Is the heart of the Fennoscandian rodent cycle still beating?.    From Wordnik.com.  [General characteristics of arctic species and their adaptations in the context of changes in climate and ultraviolet-B radiation levels] Reference

How much do weasels shape microtine cycles in the northern Fennoscandian taiga?.    From Wordnik.com.  [Effects of changes in climate and UV radiation levels on structure of arctic ecosystems in the short and long term] Reference

"Climate change and terrestrial wildlife management in the Fennoscandian North.".    From Wordnik.com.  [Climate change and terrestrial wildlife management in the Fennoscandian North] Reference

The Holocene coincides with the removal of the Laurentide and Fennoscandian ice sheets.    From Wordnik.com.  [A New Preprint by Wunsch on Abrupt Climate Change « Climate Audit] Reference

Forest tundra vegetation represented by the Fennoscandian mountain birch forest, Abisko, northern Sweden.    From Wordnik.com.  [Effects of changes in climate and UV radiation levels on structure of arctic ecosystems in the short and long term] Reference

Holocene climate reconstructions from the Fennoscandian tree-line area based on pollen data from Toskaljavri.    From Wordnik.com.  [Historical changes in freshwater ecosystems in the Arctic] Reference

Cladoceran and chironomid assemblages as quantitative indicators of water depth in subarctic Fennoscandian lakes.    From Wordnik.com.  [Effects of climate change on general hydro-ecology in the Arctic] Reference

The total initial depression is assumed to have been about 900 – 1,000 m when the Fennoscandian Ice Sheet was 3,400-3,700 m thick.    From Wordnik.com.  [Kvarken Archipelago High Coast, Finland and Sweden] Reference

Spatio-temporal variability and environmental controls of methane fluxes at the forest-tundra ecotone in the Fennoscandian mountains.    From Wordnik.com.  [Effects of changes in climate and UV radiation levels on function of arctic ecosystems in the short and long term] Reference

The disappearance of D-O events in the Holocene coincides with the disappearance also of the Laurentide and Fennoscandian ice sheets.    From Wordnik.com.  [A New Preprint by Wunsch on Abrupt Climate Change « Climate Audit] Reference

Immediately following the collapse of the Fennoscandian ice-sheet at the end of the ice-age, initial crustal rebound rates reached about 7.5 cm/yr.    From Wordnik.com.  [The Dutch experience of sea-level rise « Climate Audit] Reference

Holocene vegetational and limnological changes in the Fennoscandian tree-line area as documented by pollen and diatom records from Lake Tsuolbmajavri, Finland.    From Wordnik.com.  [Effects of climate change on hydro-ecology of contributing basins in the Arctic] Reference

In the Fennoscandian countries there is a strong tradition for hunters to report the number of animals killed, and hunters voluntarily assist in wildlife surveys.    From Wordnik.com.  [Climate change and terrestrial wildlife management in the Fennoscandian North] Reference

Consequently, the number of hunters living close to the land in the Fennoscandian Arctic is decreasing while those from urban centers outside the region are increasing.    From Wordnik.com.  [Climate change and terrestrial wildlife management in the Fennoscandian North] Reference

During the most recent of these, the Weichsel, the vast Fennoscandian glacier ice cap 3 km thick was centered on, and had its greatest volume directly over, the High Coast area.    From Wordnik.com.  [Kvarken Archipelago High Coast, Finland and Sweden] Reference

Norway and Greenland, the only Fennoscandian countries that have polar bears, are both signing members of the International Agreement on the Conservation of Polar Bears (IACPB).    From Wordnik.com.  [Management and conservation of marine mammals and seabirds in the Arctic] Reference

The Fennoscandian countries have established special snowmobile routes to concentrate this traffic and so prevent more widespread damage and disturbance to snow-covered habitats.    From Wordnik.com.  [Human impacts on the biodiversity of the Arctic] Reference

Furthermore, a common feature is distinct changes in growth sensitivity to climate at all sites during that period, a feature that has also been observed at several other Fennoscandian sites.    From Wordnik.com.  [Direct climate effects on tree growth in the Arctic] Reference

Management of wildlife in the Fennoscandian Arctic under conditions of a changing climate must be "adaptive" and thus capable of responding to changes in ecosystem dynamics that at times may be unpredictable and therefore unanticipated.    From Wordnik.com.  [Climate change and terrestrial wildlife management in the Fennoscandian North] Reference

As for the uplift of two more closely related non-World Heritage sites: that of the Skargard Archipelago off Stockholm lacks glacial till deposits; and that of the northern and western White Sea shores on the periphery of the Fennoscandian shield is only 1,0-2,5 mm per year.    From Wordnik.com.  [Kvarken Archipelago High Coast, Finland and Sweden] Reference

There is a need to establish a comprehensive monitoring program for all wildlife species (moose and some of the large carnivores are currently monitored within each country), with monitoring stations spread out over the Fennoscandian countries, and with coordination of these efforts.    From Wordnik.com.  [Climate change and terrestrial wildlife management in the Fennoscandian North] Reference

Whereas larger ice sheets existed on Earth at the outset of the last glacial termination, when the large Laurentian and Fennoscandian ice sheets began to melt, than during the Holocene, comparisons between climate forcings during the glacial termination and those operating since about 1750 may be instructive.    From Wordnik.com.  [21st century climate tipping points] Reference

Fennoscandian Tundra Ecosystems: Plants and Microorganisms.    From Wordnik.com.  [General characteristics of arctic species and their adaptations in the context of changes in climate and ultraviolet-B radiation levels] Reference

In the stable Fennoscandian craton, where the Swedish Forsmark and Finnish Olkiluoto sites are located, glacial cycles create an added hazard.    From Wordnik.com.  [Featured Articles] Reference

Title: “Reconstruction of Low- and High-Frequency Summer Temperature Changes From a Tree-Ring Archive of Fennoscandian Forest-Limit Scots Pine”.    From Wordnik.com.  [Juckes and the Indigirka River Alter Ego « Climate Audit] Reference

During periods of glaciation, however, two huge ice sheets, the British and the Fennoscandian, trapped water between the glacier to the north and the land barrier to the south.    From Wordnik.com.  [Telegraph.co.uk: news, business, sport, the Daily Telegraph newspaper, Sunday Telegraph] Reference

Of note is that the postglacial amplification of seismicity was not restricted to the areas beneath the large Laurentide and Fennoscandian ice sheets but also occurred in regions affected by smaller ice caps or lakes, e.g. the Basin-and-Range Province.    From Wordnik.com.  [Campaign against Climate Change aggregator] Reference

450,000 years ago during a glaciation (ice age), water became trapped between the British and Fennoscandian ice sheets, and an enormous glacial lake was formed bounded by glaciers in the north and the land bridge in the south.    From Wordnik.com.  [PhysOrg.com - latest science and technology news stories] Reference

With respect to Tornetrask quite simply I cannot recall why – I have subsequently compared some of the Fennoscandian data with Esper’s work – there are differences but I seem to recall the general trends are pretty similar.    From Wordnik.com.  [Crowley on Zhu [1973] « Climate Audit] Reference