Broad range of 2050 warming from an observationally constrained large climate model ensemble
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Rubisco activity and regulation as targets for crop improvementEffects of long-term individual and combined water and temperature stress on the growth of rice, wheat and maize: relationship with morphological and physiological acclimation.Winter Conditions and Land Cover Structure the Subnivium, A Seasonal Refuge beneath the Snow.Choice of baseline climate data impacts projected species' responses to climate change.Expression of cyanobacterial FBP/SBPase in soybean prevents yield depression under future climate conditions.Small heat-shock proteins protect from heat-stroke-associated neurodegeneration.Uncertainty: Climate models at their limit?A field facility to simulate climate warming and increased nutrient supply in shallow aquatic ecosystems.Predicting evolution in response to climate change: the example of sprouting probability in three dormancy-prone orchid speciesHyperthermia on skin immune system and its application in the treatment of human papillomavirus-infected skin diseases.Feedbacks, climate sensitivity and the limits of linear models.Atmospheric CH4 oxidation by Arctic permafrost and mineral cryosols as a function of water saturation and temperature.Canopy warming caused photosynthetic acclimation and reduced seed yield in maize grown at ambient and elevated [CO2 ].Greater future global warming inferred from Earth's recent energy budget.Beyond equilibrium climate sensitivityA 1200-year multiproxy record of tree growth and summer temperature at the northern pine forest limit of EuropeObtaining diverse behaviors in a climate model without the use of flux adjustmentsHistory matching for exploring and reducing climate model parameter space using observations and a large perturbed physics ensembleIdentifying and removing structural biases in climate models with history matchingPerturbed physics ensemble using the MIROC5 coupled atmosphere–ocean GCM without flux corrections: experimental design and resultsKey factors governing uncertainty in the response to sunshade geoengineering from a comparison of the GeoMIP ensemble and a perturbed parameter ensembleQuantifying uncertainty in future Southern Hemisphere circulation trends
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P2860
Broad range of 2050 warming from an observationally constrained large climate model ensemble
description
article
@en
im März 2012 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в березні 2012
@uk
name
Broad range of 2050 warming fr ...... d large climate model ensemble
@en
Broad range of 2050 warming fr ...... d large climate model ensemble
@nl
type
label
Broad range of 2050 warming fr ...... d large climate model ensemble
@en
Broad range of 2050 warming fr ...... d large climate model ensemble
@nl
prefLabel
Broad range of 2050 warming fr ...... d large climate model ensemble
@en
Broad range of 2050 warming fr ...... d large climate model ensemble
@nl
P2093
P2860
P50
P356
P1433
P1476
Broad range of 2050 warming fr ...... d large climate model ensemble
@en
P2093
Ben B. B. Booth
Benjamin M. Sanderson
Carl Christensen
Chris E. Forest
Claudio Piani
Daniel J. Rowlands
David J. Frame
Dáithí A. Stone
Eleanor J. Highwood
P2860
P2888
P304
P356
10.1038/NGEO1430
P407
P577
2012-03-25T00:00:00Z