Earth’s Orbit and Its Variations
How Does the Tilt Affect Climate?
How Does Orbit’s Shape Affect Climate
Seasons and the Elliptical Orbit
Tilt Change (Obliquity Variation)
Eccentricity of The Elliptical Orbit
Eccentricity and Seasonal Insolation
Precession and Seasonal Insolation
Impacts of Precession and Eccentricity on Insolation
Insolation Control of Ice Sheets
Temperature and Ice Mass Balance
Seasons and the Size of Ice Sheet
Insolation Control of Ice Sheet Size
Three Factors that Control Ice Sheets
Insolation Control of Ice Sheet Size
Ice Sheet Lags Behind Summer Insolation Forcing
Delayed Bedrock Response Beneath Ice Sheets
Full Cycle of Ice Growth and Decay
Factors in Long-Term Evolution of Ice Sheets
Conceptual Phases of Ice Sheet Evolution
Evidence of Ice Sheet Evolution
Ice Sheet Changes Over the Last 150,000 Years
Orbital-Scale Changes in CO2 and CH4
Orbital-Scale Changes in CO2 and CH4
Orbital-Scale Changes in Methane
Insolation Control of Monsoons
The Orbital Monsoon Hypothesis
How Did Monsoon Affect Methane?
Possibility 1: Physical Oceanographic Explanation of CO2 Changes
Possibility 2: Deep Ocean Reservoir
Ocean Carbon Pumping Hypothesis
How Glaciations Increased Productions at Low Latitudes?
How Glaciations Increased Productions Near Antarctica?
Changes in North Atlantic Deep Water
Changes in Circulation of Deep Water During Glaciations
Carbon System Controls on CO2 in the Glacial Atmosphere
The Mystery of the 100,000-Year Cycle
Why Have Ice Sheets Grown Larger Since 0.9 Myr Ago?
Why Have Ice Sheets Grown Larger Since 0.9 Myr Ago?