about
Sensitivity of Holocene atmospheric CO2 and the modern carbon budget to early human land use: analyses with a process-based modelAn efficient and accurate representation of complex oceanic and biospheric models of anthropogenic carbon uptakeWhat caused Earth's temperature variations during the last 800,000 years? Data-based evidence on radiative forcing and constraints on climate sensitivitySolar influence on climate during the past millennium: results from transient simulations with the NCAR Climate System ModelHistorical and idealized climate model experiments: an intercomparison of Earth system models of intermediate complexityClimate: how unusual is today's solar activity?Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organismsRates of change in natural and anthropogenic radiative forcing over the past 20,000 yearsTemperature increase of 21st century mitigation scenariosAllowable carbon emissions lowered by multiple climate targets.Taking action against ocean acidification: a review of management and policy options.Constraints on radiative forcing and future climate change from observations and climate model ensembles.Spatial variability and temporal trends in water-use efficiency of European forests.Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciation.OCEANOGRAPHY. Contrasting futures for ocean and society from different anthropogenic CO₂ emissions scenarios.Past and future evolution of Abies alba forests in Europe - comparison of a dynamic vegetation model with palaeo data and observations.Holocene peatland and ice-core data constraints on the timing and magnitude of CO2 emissions from past land use.Ensemble reconstruction constraints on the global carbon cycle sensitivity to climate.Carbon isotope constraints on the deglacial CO₂ rise from ice cores.Global warming: Growing feedback from ocean carbon to climate.Stable isotope constraints on Holocene carbon cycle changes from an Antarctic ice core.Projected pH reductions by 2100 might put deep North Atlantic biodiversity at riskClimate and human influences on global biomass burning over the past two millenniaLong-Term Climate Commitments Projected with Climate–Carbon Cycle ModelsEvidence for distinct modes of solar activityClimate–Carbon Cycle Feedback Analysis: Results from the C4MIP Model IntercomparisonOceanic sources, sinks, and transport of atmospheric CO2Intensification of tropical Pacific biological productivity due to volcanic eruptionsMethane emissions from floodplains in the Amazon Basin: challenges in developing a process-based model for global applicationsAn efficient and accurate representation of complex oceanic and biospheric models of anthropogenic carbon uptakeAnthropogenic perturbation of the carbon fluxes from land to oceanCarbon dioxide and climate impulse response functions for the computation of greenhouse gas metrics: a multi-model analysisComparative carbon cycle dynamics of the present and last interglacialMultiple greenhouse-gas feedbacks from the land biosphere under future climate change scenariosSimulated changes in vegetation distribution, land carbon storage, and atmospheric CO2 in response to a collapse of the North Atlantic thermohaline circulationProbabilistic climate change projections using neural networksCarbon balance of the terrestrial biosphere in the Twentieth Century: Analyses of CO2, climate and land use effects with four process-based ecosystem modelsGrowth enhancement due to global atmospheric change as predicted by terrestrial ecosystem models: consistent with US forest inventory dataA first-order analysis of the potential role of CO2 fertilization to affect the global carbon budget: a comparison of four terrestrial biosphere modelsThe substitution of high-resolution terrestrial biosphere models and carbon sequestration in response to changing CO2and climate
P50
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P50
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hulumtues
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հետազոտող
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Fortunat Joos
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P106
P1153
7004423053
P21
P31
P496
0000-0002-9483-6030
P569
2000-01-01T00:00:00Z