In this paper, we develop a discrete time, state variable feedback control regime to analyze the closed-loop properties associated with stabilizing the global mean surface temperature anomaly at 2 °C within a sequential decision making framework made u
The accumulation of greenhouse gases is the main reason for the global warming process. Water vapour...
The correct understanding of the transient response to external radiative perturbation is important ...
A method for estimating uncertainty in future climate change is discussed in detail and applied to p...
In this paper, we develop a discrete time, state variable feedback control regime to analyze the clo...
International audienceThe response of the various climatic processes to climate change can amplify (...
The sensitivity of global climate with respect to forcing is generally described in terms of the glo...
There is evidence that a natural control system influences global atmospheric surface temperature (L...
In the ECHAM5/MPI-OM model a collapse of the Atlantic thermohaline circulation results in a global s...
Controlling global warming through collective cooperation is a non-optional threshold public goods g...
This study examines in detail the 'atmospheric' radiative feedbacks operating in a coupled General C...
Feedback terminology In this section we derive the parameters we use in discussing feedbacks. We emp...
This paper is devoted to the temperature control and the stabilization under input constraints of ex...
Global warming in response to external radiative forcing is determined by the feedback of the climat...
If solar radiation management (SRM) were ever implemented, feedback of the observed climate state mi...
Author Posting. © American Geophysical Union, 2018. This article is posted here by permission of Am...
The accumulation of greenhouse gases is the main reason for the global warming process. Water vapour...
The correct understanding of the transient response to external radiative perturbation is important ...
A method for estimating uncertainty in future climate change is discussed in detail and applied to p...
In this paper, we develop a discrete time, state variable feedback control regime to analyze the clo...
International audienceThe response of the various climatic processes to climate change can amplify (...
The sensitivity of global climate with respect to forcing is generally described in terms of the glo...
There is evidence that a natural control system influences global atmospheric surface temperature (L...
In the ECHAM5/MPI-OM model a collapse of the Atlantic thermohaline circulation results in a global s...
Controlling global warming through collective cooperation is a non-optional threshold public goods g...
This study examines in detail the 'atmospheric' radiative feedbacks operating in a coupled General C...
Feedback terminology In this section we derive the parameters we use in discussing feedbacks. We emp...
This paper is devoted to the temperature control and the stabilization under input constraints of ex...
Global warming in response to external radiative forcing is determined by the feedback of the climat...
If solar radiation management (SRM) were ever implemented, feedback of the observed climate state mi...
Author Posting. © American Geophysical Union, 2018. This article is posted here by permission of Am...
The accumulation of greenhouse gases is the main reason for the global warming process. Water vapour...
The correct understanding of the transient response to external radiative perturbation is important ...
A method for estimating uncertainty in future climate change is discussed in detail and applied to p...
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