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The local, remote, and global consequences of climate feedbacks
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Robust polar amplification in ice-free climates relies on ocean heat transport a...
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A CESM2 model hierarchy for assessing the causes of dramatic interannual variabi...
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Sea ice perturbations in aquaplanet simulations: Isolating the physical climate...
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Sea Ice Loss, Water Vapor Increases, and Their Interactions with Atmospheric Ene...
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Atmospheric Eddies Mediate Lapse Rate Feedback and Arctic Amplification
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Current-climate sea ice amount and seasonality as constraints for future Arctic...
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Warm Arctic–Cold Eurasia pattern driven by atmospheric blocking in models and ob...
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Atmospheric Eddies Mediate Lapse Rate Feedback and Arctic Amplification
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Coupled High-Latitude Climate Feedbacks and Their Impact on Atmospheric Heat Tra...
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Supporting Data for Feldl et al. 2017: Coupled high-latitude climate feedbacks a...
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Supporting Data for Feldl et al. 2017: Coupled high-latitude climate feedbacks a...
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Emergent Behavior of Arctic Precipitation in Response to Enhanced Arctic Warming...
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Coupled High-Latitude Climate Feedbacks and Their Impact on Atmospheric Heat Tra...
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Causal Interactions between Southern Ocean Polynyas and High-Latitude Atmosphere...
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Contributions to regional precipitation change and its polar-amplified pattern u...
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Sea ice and atmospheric circulation shape the high-latitude lapse rate feedback
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Sea ice and atmospheric circulation shape the high-latitude lapse rate feedback
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Sea ice and atmospheric circulation shape the high-latitude lapse rate feedback
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Process Drivers, Inter-Model Spread, and the Path Forward: A Review of Amplified...
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54 ENVIRONMENTAL SCIENCES
Climate change
Energy transport
Feedback
Atmospheric sciences
Climate sensitivity
ATMOSPHERIC HEAT-TRANSPORT
Atmosphere-ocean interaction
Atmospheric Science
Atmospheric Sciences
Causal Inference
Climate Action
Climate Variability
Climate change science
Climate models
Earth Sciences
Environmental Chemistry
GENERAL-CIRCULATION MODEL
GLOBAL CLIMATE MODEL
Geomatic Engineering
Global and Planetary Change
Hydrologic cycle
INCREASED CO2
INDIVIDUAL FEEDBACK PROCESSES
LAPSE-RATE
Large-scale motions
MERIDIONAL OVERTURNING CIRCULATION
MIXED-PHASE CLOUDS
Meteorology & Atmospheric Sciences
Model Projections
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