about
Historical and idealized climate model experiments: an intercomparison of Earth system models of intermediate complexityComment on "Strong signature of the active Sun in 100 years of terrestrial insolation data" by W. WeberA regime shift in the Sun-Climate connection with the end of the Medieval Climate Anomaly.Formation of most of our coal brought Earth close to global glaciation.Baby, it's cold outside: Climate model simulations of the effects of the asteroid impact at the end of the CretaceousExceptional twentieth-century slowdown in Atlantic Ocean overturning circulationObserved fingerprint of a weakening Atlantic Ocean overturning circulationOn the effect of a new grand minimum of solar activity on the future climate on EarthAre the most recent estimates for Maunder Minimum solar irradiance in agreement with temperature reconstructions?The faint young Sun problemEvaluation of biospheric components in Earth system models using modern and palaeo-observations: the state-of-the-artLong-Term Climate Change Commitment and Reversibility: An EMIC IntercomparisonExtremely compact massive galaxies at z 1.4Dating the stellar population in massive early-type galaxies atz∼ 1.5Looking for obscured QSOs in the X-ray emitting ERO populationThe density of very massive evolved galaxies to z = 1.7Corrigendum to “Climate simulations of Neoproterozoic snowball Earth events: Similar critical carbon dioxide levels for the Sturtian and Marinoan glaciations” [Earth Planet. Sci. Lett. 404 (2014) 200–205]Erratum: Corrigendum: Evidence for an exceptional twentieth-century slowdown in Atlantic Ocean overturningAsymmetry and uncertainties in biogeophysical climate–vegetation feedback over a range of CO<sub>2</sub> forcingsClimate simulations of Neoproterozoic snowball Earth events: Similar critical carbon dioxide levels for the Sturtian and Marinoan glaciationsQuantifying the global carbon cycle response to volcanic stratospheric aerosol radiative forcing using Earth System ModelsTime-scale and state dependence of the carbon-cycle feedback to climateA volcanically triggered regime shift in the subpolar North Atlantic Ocean as a possible origin of the Little Ice AgeAlbedo and heat transport in 3-D model simulations of the early Archean climateOn the Relation Between Solar Activity and Clear-Sky Terrestrial IrradianceErratum to: On the Relation Between Solar Activity and Clear-Sky Terrestrial IrradianceOn the effect of orbital forcing on mid-Pliocene climate, vegetation and ice sheetsUnderstanding the influence of solar irradiance changes on Earth’s climate during the HoloceneFaint young Sun problem more severe due to ice-albedo feedback and higher rotation rate of the early EarthLimits to biodiversity cycles from a unified model of mass-extinction eventsThe Smithsonian solar constant data revisited: no evidence for a strong effect of solar activity in ground-based insolation dataClimate modelling of mass-extinction events: a reviewIntegrated specific star formation rates of galaxies, groups, and clusters: a continuous upper limit with stellar mass?The impact of Spitzer infrared data on stellar mass estimates – and a revised galaxy stellar mass function at 0 < z < 5The Kormendy relation of massive elliptical galaxies at z 1.5: evidence for size evolutionThe Munich Near-Infrared Cluster Survey - IX. Galaxy evolution to z 2 from optically selected cataloguesIntegrated specific star formation rates of galaxies, groups, and clusters: a continuous upper limit with stellar mass?The evolution of the luminosity functions in the FORS deep field from low to high redshiftThe MUNICS Project: Galaxy Assembly at 0 < z < 1The TESIS Project: Are Type 2 QSO Hidden in X-Ray Emitting EROs?
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P50
description
onderzoeker
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researcher
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ricercatore
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հետազոտող
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name
Georg Feulner
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Georg Feulner
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Georg Feulner
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Georg Feulner
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Georg Feulner
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Georg Feulner
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Georg Feulner
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Georg Feulner
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Georg Feulner
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Georg Feulner
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Georg Feulner
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Georg Feulner
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P214
P1053
A-1933-2011
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P21
P214
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