about
What caused Earth's temperature variations during the last 800,000 years? Data-based evidence on radiative forcing and constraints on climate sensitivityEvidence for ice-free summers in the late Miocene central Arctic Ocean.Tropical Atlantic temperature seasonality at the end of the last interglacialResponse of Atlantic overturning to future warming in a coupled atmosphere-ocean-ice sheet modelEvidence for Two Distinct Modes of Large-Scale Ocean Circulation Changes over the Last CenturyMillennial-scale variability in Antarctic ice-sheet discharge during the last deglaciationSea surface temperature of the mid-Piacenzian ocean: a data-model comparison.Southern Ocean origin for the resumption of Atlantic thermohaline circulation during deglaciation.Abrupt glacial climate shifts controlled by ice sheet changes.Evidence for obliquity forcing of glacial Termination II.Global climate models: past, present, and future.The Holocene temperature conundrum.The seasonal sea-ice zone in the glacial Southern Ocean as a carbon sinkLinkages between atmospheric blocking, sea ice export through Fram Strait and the Atlantic Meridional Overturning CirculationEquatorial Pacific forcing of western Amazonian precipitation during Heinrich Stadial 1.Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial.Sea level fall during glaciation stabilized atmospheric CO2 by enhanced volcanic degassing.Persistent drying in the tropics linked to natural forcing.Synchronicity of Antarctic temperatures and local solar insolation on orbital timescales.Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge.Corrigendum: The seasonal sea-ice zone in the glacial Southern Ocean as a carbon sink.Deriving dynamical models from paleoclimatic records: application to glacial millennial-scale climate variability.Increased seasonality in Middle East temperatures during the last interglacial period.Thermohaline circulation hysteresis: A model intercomparisonChallenges in quantifying Pliocene terrestrial warming revealed by data–model discordEvaluating the dominant components of warming in Pliocene climate simulationsUsing results from the PlioMIP ensemble to investigate the Greenland Ice Sheet during the mid-Pliocene Warm PeriodMid-pliocene Atlantic Meridional Overturning Circulation not unlike modernLarge-scale features of Pliocene climate: results from the Pliocene Model Intercomparison ProjectMid-Pliocene East Asian monsoon climate simulated in the PlioMIPSimulating the Antarctic ice sheet in the late-Pliocene warm period: PLISMIP-ANT, an ice-sheet model intercomparison projectAbrupt North Atlantic circulation changes in response to gradual CO2 forcing in a glacial climate stateClimatic impacts of fresh water hosing under Last Glacial Maximum conditions: a multi-model studyThe PMIP4 contribution to CMIP6 – Part 2: Two interglacials, scientific objective and experimental design for Holocene and Last Interglacial simulationsThe PMIP4 contribution to CMIP6 – Part 4: Scientific objectives and experimental design of the PMIP4-CMIP6 Last Glacial Maximum experiments and PMIP4 sensitivity experimentsClimate signature of solar irradiance variations: analysis of long-term instrumental, historical, and proxy data40. Chronology and climate forcing of the last four interglacialsA tropical mechanism for Northern Hemisphere deglaciationA multi-model assessment of last interglacial temperaturesImpact of Weddell Sea shelf progradation on Antarctic bottom water formation during the Miocene
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P50
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Gerrit Lohmann
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Gerrit Lohmann
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Gerrit Lohmann
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Gerrit Lohmann
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Gerrit Lohmann
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Gerrit Lohmann
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Gerrit Lohmann
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