Spatial Variability of the Dominant Climate Signal in <i>Cassiope tetragona</i> from Sites in Arctic Canada

<span style="font-family: 'Times New Roman'; color: #221e1f;">Our study investigates the nature of the climate signal in three populations of the Arctic dwarf-shrub <em>Cassiope tetragona </em>using dendrochronological and stable isotope...

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Bibliographic Details
Published in:ARCTIC
Main Authors: Rayback, Shelly A., Lini, Andrea, Henry, Gregory H.R.
Format: Article in Journal/Newspaper
Language:unknown
Published: The Arctic Institute of North America 2011
Subjects:
Online Access:http://dx.doi.org/10.14430/arctic4083
http://arctic.journalhosting.ucalgary.ca/arctic/index.php/arctic/article/viewFile/4083/4056
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Summary:<span style="font-family: 'Times New Roman'; color: #221e1f;">Our study investigates the nature of the climate signal in three populations of the Arctic dwarf-shrub <em>Cassiope tetragona </em>using dendrochronological and stable isotope analysis techniques. We present 15 new <em>C. tetragona </em>chronologies from three sites (Axel Heiberg, Bathurst, and Devon islands) in the eastern Canadian Arctic, of which three are the first continuous stable carbon isotope ratio (δ¹³C) time series developed for Arctic shrubs. Correlation and multivariate regression analyses revealed that multiple and different climate factors influenced the chronologies within and between the three sites. At the Axel Heiberg Island site, the dominant climatic influences over annual stem elongation were previous year (t-1) and current year (t) summer precipitation, while annual production of flower buds was influenced by (t) winter precipitation and spring temperature. At Bathurst Island, annual production of flower buds responded to (t-1) growing season sunshine hours and winter precipitation and to (t) late growing season temperature and moisture availability. Our analysis of the Axel </span><span style="font-family: 'Times New Roman'; color: black;">H</span><span style="font-family: 'Times New Roman'; color: #221e1f;">eiberg and Bathurst Island models revealed the positive influence on δ</span><span style="font-family: 'Times New Roman'; color: #221e1f;">13</span><span style="font-family: 'Times New Roman'; color: #221e1f;">C values of (t-1) winter temperature—and on </span><span style="font-family: 'Times New Roman'; color: black;">B</span><span style="font-family: 'Times New Roman'; color: #221e1f;">athurst Island only, of (t-1) spring sunshine hours. The combined influence of these parameters on ...