The Quantum Mechanics of Global Warming - University of Virginia

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Physics <strong>of</strong> Feedbacks Input (I) System Output (O) gain (g) O = I + gI + ggI + ··· = I 1 − g if g
Physics <strong>of</strong> Feedbacks Input (I) System Output (O) gain (g) O = I + gI + ggI + ··· = I 1 − g if g
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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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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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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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Page 81 and 82: Coriolis Force
Page 83 and 84: Coriolis Force ∂q ∂t + J(ψ, q)
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Page 91 and 92: Stratification q = ∇ 2 ψ + f −
Page 93 and 94: Stratification Sets Synoptic Length
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Page 105 and 106: PV = nRT Thermodynamics vs. Statist
Page 109 and 110: Hopf Functional Approach
Page 111 and 112: Hopf Functional Approach dx dt = x2
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Page 116 and 117: A. Sanchez-Lavega et al. Nature 451
Page 118 and 119: 0 A. Sanchez-Lavega et al. Nature 4
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Page 132 and 133: Some Feedbacks Already Included in
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Page 142 and 143: An estimate of the contribution to
Page 145: Source: Global Warming Art
Page 148 and 149: What Can Modern Physics Contribute?
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