GCM simulations of Titan's middle and lower atmosphere and comparison to observations

Earth and Planetary Sciences

• General Circulation Model 100%
• Tropics 100%
• Lower Atmosphere 100%
• Boundary Layer 50%
• Superrotation 50%
• Radiative Transfer 50%
• Atmospheric Model 50%
• Angular Momentum 50%
• Mesosphere 50%
• Temperature Anomaly 50%
• Turbulent Diffusion 50%
• Liquid Surface 50%
• Stratopause 50%

Keyphrases

• Dynamical Core 66%
• Large-scale Condensation 33%
• Core Ability 33%
• Flexible Modeling 33%