an experiment from 1999 to 2002, lengthening the growing season in arctic Alaska, to determine the effects that this simulation of climate change had on the growth of hollows dominated by Sphagnum angustifolium. The lengthened growing season was associated with a decrease in annual moss height increment of 78 and 69 % for 1999 and 2000, respectively. These growth reductions may be related to freeze/thaw episodes and prolonged periods of cold in those years. The growth of individuals exposed to snow removal was also reduced by high global radiation. Overall, snow removal did not significantly affect the seasonal dynamics of growth, but seasonal patterns of growth strongly differed among years. These differences in seasonal dynamics suggest that Sphagnum growth is driven by opportunistic responses to favorable conditions rather than ontogenetic drivers. In addition, we compared environmental variation and growth between control and snow removal plots. Growth of Sphagnum in both treatments was stimulated by warmer soil temperatures and drier conditions. With earlier snowmelt as a result of warmer temperatures, it is likely that S. angustifolium will be subjected to higher levels of radiation and possibly greater photoinhibition which may lead to lower growth rates and significant implications for moss production in tussock tundra.