Transient simulations of Holocene atmospheric carbon dioxide and terrestrial carbon since the Last Glacial Maximum - Wikidata - awgldk - TriplyDB

Transient simulations of Holocene atmospheric carbon dioxide and terrestrial carbon since the Last Glacial Maximum

Transient simulations of Holocene atmospheric carbon dioxide and terrestrial carbon since the Last Glacial Maximum

http://www.wikidata.org/entity/Q58113996

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Elevated-CO2 Response of Stomata and Its Dependence on Environmental Factors Ecosystem dynamics based on plankton functional types for global ocean biogeochemistry models Spatial variability and temporal trends in water-use efficiency of European forests.The Anthropocene: conceptual and historical perspectives.Integrating models with data in ecology and palaeoecology: advances towards a model-data fusion approach.Greenhouse gases in the Earth system: a palaeoclimate perspective.Interglacials of the last 800,000 years Late Holocene climate: Natural or anthropogenic?Lowering of glacial atmospheric CO2in response to changes in oceanic circulation and marine biogeochemistry Holocene carbon emissions as a result of anthropogenic land cover change Dendro-archeo-ecology in North America and Europe: Re-purposing Historical Materials to Study Ancient Human-Environment Interactions Observational constraints on the causes of Holocene CO2change Changes in the hydrological cycle, ocean circulation, and carbon/nutrient cycling during the last interglacial and glacial transition A futurist perspective on the Anthropocene Atmosphericδ13CO2and its relation topCO2and deep oceanδ13C during the late Pleistocene A model-based interpretation of low-frequency changes in the carbon cycle during the last 120,000 years and its implications for the reconstruction of atmospheric Δ14C Quantitative interpretation of atmospheric carbon records over the last glacial termination Meridional reorganizations of marine and terrestrial productivity during Heinrich events Poorly ventilated deep ocean at the Last Glacial Maximum inferred from carbon isotopes: A data-model comparison study Impact of oceanic circulation changes on atmosphericδ13CO2 Toward explaining the Holocene carbon dioxide and carbon isotope records: Results from transient ocean carbon cycle-climate simulations Late Quaternary variations in tree cover at the northern forest-tundra ecotone Paleoclimate modeling in China: A review Holocene carbon cycle dynamics A lowering effect of reconstructed Holocene changes in sea surface temperatures on the atmospheric CO2concentration Holocene climate and carbon cycle dynamics: Experiments with the “green” McGill Paleoclimate Model

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Transient simulations of Holocene atmospheric carbon dioxide and terrestrial carbon since the Last Glacial Maximum

http://www.wikidata.org/entity/Q58113996

description

wetenschappelijk artikel

@nl

наукова стаття, опублікована у квітні 2004

@uk

name

Transient simulations of Holoc ...... since the Last Glacial Maximum

@en

Transient simulations of Holoc ...... since the Last Glacial Maximum

@nl

type

label

Transient simulations of Holoc ...... since the Last Glacial Maximum

@en

Transient simulations of Holoc ...... since the Last Glacial Maximum

@nl

prefLabel

Transient simulations of Holoc ...... since the Last Glacial Maximum

@en

Transient simulations of Holoc ...... since the Last Glacial Maximum

@nl

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Global Biogeochemical Cycles

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Transient simulations of Holoc ...... since the Last Glacial Maximum

@en

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I. C. Prentice

http://www.w3.org/2001/XMLSchema#string

Paul J. Valdes

http://www.w3.org/2001/XMLSchema#string

Stefan Gerber

http://www.w3.org/2001/XMLSchema#string

P2860

Increases in terrestrial carbon storage from the Last Glacial Maximum to the present

Global warming and marine carbon cycle feedbacks on future atmospheric CO2

Estimating the change of carbon in the terrestrial biosphere from 18 000 BP to present using a carbon cycle model.

13C discrimination during CO2 assimilation by the terrestrial biosphere.

Atmospheric CO2 concentrations over the last glacial termination.

Net primary production of a forest ecosystem with experimental CO2 enrichment

Dual modes of the carbon cycle since the Last Glacial Maximum.

The Anthropogenic Greenhouse Era Began Thousands of Years Ago

Ice Age terrestrial carbon changes revisited

Global response of terrestrial ecosystem structure and function to CO2and climate change: results from six dynamic global vegetation models

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scholarly article

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10.1029/2003GB002156

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2

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18

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Bette Otto-Bliesner

P577

2004-04-03T00:00:00Z

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