Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
about
Arctic plant diversity in the Early Eocene greenhouseMid-latitude afforestation shifts general circulation and tropical precipitationThe role of vegetation-microclimate feedback in promoting shrub encroachment in the northern Chihuahuan desert.Climate change and the past, present, and future of biotic interactions.How warm was the last interglacial? New model-data comparisons.Climate warming feedback from mountain birch forest expansion: reduced albedo dominates carbon uptake.Vegetation shift from deciduous to evergreen dwarf shrubs in response to selective herbivory offsets carbon losses: evidence from 19 years of warming and simulated herbivory in the subarctic tundra.Modelling tundra vegetation response to recent arctic warming.Large impacts of climatic warming on growth of boreal forests since 1960Deciduous trees are a large and overlooked sink for snowmelt water in the boreal forest.Influence of the physical terrestrial Arctic in the eco-climate system.Interglacials of the last 800,000 yearsGlobal biogeography of autotroph chemistry: is insolation a driving force?Observed increase in local cooling effect of deforestation at higher latitudesInclusion of local environmental conditions alters high-latitude vegetation change predictions based on bioclimatic modelsLocal temperature response to land cover and management change driven by non-radiative processesInteractions between perturbations to different Earth system components simulated by a fully-coupled climate modelGreening in the circumpolar high-latitude may amplify warming in the growing seasonHow will land use affect air temperature in the surface boundary layer? Lessons learned from a comparative study on the energy balance of an oak savanna and annual grassland in California, USAPotential and Actual impacts of deforestation and afforestation on land surface temperatureThe Holocene thermal maximum and late-Holocene cooling in the tundra of NE European RussiaClimate warming as a driver of tundra shrubline advanceArctic greening can cause earlier seasonality of Arctic amplificationLandscape Heterogeneity of Shrub Expansion in Arctic AlaskaA 2000-year record of lake ontogeny and climate variability from the north-eastern European Russian ArcticAmplified Feedback Mechanism of the Forests-Aerosols-Climate System
P2860
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P2860
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
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2010 nî lūn-bûn
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2010 թուականի Յունուարին հրատարակուած գիտական յօդուած
@hyw
2010 թվականի հունվարին հրատարակված գիտական հոդված
@hy
2010年の論文
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2010年論文
@yue
2010年論文
@zh-hant
2010年論文
@zh-hk
2010年論文
@zh-mo
2010年論文
@zh-tw
2010年论文
@wuu
name
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
@ast
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
@en
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
@nl
type
label
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
@ast
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
@en
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
@nl
prefLabel
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
@ast
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
@en
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
@nl
P2093
P2860
P356
P1476
Changes in Arctic vegetation amplify high-latitude warming through the greenhouse effect.
@en
P2093
Gordon B Bonan
Inez Y Fung
Samuel Levis
P2860
P304
P356
10.1073/PNAS.0913846107
P407
P577
2010-01-07T00:00:00Z