Lectures in Earth's Atmosphere
Lecture 1: Atmospheric Content
Lecture 2: Earth'S Temperature Without Gh Gases
Lecture 3: What Happens To Sunlight When It Reaches Earth?
Lecture 4: What Is The Greenhouse Effect?
Lecture 5: What Is The Atmospheric Energy Balance?
Lecture 6: Atmospheric Temperature Gradient
Lecture 7: How A Gas Molecule Absorbs Energy
Lecture 8: What Is The Mean Free Path?
Lecture 9: How A Gas Molecule Absorbs Radiation
Lecture 10: 3 Types Of Energy Of A Gas Molecule
Lecture 11: Quantum Jump In Vibrational And Rotational Energy
Lecture 12: What Are The 3 Main Vibrational Modes?
Lecture 13: What Are Combination Transition States Of H2O & Co2?
Lecture 14: What Causes The Wide Absorption Spectrum?
Lecture 15: The Molecular Absorption Spectrum Graphed
Lecture 16: The Key To Our Survival: Spectrum Broadening
Lecture 17: How Does Co2 Keep Us Warm?
Lecture 18: How Does H2O Keep Us Warm?
Lecture 19: How H2O Absorption Spectrum Compares To Co2
Lecture 20: Comparing All Major Geenhouse Gases
Lecture 21: What Is The Overlap Effect?
Lecture 22: How Is The Upper Atmosphere Heated?
Lecture 23: How Is The Lower Atmosphere Heated? (Part 1)
Lecture 24: How Is The Lower Atmosphere Heated? (Part 2)
Lecture 25: What Is The Greenhouse Effect?
Lecture 26: Stefan Botzmann Law: Earth'S Thermostat
Lecture 27: Radiation Peak Shift: Blackbody Radiation Curve
Lecture 28: What Is The Heat Capacity Of Earth'S Atmosphere?
Lecture 29: The Daily Warming Cycle: Part 1
Lecture 30: The Daily Warming Cycle: Part 2
Lecture 31: The Daily Warming Cycle: Part 3
Lecture 32: What Is The Lapse Rate?
Lecture 33: What Is The Diurnal Temperature Range?
Lecture 34: The Diurnal Temperature Range & Water Vapor
Lecture 35: The Diurnal Temperature Range: Example
Lecture 36: The Jet Stream
Lecture 37: The Jet Stream Effect
Lecture 38: The Movement Of Large Air Masses
Lecture 39: How Does Increasing Ch4 Change G.H. Effect?
Lecture 40: How Does Increasing N2O Change G.H. Effect?
Lecture 41: How Does Increase Co2 Change G.H. Effect?
Lecture 42: What Is The Decrease In Molecular Distance?
Lecture 43: The Atmospheric Effectiveness Of Co2? Part 1
Lecture 44: The Atmospheric Effectiveness Of Co2? Part 2
Lecture 45: What Does The Co2 Absorption Spectrum Imply?
Lecture 46: What Is The Transmission Spectrum Of Co2 (1M)?
Lecture 47: The Transmission Spectrum Of Co2 (10M)
Lecture 48: The Transmission Spectrum Of Co2 (100M)
Lecture 49: The Transmission Spectrum Of Co2 (1Km)
Lecture 50: The Transmission Spectrum Of Co2 (10Km)
Lecture 51: The Co2 And H2O Overlap Spectrum
Lecture 52: What Is The G.H. Effect Contribution Of Co2?(100M)
Lecture 53: What Is The Doubling Effect With Different Models?
Lecture 54: Complications With Calculating The G.H. Effect
Lecture 55: What Is The Temperature Model Sensitivity?
Lecture 56: The 1St 20 Ppm Produces 50% Of Greenhouse Effect
Lecture 57: Is Atmospheric Water Vapor Increasing?
Lecture 58: What Is The Relative Humidity Trend?
Lecture 59: What Is Tpw? (Total Precipitable Water)
Lecture 60: What Is Earth'S Temperature History?
Lecture 61: The Greenhouse Effect: What Can We Conclude?