about
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 cycle. The dominant role of semi-arid ecosystems in the trend and variability of the land CO₂ sink.Terrestrial nitrogen cycling in Earth system models revisited.Precipitation and carbon-water coupling jointly control the interannual variability of global land gross primary productionResponse to Comment on "Mycorrhizal association as a primary control of the CO2 fertilization effect".Ecosystem responses to elevated CO2 governed by plant-soil interactions and the cost of nitrogen acquisition.Quantifying soil moisture impacts on light use efficiency across biomes.Greening of the Earth and its driversGlobal Carbon Budget 2016Simple process-led algorithms for simulating habitats (SPLASH v.1.0): robust indices of radiation, evapotranspiration and plant-available moistureLand-use and land-cover change carbon emissions between 1901 and 2012 constrained by biomass observationsGlobal Carbon Budget 2017Regional carbon fluxes from land use and land cover change in Asia, 1980–2009Reconciling Precipitation with Runoff: Observed Hydrological Change in the MidlatitudesMultiple greenhouse-gas feedbacks from the land biosphere under future climate change scenariosImpacts of Global Change on Mediterranean Forests and Their ServicesThe Ecosystem Impacts of Severe WarmingPast and future carbon fluxes from land use change, shifting cultivation and wood harvestUsing research networks to create the comprehensive datasets needed to assess nutrient availability as a key determinant of terrestrial carbon cyclingN<sub>2</sub>O changes from the Last Glacial Maximum to the preindustrial – Part I: Quantitative reconstruction of terrestrial and marine emissions using N<sub>2</sub>O stable isotopes in ice coresN<sub>2</sub>O changes from the Last Glacial Maximum to the preindustrial – Part II: Terrestrial N<sub>2</sub>O emissions constrain carbon-nitrogen interactionsSpatial variance of spring phenology in temperate deciduous forests is constrained by background climatic conditionsDisentangling the role of photosynthesis and stomatal conductance on rising forest water-use efficiencyOrganizing principles for vegetation dynamics
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description
hulumtues
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name
Benjamin D Stocker
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Benjamin D Stocker
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Benjamin D Stocker
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Benjamin D Stocker
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Benjamin D Stocker
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Benjamin D Stocker
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Benjamin D Stocker
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