The State Dependency of Climate Sensitivity and Cloud Responses to CO2 Doubling

dc.contributor.authorSmith, Brandon
dc.contributor.supervisorGoldblatt, Colin
dc.date.accessioned2023-01-31T19:04:17Z
dc.date.available2023-01-31T19:04:17Z
dc.date.copyright2023en_US
dc.date.issued2023-01-31
dc.degree.departmentSchool of Earth and Ocean Sciences
dc.degree.levelMaster of Science M.Sc.en_US
dc.description.abstractCloud feedbacks are a large source of uncertainty in paleoclimate studies and in the constraint of climate sensitivity, and it is thought that climate sensitivity depends on climate state because of these feedbacks. Here we evaluate the state dependence of both climate sensitivity and cloud responses to CO2 doubling for a palate of climates with varying solar luminosity and CO2 concentrations, yet near-equivalent global mean surface temperatures. We find that cloud responses to CO2 doubling and climate sensitivity are largely dependent on the magnitude of radiative forcing from doubling CO2 alone, and are therefore independent of climate state. We also determine that the most important responses in clouds occur in the mid-latitude storm tracks, owing to inhibited baroclinic activity as a consequence of a more equable climate under higher CO2 concentrations.en_US
dc.description.scholarlevelGraduateen_US
dc.identifier.urihttp://hdl.handle.net/1828/14717
dc.languageEnglisheng
dc.language.isoenen_US
dc.rightsAvailable to the World Wide Weben_US
dc.titleThe State Dependency of Climate Sensitivity and Cloud Responses to CO2 Doublingen_US
dc.typeThesisen_US

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