Vegetation change in Southeast Greenland? Tasiilaq revisited after 40 years

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F11%3A00054652" target="_blank" >RIV/00216224:14310/11:00054652 - isvavai.cz</a>
Result on the web
<a href="http://onlinelibrary.wiley.com/doi/10.1111/j.1654-109X.2010.01107.x/abstract" target="_blank" >http://onlinelibrary.wiley.com/doi/10.1111/j.1654-109X.2010.01107.x/abstract</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1111/j.1654-109X.2010.01107.x" target="_blank" >10.1111/j.1654-109X.2010.01107.x</a>

Result language
angličtina
Original language name
Vegetation change in Southeast Greenland? Tasiilaq revisited after 40 years
Original language description
Questions: Are there changes in species composition of the oceanic, Low-Arctic tundra vegetation after 40 years? Can possible changes be attributed to climate change? Location: Ammassalik Island near Tasiilaq, Southeast Greenland. Methods: Species composition and cover of 11 key vegetation types were recorded in 110 vegetation survey plots in 1968?1969 and in 11 permanent plots in 1981. Recording was repeated in 2007. Temporal changes in species composition and cover between the surveys were tested using permutation tests linked with constrained ordinations for vegetation types, and Mann?Whitney tests for individual species. Changes in vegetation were related to climate change. Results: Although climate became warmer over the studied period, most of the vegetation types showed minor changes. The changes were most conspicuous in mire and snowbed vegetation, such as the Carex rariflora mire and Hylocomium splendens snowbed. In the C.
Czech name
—
Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
EF - Botany
OECD FORD branch
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Publication year
2011
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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