about
Abrupt Glacial Climate Changes due to Stochastic ResonancePossible solar origin of the 1,470-year glacial climate cycle demonstrated in a coupled model.MIS-11 duration key to disappearance of the Greenland ice sheet.Glacial integrative modellingA movable trigger: Fossil fuel CO2and the onset of the next glaciationThermohaline circulation hysteresis: A model intercomparisonSimulation of an abrupt change in Saharan vegetation in the Mid-HoloceneLowering of glacial atmospheric CO2in response to changes in oceanic circulation and marine biogeochemistryHow cold was the Last Glacial Maximum?Comment on “Aerosol radiative forcing and climate sensitivity deduced from the Last Glacial Maximum to Holocene transition” by Petr Chylek and Ulrike LohmannMultistability and critical thresholds of the Greenland ice sheetThe importance of ocean temperature to global biogeochemistryClimate Change in Northern Africa: The Past is Not the FutureSimulation of modern and glacial climates with a coupled global model of intermediate complexityA global analysis of erosion of sandy beaches and sea-level rise: An application of DIVAPotential climatic transitions with profound impact on EuropeErratum to: The earth system model of intermediate complexity CLIMBER-3α. Part I: description and performance for present-day conditionsThe earth system model of intermediate complexity CLIMBER-3α. Part I: description and performance for present-day conditionsThe earth system model of intermediate complexity CLIMBER-3α. Part I: description and performance for present-day conditionsClimatic response to anthropogenic sulphate aerosols versus well-mixed greenhouse gases from 1850 to 2000 AD in CLIMBER-2SEMIC: an efficient surface energy and mass balance model applied to the Greenland ice sheetComparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approachImpacts of future land cover changes on atmospheric CO2and climateMillennial-scale shifts in the methane hydrate stability zone due to Quaternary climate changeModeling Obliquity and CO2Effects on Southern Hemisphere Climate during the Past 408 ka*The Effect of Obliquity-Driven Changes on Paleoclimate Sensitivity During the Late PleistoceneVegetation and climate history in the Laptev Sea region (Arctic Siberia) during Late Quaternary inferred from pollen recordsWave-induced upper-ocean mixing in a climate model of intermediate complexityTime-scale and state dependence of the carbon-cycle feedback to climateStability Analysis of the Climate-Vegetation System in the Northern High LatitudesSimulation of the future sea level contribution of Greenland with a new glacial system modelSimulation of the future sea level contribution of Greenland with a new glacial system modelVegetation dynamics amplifies precessional forcingDid Humankind Prevent a Holocene Glaciation?Transient simulation of the last glacial inception. Part II: sensitivity and feedback analysisCarbon cycle, vegetation, and climate dynamics in the Holocene: Experiments with the CLIMBER-2 modelOcean biology could control atmospheric δ13C during glacial-interglacial cycleBiogeophysical versus biogeochemical feedbacks of large-scale land cover changeModelling climate response to historical land cover change. GCTE/LUCC RESEARCH LETTEROn the stability of the atmosphere-vegetation system in the Sahara/Sahel region
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P50
name
Andrey Ganopolski
@ast
Andrey Ganopolski
@en
Andrey Ganopolski
@es
Andrey Ganopolski
@nl
type
label
Andrey Ganopolski
@ast
Andrey Ganopolski
@en
Andrey Ganopolski
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Andrey Ganopolski
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prefLabel
Andrey Ganopolski
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Andrey Ganopolski
@en
Andrey Ganopolski
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Andrey Ganopolski
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P31
P5463
Ganopolski_Andrey