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Three tables and a json file are provided containing effective climate sensitivity, effective 2xco 2 radiative forcing, and radiative feedbacks for all cmip5 and cmip6 models that have published output from abrupt co 2 quadrupling experiments. In this study, we diagnose the forcings, feedbacks, and ecs values in all available cmip6 models. This notebook uses the “gregory method” to approximate the ecs of cmip6 models based on the first 150 years after an abrupt quadrupling of co 2 concentrations.

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To view the information about all cmip6 requested variables, you can search the cmip6 mip table here In all of these models, high ecs values are at least partly attributed to larger cloud feedbacks than their predecessors Here you can search through the requested experiments for cmip6 by their experiment id, title, mip or number of total years for the experiment (ntot).

Cmip6 models have higher lcf on average

Ecs has increased significantly in the latest generation of gcms, with values exceeding 4.5 ̊c in 9/19 models This increase is due to stronger positive cloud feedbacks from decreasing extratropical low cloud coverage and albedo. Comparing wcrp assessment with cmip6 52 cmip6 models 30% (16/52) have an ecs higher than 4.5°c Tables of ecs, effective radiative forcing, and radiative feedbacks from zelinka et al., grl (2020)

A full, alphabetised list of modelling centres and esgf nodes providing cmip6 data can be found here A map showing all the esgf nodes, along with the cmip modelling centres can be found on here.