2012
DOI: 10.1007/978-94-007-4569-8_3
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Climate Changes in Siberia

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Cited by 45 publications
(37 citation statements)
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“…As a consequence, a progressive shift from N limitation to P limitation or N-P co-limitation can occur (Ågren et al, 2012;Peñuelas et al, 2012;Vitousek et al, 2010). These modifications of biogeochemical cycling on global and regional scales will participate in the way ecosystem reshaping is driven, for example through the modification of plant communities as they adapt to new stoichiometric constraints (Güsewell, 2004). It may also have consequences for agricultural potential on these scales.…”
Section: Introductionmentioning
confidence: 99%
“…As a consequence, a progressive shift from N limitation to P limitation or N-P co-limitation can occur (Ågren et al, 2012;Peñuelas et al, 2012;Vitousek et al, 2010). These modifications of biogeochemical cycling on global and regional scales will participate in the way ecosystem reshaping is driven, for example through the modification of plant communities as they adapt to new stoichiometric constraints (Güsewell, 2004). It may also have consequences for agricultural potential on these scales.…”
Section: Introductionmentioning
confidence: 99%
“…Permafrost vulnerability to climate change may be underestimated unless effects of wildfire are considered [12]. Although wildfire in boreal forests is a natural phenomenon, its frequency increased significantly [37,38]. Mean fire return in Siberia ranges from 20 to 350 years, with a drastic increase in the southern part due to frequent dry seasons and changes in human behavior [39,40].…”
Section: Resultsmentioning
confidence: 99%
“…The decreased glaciation of the Arctic Sea influenced warm sea currents and formation of intensive northwestern transfer of wet air masses from the north of Fennoscandia increasing the precipitation over Siberia. The total annual precipitation rate was approximately 25 mm higher than today (Groisman et al, 2013). One of the available humidity reconstructions shows the maximum level of wetness of the Holocene during the Boreal period (Blyakharchuk, 2009).…”
Section: Discussionmentioning
confidence: 99%
“…The pollen-based postglacial long-term climate reconstructions for Western Siberia (Blyakharchuk, 2009; Groisman et al, 2013) distinguish drier and wetter time periods. The increased precipitation or decreased runoff probably influenced the rivers; however, there is only limited knowledge on the postglacial palaeoecology, including the flooding history from the Ob region.…”
Section: Introductionmentioning
confidence: 99%