The traditional forcing-feedback framework has provided an indispensable basis for discussing global climate changes. However, as analysis of model behavior has become more detailed, shortcomings and ambiguities in the framework have become more evident, and physical effects unaccounted for by the traditional framework have become interesting. In particular, the new concept of adjustments, which are responses to forcings that are not mediated by the global-mean temperature, has emerged. This concept, related to the older ones of climate efficacy and stratospheric adjustment, is a more physical way of capturing unique responses to specific forcings. We present a pedagogical review of the adjustment concept, why it is important, and how it ca...
This is the publisher’s final pdf. The published article is copyrighted by the American Meteorologic...
[1] We quantify forcing and feedbacks across available CMIP5 coupled atmosphere-ocean general circul...
Volcanic aerosol forcing has previously been found to cause a weak global mean temperature response,...
The traditional forcing–feedback framework has provided an indispensable basis for discussing global...
Performing equilibrium climate change simulations is a standard method to study the forcing-response...
The climate sensitivity parameter has long been assumed to be constant. However, recent studies foun...
There is ample evidence that various radiative forcing mechanisms differ with respect to their effec...
Processes in the climate system that can either amplify or dampen the climate response to an externa...
The total climate impact of any transport sector consists of several individual contributions from, ...
The regional climate response to radiative forcing is largely controlled by changes in the atmospher...
The regional climate response to radiative forcing is largely controlled by changes in the atmospher...
Feedback terminology In this section we derive the parameters we use in discussing feedbacks. We emp...
Understanding the role of clouds in climate change remains a considerable challenge. Traditionally, ...
Global temperature has increased significantly during the past century. Understanding the causes of ...
This is the publisher’s final pdf. The published article is copyrighted by the American Meteorologic...
[1] We quantify forcing and feedbacks across available CMIP5 coupled atmosphere-ocean general circul...
Volcanic aerosol forcing has previously been found to cause a weak global mean temperature response,...
The traditional forcing–feedback framework has provided an indispensable basis for discussing global...
Performing equilibrium climate change simulations is a standard method to study the forcing-response...
The climate sensitivity parameter has long been assumed to be constant. However, recent studies foun...
There is ample evidence that various radiative forcing mechanisms differ with respect to their effec...
Processes in the climate system that can either amplify or dampen the climate response to an externa...
The total climate impact of any transport sector consists of several individual contributions from, ...
The regional climate response to radiative forcing is largely controlled by changes in the atmospher...
The regional climate response to radiative forcing is largely controlled by changes in the atmospher...
Feedback terminology In this section we derive the parameters we use in discussing feedbacks. We emp...
Understanding the role of clouds in climate change remains a considerable challenge. Traditionally, ...
Global temperature has increased significantly during the past century. Understanding the causes of ...
This is the publisher’s final pdf. The published article is copyrighted by the American Meteorologic...
[1] We quantify forcing and feedbacks across available CMIP5 coupled atmosphere-ocean general circul...
Volcanic aerosol forcing has previously been found to cause a weak global mean temperature response,...