2012•MPG.PuRe (Max Planck Society)Open access

The Causes and Implications of Persistent Atmospheric Carbon Dioxide Biases in Earth System Models

Forrest M. Hoffman, James T. Randerson

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Abstract

I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system. I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system. I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system. I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system.

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I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system. I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system. I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system. I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system.

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Available abstract

I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system. I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system. I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system. I Rapidly increasing atmospheric carbon dioxide (CO2) concentrations are altering Earth’s climate. I Perturbation of the carbon cycle could induce feedbacks on future CO2 concentrations and climate. I Climate-carbon cycle feedbacks are highly uncertain and potentially large. I Prediction of feedbacks requires knowledge of mechanisms connecting carbon and nutrients with the climate system.

Key concepts: Carbon dioxide in Earth's atmosphere, Earth (classical element), Carbon dioxide, Astrobiology, Environmental science, Earth system science, Climatology, Atmospheric sciences

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