Circumpolar arctic tundra biomass and productivity dynamics in response to projected climate change and herbivory

Abstract Satellite remote sensing data have indicated a general ‘greening’ trend in the arctic tundra biome. However, the observed changes based on remote sensing are the result of multiple environmental drivers, and the effects of individual controls such as warming, herbivory, and other disturbanc...

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Bibliographic Details
Published in:Global Change Biology
Main Authors: Yu, Qin, Epstein, Howard, Engstrom, Ryan, Walker, Donald
Other Authors: National Aeronautics and Space Administration, National Science Foundation
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2017
Subjects:
Online Access:http://dx.doi.org/10.1111/gcb.13632
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgcb.13632
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.13632
https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.13632
https://onlinelibrary.wiley.com/doi/am-pdf/10.1111/gcb.13632
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Summary:Abstract Satellite remote sensing data have indicated a general ‘greening’ trend in the arctic tundra biome. However, the observed changes based on remote sensing are the result of multiple environmental drivers, and the effects of individual controls such as warming, herbivory, and other disturbances on changes in vegetation biomass, community structure, and ecosystem function remain unclear. We apply ArcVeg, an arctic tundra vegetation dynamics model, to estimate potential changes in vegetation biomass and net primary production ( NPP ) at the plant community and functional type levels. ArcVeg is driven by soil nitrogen output from the Terrestrial Ecosystem Model, existing densities of Rangifer populations, and projected summer temperature changes by the NCAR CCSM 4.0 general circulation model across the Arctic. We quantified the changes in aboveground biomass and NPP resulting from (i) observed herbivory only; (ii) projected climate change only; and (iii) coupled effects of projected climate change and herbivory. We evaluated model outputs of the absolute and relative differences in biomass and NPP by country, bioclimate subzone, and floristic province. Estimated potential biomass increases resulting from temperature increase only are approximately 5% greater than the biomass modeled due to coupled warming and herbivory. Such potential increases are greater in areas currently occupied by large or dense Rangifer herds such as the Nenets‐occupied regions in Russia (27% greater vegetation increase without herbivores). In addition, herbivory modulates shifts in plant community structure caused by warming. Plant functional types such as shrubs and mosses were affected to a greater degree than other functional types by either warming or herbivory or coupled effects of the two.