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Spatial continuous modeling of early Cenozoic carbon cycle and climate. [PDF]
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Mechanical Engineering, 2023
Abstract Recently, ASME’s Video Production team visited three facilities in New York City that are capturing carbon dioxide emissions before they enter the atmosphere and using them in industrial processes can have the same net effect as averting emissions in the first place.
Walter Reineke, Michael Schlömann
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Abstract Recently, ASME’s Video Production team visited three facilities in New York City that are capturing carbon dioxide emissions before they enter the atmosphere and using them in industrial processes can have the same net effect as averting emissions in the first place.
Walter Reineke, Michael Schlömann
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Science, 2013
Enhanced levels of anaerobic respiration processes may explain oscillations in Earth's carbon cycle. [Also see Research Article by Schrag et al. ]
Canfield, D.E., Kump, L.R.
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Enhanced levels of anaerobic respiration processes may explain oscillations in Earth's carbon cycle. [Also see Research Article by Schrag et al. ]
Canfield, D.E., Kump, L.R.
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Scientific American, 1970
The amount of carbon dioxide in the atmosphere is of fundamental importance for the radiative balance of the Earth relative to space. Changes of the atmospheric CO2 concentration, as now caused by the rapidly increasing use of fossil fuels, need therefore be considered carefully when concerned with possible future changes of the climate of the Earth ...
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The amount of carbon dioxide in the atmosphere is of fundamental importance for the radiative balance of the Earth relative to space. Changes of the atmospheric CO2 concentration, as now caused by the rapidly increasing use of fossil fuels, need therefore be considered carefully when concerned with possible future changes of the climate of the Earth ...
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Black Carbon and the Carbon Cycle
Science, 1998When vegetation and fossil fuels burn, the combustion creates "black carbon" that becomes distributed throughout the environment. Determining how it is created and where it goes is important for studying the past history of fire and for understanding global carbon and oxygen budgets.
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Climate extremes and the carbon cycle
Nature, 2013The terrestrial biosphere is a key component of the global carbon cycle and its carbon balance is strongly influenced by climate. Continuing environmental changes are thought to increase global terrestrial carbon uptake. But evidence is mounting that climate extremes such as droughts or storms can lead to a decrease in regional ecosystem carbon stocks ...
Reichstein, Markus +17 more
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1957
Primarily as the result of living processes the carbon which is contained in the oceans, in the atmosphere and in living matter is cycled at a rate which is extremely rapid, particularly when viewed in the perspective of the geologic time scale.
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Primarily as the result of living processes the carbon which is contained in the oceans, in the atmosphere and in living matter is cycled at a rate which is extremely rapid, particularly when viewed in the perspective of the geologic time scale.
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Global Carbon Cycle and Carbon Sequestration
1995The concentration of greenhouse gases in the atmosphere will probably double at a timescale of a few human generations. This increase may induce climatic changes that will exceed the adaptive capacity of nature, and indeed of the human society. The intensification of the otherwise beneficial natural greenhouse effect has become a cause of concern ...
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2000
Preface Acknowledgements Part I. Introduction: 1. Introduction 2. Excerpts from 1994 and 1995 IPCC Reports Part II. The Missing Carbon Sink: 3. Carbon dioxide emissions from fossil fuel consumption and cement manufacture, 1751-1991 and an estimate of their isotopic composition and latitudinal distribution 5.
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Preface Acknowledgements Part I. Introduction: 1. Introduction 2. Excerpts from 1994 and 1995 IPCC Reports Part II. The Missing Carbon Sink: 3. Carbon dioxide emissions from fossil fuel consumption and cement manufacture, 1751-1991 and an estimate of their isotopic composition and latitudinal distribution 5.
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