about
Making sense of palaeoclimate sensitivityWhat caused Earth's temperature variations during the last 800,000 years? Data-based evidence on radiative forcing and constraints on climate sensitivityGeoengineering potential of artificially enhanced silicate weathering of olivineSynchronous change of atmospheric CO2 and Antarctic temperature during the last deglacial warming.Carbon isotope constraints on the deglacial CO₂ rise from ice cores.Radiocarbon constraints on the extent and evolution of the South Pacific glacial carbon poolSea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing.Multicriteria evaluation of simulated logging scenarios in a tropical rain forest.Responses of ocean circulation and carbon cycle to changes in the position of the Southern Hemisphere westerlies at Last Glacial Maximum.Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletionPermafrost thawing as a possible source of abrupt carbon release at the onset of the Bølling/Allerød.Comparing Climate Sensitivity, Past and Present.Deglacial mobilization of pre-aged terrestrial carbon from degrading permafrostSimulated changes in vegetation distribution, land carbon storage, and atmospheric CO2 in response to a collapse of the North Atlantic thermohaline circulationLessons learned from applying a forest gap model to understand ecosystem and carbon dynamics of complex tropical forestsOn the state dependency of the equilibrium climate sensitivity during the last 5 million yearsA 156 kyr smoothed history of the atmospheric greenhouse gases CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O and their radiative forcingComment on “ Scrutinizing the carbon cycle and CO 2 residence time in the atmosphere ” by H. HardeMarine radiocarbon reservoir age simulations for the past 50,000 yearsComment on "Changes in atmospheric CO 2 levels recorded by the isotopic signature of n -alkanes from plants" from K.S. Machado and S. FroehnerComment on “Synchronous records of pCO2 and Δ14C suggest rapid, ocean-derived pCO2 fluctuations at the onset of Younger Dryas” by Steinthorsdottir et alA reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the last glacial inceptionAtmosphericδ13CO2and its relation topCO2and deep oceanδ13C during the late PleistoceneThe role of Southern Ocean processes in orbital and millennial CO2 variations – A synthesisIron fertilisation and century-scale effects of open ocean dissolution of olivine in a simulated CO2removal experimentGeoengineering impact of open ocean dissolution of olivine on atmospheric CO2, surface ocean pH and marine biologyModeled Influence of Land Ice and CO2 on Polar Amplification and Paleoclimate Sensitivity During the Past 5 Million YearsThe Effect of Obliquity-Driven Changes on Paleoclimate Sensitivity During the Late PleistoceneA State-Dependent Quantification of Climate Sensitivity Based on Paleodata of the Last 2.1 Million YearsCoccolithophore variability across Marine Isotope Stage 11 in the Pacific sector of the Southern Ocean and its potential impact on the carbon cycleUsing the Suess effect on the stable carbon isotope to distinguish the future from the past in radiocarbonOn the state dependency of fast feedback processes in (paleo) climate sensitivityEnhanced chemical weathering as a geoengineering strategy to reduce atmospheric carbon dioxide, supply nutrients, and mitigate ocean acidificationA comparison of five classifications of species into functional groups in tropical forests of French GuianaAbrupt rise in atmospheric CO 2 at the onset of the Bølling/Allerød: in-situ ice core data versus true atmospheric signalsReconstruction of a continuous high-resolution CO<sub>2</sub> record over the past 20 million yearsConstraint of the CO2rise by new atmospheric carbon isotopic measurements during the last deglaciationMechanisms for the Onset of the African Humid Period and Sahara Greening 14.5–11 ka BP*Towards ground-truthing of spaceborne estimates of above-ground life biomass and leaf area index in tropical rain forestsComment on “Magnetic effect on CO2solubility in seawater: A possible link between geomagnetic field variations and climate” by Alexander Pazur and Michael Winklhofer
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P50
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onderzoeker
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researcher
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հետազոտող
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Peter Köhler
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Peter Köhler
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Peter Köhler
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Peter Köhler
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Peter Köhler
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Peter Köhler
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Peter Köhler
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Peter Köhler
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prefLabel
Peter Köhler
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Peter Köhler
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Peter Köhler
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Peter Köhler
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P106
P1153
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P31
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0000-0003-0904-8484