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International Polar Year 2007–2008 - WMO

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most strongly along ponds and streams and areas with<br />

abundant moisture and nutrients. Similar changes<br />

have been observed by the BTF researchers in wetland<br />

vegetation of East Greenland, but changes in productive<br />

habitats in West Greenland over the past 42 years<br />

were not so dramatic. Changes in more barren rocky<br />

landscapes are less obvious in Canada, although there<br />

is strong increase in lichen cover that cause increased<br />

NDVI on these surfaces as well. A new satellite-derived<br />

data set (AVHRR GIMMS NDVI data) has permitted IPY-<br />

GOA to make the first analysis of NDVI trends in the<br />

High Arctic (north of 72°). Dry, unproductive sites in<br />

West Greenland and Svalbard re-visited after 70 years<br />

(Prach, 2010; Fig. 2.9-5) were also much smaller than<br />

those in the more productive habitats.<br />

In the Low Arctic, several GOA studies indicate<br />

that change is occurring most rapidly in areas<br />

Fig. 2.9-3. Mean monthly<br />

surface-air-temperature<br />

pattern for the Abisko<br />

region for different periods:<br />

(a) August 1913-2008, (b)<br />

August 2000-2008, (c)<br />

January 1913-2008, (d)<br />

January 2000-2008. For the<br />

August data, growth days<br />

above 5°C (GDD5) are used<br />

because of their importance<br />

for climate-impacts<br />

research.<br />

(From Yang et al., in press)<br />

where disturbance is most frequent. In the central<br />

Yamal Peninsula in West Siberia, Russia greening is<br />

concentrated in riparian areas and upland landslides<br />

associated with degrading massive ground ice, where<br />

low-willow shrublands replace the zonal sedge, dwarfshrub<br />

tundra growing on nutrient-poor sands (Walker<br />

et al., 2009; Walker et al., 2010 in press). Analysis of<br />

annual growth rings in the Varendei tundra of the<br />

Nenets Autonomous Okrug, Russia shows that willow<br />

growth is closely linked to the temperature record and<br />

increasing NDVI, demonstrating a clear relationship<br />

between deciduous shrub growth and Arctic warming<br />

(Forbes et al., 2009).<br />

In sub-Arctic Sweden, site re-visits under the<br />

BTF project over the past three decades showed<br />

dramatic changes in birch tree growth by a factor<br />

of six (Rundqvist et al., in press), recent invasion of<br />

s C I e n C e P r o g r a m 299

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