Tall shrub and tree expansion in Siberian tundra ecotones since the 1960s.
about
Range Expansion of Moose in Arctic Alaska Linked to Warming and Increased Shrub HabitatGenetic data from algae sedimentary DNA reflect the influence of environment over geographyCircumpolar arctic tundra biomass and productivity dynamics in response to projected climate change and herbivory.Treeline advances along the Urals mountain range - driven by improved winter conditions?Environmental Limits of Tall Shrubs in Alaska's Arctic National Parks.Novel wildlife in the Arctic: the influence of changing riparian ecosystems and shrub habitat expansion on snowshoe hares.Shrubline but not treeline advance matches climate velocity in montane ecosystems of south-central Alaska.Warming and provenance limit tree recruitment across and beyond the elevation range of subalpine forest.Different parts, different stories: climate sensitivity of growth is stronger in root collars vs. stems in tundra shrubs.Large impacts of climatic warming on growth of boreal forests since 1960Ecological consequences of the expansion of N₂-fixing plants in cold biomes.Defining functional biomes and monitoring their change globally.Moss Mediates the Influence of Shrub Species on Soil Properties and Processes in Alpine Tundra.Dissimilar responses of larch stands in northern Siberia to increasing temperatures - a field and simulation based study.A comparison of sedimentary DNA and pollen from lake sediments in recording vegetation composition at the Siberian treeline.Phenology and species determine growing-season albedo increase at the altitudinal limit of shrub growth in the sub-Arctic.Diverging shrub and tree growth from the Polar to the Mediterranean biomes across the European continent.Salix arctica changes root distribution and nutrient uptake in response to subsurface nutrients in High Arctic deserts.Warming-induced upward migration of the alpine treeline in the Changbai Mountains, northeast China.Terrestrial biosphere models underestimate photosynthetic capacity and CO2 assimilation in the Arctic.Green alder (Alnus viridis) encroachment shapes microbial communities in subalpine soils and impacts its bacterial or fungal symbionts differently.Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change.Velocity of change in vegetation productivity over northern high latitudesSeasonal and Long-Term Changes to Active-Layer Temperatures after Tall Shrubland Expansion and Succession in Arctic TundraPan-Arctic ice-wedge degradation in warming permafrost and its influence on tundra hydrologySedimentary DNA versus morphology in the analysis of diatom-environment relationshipsThe Spatial Distribution and Ecological Impacts of Aeolian Soil Erosion in Kangerlussuaq, West GreenlandClimate warming as a driver of tundra shrubline advanceTemperature-induced recruitment pulses of Arctic dwarf shrub communitiesSiberian tundra ecosystem vegetation and carbon stocks four decades after wildfireRemote Sensing of Landscape Change in Permafrost Regions
P2860
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P2860
Tall shrub and tree expansion in Siberian tundra ecotones since the 1960s.
description
2014 nî lūn-bûn
@nan
2014 թուականի Փետրուարին հրատարակուած գիտական յօդուած
@hyw
2014 թվականի փետրվարին հրատարակված գիտական հոդված
@hy
2014年の論文
@ja
2014年論文
@yue
2014年論文
@zh-hant
2014年論文
@zh-hk
2014年論文
@zh-mo
2014年論文
@zh-tw
2014年论文
@wuu
name
Tall shrub and tree expansion in Siberian tundra ecotones since the 1960s.
@ast
Tall shrub and tree expansion in Siberian tundra ecotones since the 1960s.
@en
type
label
Tall shrub and tree expansion in Siberian tundra ecotones since the 1960s.
@ast
Tall shrub and tree expansion in Siberian tundra ecotones since the 1960s.
@en
prefLabel
Tall shrub and tree expansion in Siberian tundra ecotones since the 1960s.
@ast
Tall shrub and tree expansion in Siberian tundra ecotones since the 1960s.
@en
P2860
P356
P1476
Tall shrub and tree expansion in Siberian tundra ecotones since the 1960s.
@en
P2093
Howard E Epstein
P2860
P304
P356
10.1111/GCB.12406
P577
2014-02-12T00:00:00Z