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The Quantum Mechanics of Global War
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cooler sun continental drift orogen
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Outline • Quantum Mechanics #1: b
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Outline • Quantum Mechanics #1: b
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Outline • Quantum Mechanics #1: b
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Crisis in 19th Century Classical Ph
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Crisis in 19th Century Classical Ph
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Crisis in 19th Century Classical Ph
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Crisis in 19th Century Classical Ph
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Crisis in 19th Century Classical Ph
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The Solution: Quanta Light is compo
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The Solution: Quanta Light is compo
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Temperature of the Earth Rsun The e
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Temperature of the Earth Rsun The e
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Energy Balance Luminosity = Area ×
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Energy Balance Luminosity = Area ×
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Energy Balance Luminosity = Area ×
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Energy Balance Luminosity = Area ×
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Planet Earth Mars Venus calculated
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Planet Earth Mars Venus calculated
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Why We Aren’t Freezing from Clima
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H2O hν - + + hν hν = Ef - Ei CO2
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Principal greenhouse gas: water vap
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Principal greenhouse gas: water vap
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Ω = 1372 W/m 2 John Harte, Conside
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John Harte, Consider a Spherical Co
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Tropopause Z e Z e + !Z e Held & So
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Quantum Zero-Point Motion (Harold U
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Quantum Zero-Point Motion Classical
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Quantum Zero-Point Motion Classical
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Eccentricity: 100 and 413 kyr N S
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α Draconis (2000 BC) Polaris (now)
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Spectral Analysis of Isotope Record
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What amplifies orbital forcing to p
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Martian Climate May Also Show Orbit
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LIDE 7 Ice Age Climate Forcings (W/
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Single Layer Models
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Single Layer Models Vorticity Dω D
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Single Layer Models Vorticity Dω D
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Coriolis Force
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Coriolis Force ∂q ∂t + J(ψ, q)
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Coriolis Force
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- Page 105 and 106: PV = nRT Thermodynamics vs. Statist
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- Page 116 and 117: A. Sanchez-Lavega et al. Nature 451
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- Page 126 and 127: Ecosystems & Feedbacks C. D. Keelin
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