Arctic and boreal ecosystems of western North America as components of the climate system
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Diel Variation of Biogenic Volatile Organic Compound Emissions--A field Study in the Sub, Low and High Arctic on the Effect of Temperature and LightMid-latitude afforestation shifts general circulation and tropical precipitationEcosystem responses to climate change at a Low Arctic and a High Arctic long-term research siteSoil moisture's underestimated role in climate change impact modelling in low-energy systems.Patterns in CH4 and CO2 concentrations across boreal rivers: Major drivers and implications for fluvial greenhouse emissions under climate change scenarios.Dispersal limitation drives successional pathways in Central Siberian forests under current and intensified fire regimes.Trade-offs between three forest ecosystem services across the state of New Hampshire, USA: timber, carbon, and albedo.Regional atmospheric cooling and wetting effect of permafrost thaw-induced boreal forest loss.Persistent and pervasive compositional shifts of western boreal forest plots in Canada.Barren-ground caribou (Rangifer tarandus groenlandicus) behaviour after recent fire events; integrating caribou telemetry data with Landsat fire detection techniques.Interactive effects between plant functional types and soil factors on tundra species diversity and community composition.Frequent fires in ancient shrub tundra: implications of paleorecords for arctic environmental changeChanges in Arctic vegetation amplify high-latitude warming through the greenhouse effect.Enzymology under global change: organic nitrogen turnover in alpine and sub-Arctic soils.Conceptualising the interactive effects of climate change and biological invasions on subarctic freshwater fish.Effects of biotic feedback and harvest management on boreal forest fire activity under climate change.Litter stoichiometric traits of plant species of high-latitude ecosystems show high responsiveness to global change without causing strong variation in litter decomposition.Nitrification rates in Arctic soils are associated with functionally distinct populations of ammonia-oxidizing archaea.Growth and phenology of three dwarf shrub species in a six-year soil warming experiment at the alpine treeline.Natural disturbance impacts on ecosystem services and biodiversity in temperate and boreal forests.Uncertainty analysis of vegetation distribution in the northern high latitudes during the 21st century with a dynamic vegetation model.Direct and indirect climate change effects on carbon dioxide fluxes in a thawing boreal forest-wetland landscape.Estimating changes in lichen mat volume through time and related effects on barren ground caribou (Rangifer tarandus groenlandicus) movementHistorical and projected trends in landscape drivers affecting carbon dynamics in Alaska.Do the energy fluxes and surface conductance of boreal coniferous forests in Europe scale with leaf area?Experimental warming alters potential function of the fungal community in boreal forest.Comparison of Ant Community Diversity and Functional Group Composition Associated to Land Use Change in a Seasonally Dry Oak Forest.Latent heat exchange in the boreal and arctic biomes.Delayed spring phenology on the Tibetan Plateau may also be attributable to other factors than winter and spring warming.Interactive effects of temperature and habitat complexity on freshwater communities.Potential shifts in dominant forest cover in interior Alaska driven by variations in fire severity.Sensitivity of Siberian larch forests to climate changeExperimental warming and burn severity alter soil CO2 flux and soil functional groups in a recently burned boreal forestEvidence and implications of recent and projected climate change in Alaska's forest ecosystemsRecent shift in Eurasian boreal forest greening response may be associated with warmer and drier summersVegetation-microclimate feedbacks in woodland-grassland ecotonesExpanding forests and changing growth forms of Siberian larch at the Polar Urals treeline during the 20th centuryVariability of groundwater levels and total organic carbon in the riparian zone of a boreal catchmentIs carbon within the global terrestrial biosphere becoming more oxidized? Implications for trends in atmospheric O2Shifted energy fluxes, increased Bowen ratios, and reduced thaw depths linked with drainage-induced changes in permafrost ecosystem structure
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Arctic and boreal ecosystems of western North America as components of the climate system
description
im Dezember 2000 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
@nl
наукова стаття, опублікована в грудні 2000
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name
Arctic and boreal ecosystems of western North America as components of the climate system
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Arctic and boreal ecosystems of western North America as components of the climate system
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type
label
Arctic and boreal ecosystems of western North America as components of the climate system
@en
Arctic and boreal ecosystems of western North America as components of the climate system
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prefLabel
Arctic and boreal ecosystems of western North America as components of the climate system
@en
Arctic and boreal ecosystems of western North America as components of the climate system
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P2093
P2860
P1476
Arctic and boreal ecosystems of western North America as components of the climate system
@en
P2093
A. D. Mcguire
D. Baldocchi
E. B. Rastetter
E. Kasischke
F. S. Chapin
J. Randerson
S. A. Zimov
S. E. Hobbie
P2860
P304
P356
10.1046/J.1365-2486.2000.06022.X
P577
2000-12-01T00:00:00Z