Prolonged effect of the stratospheric pathway in linking Barents–Kara Sea sea ice variability to the midlatitude circulation in a simplified model

Keyphrases

• Simplified Model 100%
• Prolonged Effect 100%
• Midlatitude Circulation 100%
• Sea Ice Variability 100%
• Stratospheric Pathway 100%
• Surface Heating 66%
• Downward Migration 66%
• Advection 33%
• Mid-latitude 33%
• Troposphere 33%
• Planetary Waves 33%
• Eliassen-Palm Flux 33%
• Deceleration 33%
• Cold Air 33%
• Early Winter 33%
• Lead-lag Relationship 33%
• Low-level Jet 33%
• Late Winter 33%
• Idealized Models 33%
• Dynamical Mechanism 33%
• Constructive Interference 33%
• Central Asia 33%
• Stratospheric Polar Vortex 33%
• Stratospheric Response 33%
• Atmospheric General Circulation Model 33%

Earth and Planetary Sciences

• Temperate Region 100%
• Near-Surface Geology 50%
• Stratosphere 25%
• Troposphere 25%
• Advection 25%
• Cold Air 25%
• Atmospheric General Circulation Models 25%
• Polar Vortex 25%
• Central Asia 25%