The Causes and Implications of Persistent Atmospheric Carbon Dioxide Biases in Earth System Models
Forrest M. Hoffman, James T. Randerson
Abstract
Open-access reader
Forrest M. Hoffman, James T. Randerson
Abstract
Open-access reader
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.
Key concepts: Carbon dioxide in Earth's atmosphere, Earth (classical element), Carbon dioxide, Astrobiology, Environmental science, Earth system science, Climatology, Atmospheric sciences