2007
DOI: 10.1007/978-3-540-32730-1_24
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Responses of High Latitude Ecosystems to Global Change: Potential Consequences for the Climate System

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Cited by 34 publications
(28 citation statements)
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“…The exchange of water, energy and carbon between the surface and the atmosphere is determined by biogeophysical properties of the surface such as hydrology or albedo, as well as biogeochemical properties such as biomass, and vegetation type (Bonan et al, 1995;Chapin et al, 2005;McGuire et al, 2007). In both regional and global land surface and climate models, the biogeophysical parameters are estimated on the basis of land cover classifications.…”
Section: Introductionmentioning
confidence: 99%
“…The exchange of water, energy and carbon between the surface and the atmosphere is determined by biogeophysical properties of the surface such as hydrology or albedo, as well as biogeochemical properties such as biomass, and vegetation type (Bonan et al, 1995;Chapin et al, 2005;McGuire et al, 2007). In both regional and global land surface and climate models, the biogeophysical parameters are estimated on the basis of land cover classifications.…”
Section: Introductionmentioning
confidence: 99%
“…Although the proportion of burned area was small (e.g., ~4 % for the Lena watershed), the actual area covered was large with a 25 year fire return interval. Increased fire frequency and intensity have been observed in the second half of the 20th Century in Canada, Alaska and northern Eurasia (McGuire et al 2004(McGuire et al , 2007. Wildfires can destroy the insulating organic surface layer and warm the soil, increasing the rates of permafrost thaw and the active layer thickness Johnstone et al 2010).…”
Section: Carbon Mobilizationmentioning
confidence: 99%
“…Wildfires can destroy the insulating organic surface layer and warm the soil, increasing the rates of permafrost thaw and the active layer thickness Johnstone et al 2010). With subsequent regrowth of mosses the soils cool again, but with a warmer and drier climate, increased fire frequency and intensity may trigger a positive feedback loop between the loss of SOC and subsequent warming and thawing of permafrost soils (O'Donnell et al 2011;McGuire et al 2007). …”
Section: Carbon Mobilizationmentioning
confidence: 99%
“…With the drive of increasing temperature and aridity of climate, increasing and mostly unregulated anthropogenic impacts, Siberian terrestrial ecosystems are undergoing integral and inherent dynamics as well (McGuire et al, 2006;Shvidenko, 2009;Kurtsev, 2013), which affects the climate itself in turn, and the climate condition of other regions (Vinogradova et al, 2015), China for example. Siberia climate-land system change induced by variation of temperature and precipitation in Eurasian would have immediate impact on agriculture and ecology of China, especially for the northeast region, the greatest commodity grain base in China adjacent to Siberia.…”
Section: Introductionmentioning
confidence: 99%