Index

Documents

• Acknowledgements
• Background of Research
• Basic Equations
• Change in Surface Pressure by Evaporation and Condensation
• Changes in the Equilibrium State (Circulation Pattern) in Equilibrium States
• Changes in the Equilibrium State (Meridional Structure) in Equilibrium States
• Changes in the Equilibrium State (Precipitation Distribution) in Equilibrium States
• Characteristics of Atmospheric Disturbance in Equilibrium States
• Characteristics of Atmospheric Disturbances in the Runaway Greenhouse State
• Characteristics of One-Dimensional Radiative-Convective Equilibrium Solutions
• Characteristics of Radiative Equilibrium Solutions: Results of Stratospheric Model
• Chronology of Studies on the Runaway Greenhouse State
• Conclusion
• Condensation Heating Distribution (Troposphere) in Equilibrium States
• Conditions for the Existence of Equilibrium Solutions
• Contents
• Dependence of the Upper Limit of Radiation on Relative Humidity
• Equilibrium State of Results from Calculations with a Single Damping Layer: Meridional Energy Transport
• Equilibrium State of Results from Calculations with a Single Damping Layer: Meridional Distribution of Energy Flux
• Equilibrium State of Results from Calculations with a Single Damping Layer: Meridional Structure of the Upper Layer
• Equilibrium State of Results from Calculations with a Single Damping Layer: Meridional Structure of the Troposphere
• Equilibrium State of Results from Calculations with a Single Damping Layer: Runaway Greenhouse State
• Examination on the Vertical Resolution
• Experimental Design and List of Experiments
• Future Themes and Problems
• Global Mean Values in Equilibrium States (table 1)
• Global Mean Values in Equilibrium States
• Implications of the Present Study
• Index
• Meridional Distribution of Energy Flux in Equilibrium States
• Meridional Distribution of Specific Humidity in the Runaway Greenhouse State (Animation)
• Meridional Distribution of Temperature in the Runaway Greenhouse State (Animation)
• Meridional Distribution of Zonal Wind in the Runaway Greenhouse State (Animation)
• Meridional Energy Transport
• Meridional Energy Transport in Experiment S1200
• Meridional Energy Transport in Experiment S1380
• Meridional Energy Transport in Experiment S1570
• Meridional Energy Transport in the Runaway Greenhouse State
• Meridional Structure in the Runaway Greenhouse State
• Meridional Thermal Structure in the Runaway Greenhouse State
• Model
• Moist Convective Adjustment Scheme
• Previous Studies on the Runaway Greenhouse State
• Problems Investigated in the Present Paper
• Radiation Scheme
• Relative Humidity Distribution (Troposphere) in Equilibrium States
• Results from Experiment S1200
• Results from Experiment S1380
• Results from Experiment S1500
• Results from Experiment S1550
• Results from Experiment S1570
• Results from Experiment S1600
• Results from Experiment S1700
• Results from Experiment S1800
• Specific Humidity Distribution (Troposphere) in Equilibrium States
• Surface Pressure Distribution in the Runaway Greenhouse State (Animation)
• Surface Temperature Distribution in the Runaway Greenhouse State (Animation)
• Temperature Distribution and Mass Stream Function (Upper Layer) in Equilibrium States
• Temperature Distribution and Mass Stream Function (Troposphere) in Equilibrium States
• The Komabayashi-Ingersoll Limit with Considering Relative Humidity
• The Tropospheric Flux Emission Conditions
• The Value of the 3D Runaway Limit
• The Runaway Greenhouse State
• Time Evolution of Global Mean Values in the Runaway Greenhouse State
• Time Evolution of Physical Variables in the Runaway Greenhouse State
• Time Evolution of the Precipitation Distribution in Experiment S1200
• Time Evolution of the Precipitation Distribution in Experiment S1380
• Time Evolution of the Precipitation Distribution in Experiment S1570
• Time Evolution of the Precipitation Distribution in Experiment S1800
• Time Evolution of the Vertically Integrated Specific Humidity Distribution in Experiment S1200
• Time Evolution of the Vertically Integrated Specific Humidity Distribution in Experiment S1380
• Time Evolution of the Vertically Integrated Specific Humidity Distribution in Experiment S1570
• Time Evolution of the Vertical Mean Water Vapor Content in Experiment S1800
• Upper Damping Layers
• Utilized System and Assumptions
• Vertical Filter
• What Determines a Runaway Limit? (Comparison with the Stratospheric Model)
• What Determines a Runaway Limit? (Description with an Equilibrium Solution of 1D Radiative-Convective Model)
• What Determines a Runaway Limit? (Examination on the Vertical Structure)
• Will the "runaway state" also be realized in 3D system?
• Zonal Wind Distribution (Troposphere) in Equilibrium States
• Zonal Wind Distribution (Upper Layer) in Equilibrium States


• Abe and Matsui (1988)
• Gold(1964)
• Ingersoll (1969)
• Kasting (1988)
• Komabayashi (1967)
• Lindzen et al. (1982)
• Nakajima et al. (1992)
• Pierrerhumbert (1995)
• Plass(1961)
• Pollack (1971)
• Rasool and deBergh (1970)
• Renno et al. (1995)
• Simpson(1927)
• Vardavas and Carver (1985)

Animation

• Meridional Distribution of Temperature in Experiment S1800
• Meridional Distribution of Specific Humidity in Experiment S1800
• Meridional distribution of zonal wind in Experiment S1800
• Precipitation Distribution in Experiment S1200
• Precipitation Distribution in Experiment S1380
• Precipitation Distribution in Experiment S1570
• Precipitation Distribution in Experiment S1800
• Surface Temperature Distribution in Experiment S1800
• Surface Pressure Distribution in Experiment S1800
• Vertically Integrated Specific Humidity Distribution in Experiment S1200
• Vertically Integrated Specific Humidity Distribution in Experiment S1380
• Vertically Integrated Specific Humidity Distribution in Experiment S1570

Index