Date of this Version
5-1-2015
Document Type
Article
Abstract
Few studies have clearly linked long-term monitoring with insitu experiments to clarify potential drivers of observed change at a given site. This is especially necessary when findings from a site are applied to a much broader geographic area. Here, we document vegetation change at Barrow and Atqasuk, Alaska, occurring naturally and due to experimental warming over nearly two decades. An examination of plant cover, canopy height, and community indices showed more significant differences between years than due to experimental warming. However, changes with warming were more consistent than changes between years and were cumulative in many cases. Most cases of directional change observed in the control plots over time corresponded with a directional change in response to experimental warming. These included increases in canopy height and decreases in lichen cover. Experimental warming resulted in additional increases in evergreen shrub cover and decreases in diversity and bryophyte cover. This study suggests that the directional changes occurring at the sites are primarily due to warming and indicates that further changes are likely in the next two decades if the regional warming trend continues. These findings provide an example of the utility of coupling insitu experiments with long-term monitoring to accurately document vegetation change in response to global change and to identify the underlying mechanisms driving observed changes.
Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.
Recommended Citation
Hollister, Robert D.; May, Jeremy L.; Kremers, Kelseyann S.; Tweedie, Craig E.; Oberbauer, Steven F.; Liebig, Jennifer A.; Botting, Timothy F.; Barrett, Robert T.; and Gregory, Jessica L., "Warming experiments elucidate the drivers of observed directional changes in tundra vegetation" (2015). Department of Biological Sciences. 89.
https://digitalcommons.fiu.edu/cas_bio/89
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Comments
Ecology and Evolution published by John Wiley & Sons Ltd.