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Robust Polar Amplification in Ice-Free Climates Relies on Ocean Heat Transport and Cloud Radiative Effects
Publisher: American Meteorological Society
CORRIGENDUM
Publisher: American Meteorological Society
The Nonlinear and Nonlocal Nature of Climate Feedbacks
Publisher: American Meteorological Society
Abstract: he climate feedback framework partitions the radiative response to climate forcing into contributions from individual atmospheric processes. The goal of this study is to understand the closure of the energy budget in as ...
Climate Variability and the Shape of Daily Precipitation: A Case Study of ENSO and the American West
Publisher: American Meteorological Society
Abstract: haracterizing the relationship between large-scale atmospheric circulation patterns and the shape of the daily precipitation distribution is fundamental to understanding how dynamical changes are manifest in the hydrological ...
Causes of the Arctic’s Lower-Tropospheric Warming Structure
Publisher: American Meteorological Society
Sea Ice Loss, Water Vapor Increases, and Their Interactions with Atmospheric Energy Transport in Driving Seasonal Polar Amplification
Publisher: American Meteorological Society
Coupled High-Latitude Climate Feedbacks and Their Impact on Atmospheric Heat Transport
Publisher: American Meteorological Society
Abstract: AbstractThe response of atmospheric heat transport to anthropogenic warming is determined by the anomalous meridional energy gradient. Feedback analysis offers a characterization of that gradient and hence reveals how ...
Atmospheric Eddies Mediate Lapse Rate Feedback and Arctic Amplification
Publisher: American Meteorological Society
Abstract: AbstractProjections of amplified climate change in the Arctic are attributed to positive feedbacks associated with the retreat of sea ice and changes in the lapse rate of the polar atmosphere. Here, a set of idealized ...
Sensitivity of Polar Amplification to Varying Insolation Conditions
Publisher: American Meteorological Society
Abstract: AbstractThe mechanism of polar amplification in the absence of surface albedo feedback is investigated using an atmospheric model coupled to an aquaplanet slab ocean forced by a CO2 doubling. In particular, we examine the ...