Uniform shrub growth response to June temperature across the North Slope of Alaska

Daniel E. Ackerman, Daniel Griffin, Sarah E. Hobbie, Kelly Popham, Erin Jones, Jacques C. Finlay

Research output: Contribution to journalArticlepeer-review

24 Scopus citations


The expansion of woody shrubs in arctic tundra alters many aspects of high-latitude ecosystems, including carbon cycling and wildlife habitat. Dendroecology, the study of annual growth increments in woody plants, has shown promise in revealing how climate and environmental conditions interact with shrub growth to affect these key ecosystem properties. However, a predictive understanding of how shrub growth response to climate varies across the heterogeneous landscape remains elusive. Here we use individual-based mixed effects modeling to analyze 19 624 annual growth ring measurements in the stems of Salix pulchra (Cham.), a rapidly expanding deciduous shrub. Stem samples were collected at six sites throughout the North Slope of Alaska. Sites spanned four landscapes that varied in time since glaciation and hence in soil properties, such as nutrient availability, that we expected would modulate shrub growth response to climate. Ring growth was remarkably coherent among sites and responded positively to mean June temperature. The strength of this climate response varied slightly among glacial landscapes, but in contrast to expectations, this variability was not systematically correlated with landscape age. Additionally, shrubs at all sites exhibited diminishing marginal growth gains in response to increasing temperatures, indicative of alternative growth limiting mechanisms in particularly warm years, such as temperature-induced moisture limitation. Our results reveal a regionally-coherent and robust shrub growth response to early season growing temperature, with local soil properties contributing only a minor influence on shrub growth. Our conclusions strengthen predictions of changes to wildlife habitat and improve the representation of tundra vegetation dynamics in earth systems models in response to future arctic warming.

Original languageEnglish (US)
Article number044013
JournalEnvironmental Research Letters
Issue number4
StatePublished - Apr 2018

Bibliographical note

Funding Information:
We thank Toolik Field Station and the Arctic LTER (National Science Foundation grants #1026843 and #1637459) for valuable logistics support and guidance during this project. We also thank Dr. Benjamin Jones (US Geological Survey) for generously hosting DEA at Inigok Field Facility (Bureau of Land Management) and Teshekpuk Lake Observatory to sample at Inigok. Climate datasets for Kuparuk, Brooks Range, and Itkillik landscapes were provided by the Toolik Field Station Environmental Data Center; this material is based upon work supported by the National Science Foundation grants #455541 and #1048361. Financial support was provided by the Dayton Fund from the Bell Museum of Natural History, Explorers Club, National Science Foundation Graduate Research Fellowships Program (grant #00039202), the University of Minnesota Undergraduate Research Opportunities Program, and the University of Minnesota Department of Ecology, Evolution, and Behavior. Melissa Markay and Lucas Veitch helped process shrub samples.

Publisher Copyright:
© 2018 The Author(s). Published by IOP Publishing Ltd.


  • Arctic
  • climate change
  • dendroecology
  • glacial history
  • shrubs
  • tundra


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