about
One mechanism contributing to co-variability of the Atlantic inflow branches to the ArcticTrajectory of the Arctic as an integrated system.Methanogen community composition and rates of methane consumption in Canadian High Arctic permafrost soils.Tropical forcing of the recent rapid Arctic warming in northeastern Canada and Greenland.The ocean's role in polar climate change: asymmetric Arctic and Antarctic responses to greenhouse gas and ozone forcing.Evidence of high-elevation amplification versus Arctic amplification.Shifting El Niño inhibits summer Arctic warming and Arctic sea-ice melting over the Canada Basin.Problems encountered when defining Arctic amplification as a ratioSpatiotemporal variability in surface energy balance across tundra, snow and ice in GreenlandDifferences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depthThermal source Fourier transform infrared microtomography applied to Arctic sea ice diatoms.Enhanced modern heat transfer to the Arctic by warm Atlantic Water.Enhanced wintertime greenhouse effect reinforcing Arctic amplification and initial sea-ice melting.Ongoing Climate Change in the Arctic.Poleward upgliding Siberian atmospheric rivers over sea ice heat up Arctic upper air.Microbial community dynamics in the forefield of glaciers.Spring warming in Yukon mountains is not amplified by the snow albedo feedback.The Effect of Arctic Dust on the Retrieval of Satellite Derived Sea and Ice Surface Temperatures.Recent Arctic amplification and extreme mid-latitude weatherTropospheric temperature trends: history of an ongoing controversyWeather conditions and variation in timing of spring and fall migrations of migratory caribouImpact of sea ice cover changes on the Northern Hemisphere atmospheric winter circulationArctic Warming Ripples through EurasiaWarm-air advection, air mass transformation and fog causes rapid ice meltA transitioning Arctic surface energy budget: the impacts of solar zenith angle, surface albedo and cloud radiative forcingEnergy-balance mechanisms underlying consistent large-scale temperature responses in warm and cold climatesArctic climate and its interaction with lower latitudes under different levels of anthropogenic warming in a global coupled climate modelOcean heat transport into the Arctic in the twentieth and twenty-first century in EC-EarthArctic climate change in 21st century CMIP5 simulations with EC-EarthIsentropic constraints by midlatitude surface warming on the Arctic midtroposphereCharacteristics of summer-time energy exchange in a high Arctic tundra heath 2000–2010Trends in CO2exchange in a high Arctic tundra heath, 2000-2010The role of mineral-dust aerosols in polar temperature amplificationThe role of snow-surface coupling, radiation, and turbulent mixing in modeling a stable boundary layer over Arctic sea iceArctic Ocean Gas Hydrate Stability in a Changing ClimateSonar gas flux estimation by bubble insonification: application to methane bubble flux from seep areas in the outer Laptev SeaThe polar amplification asymmetry: role of Antarctic surface heightDrivers of North Atlantic Polar Front jet stream variabilityAdvancing adaptation planning for climate change in the Inuvialuit Settlement Region (ISR): a review and critiqueIncreasing fall-winter energy loss from the Arctic Ocean and its role in Arctic temperature amplification
P2860
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P2860
description
2008 nî lūn-bûn
@nan
2008年の論文
@ja
2008年論文
@yue
2008年論文
@zh-hant
2008年論文
@zh-hk
2008年論文
@zh-mo
2008年論文
@zh-tw
2008年论文
@wuu
2008年论文
@zh
2008年论文
@zh-cn
name
Vertical structure of recent Arctic warming.
@en
Vertical structure of recent Arctic warming.
@nl
type
label
Vertical structure of recent Arctic warming.
@en
Vertical structure of recent Arctic warming.
@nl
prefLabel
Vertical structure of recent Arctic warming.
@en
Vertical structure of recent Arctic warming.
@nl
P2093
P356
P1433
P1476
Vertical structure of recent Arctic warming.
@en
P2093
Erland Källén
Gunilla Svensson
Rune G Graversen
P2888
P356
10.1038/NATURE06502
P407
P577
2008-01-01T00:00:00Z
P5875
P6179
1008001593