The Quantum Mechanics of Global Warming - University of Virginia

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Energy Balance Luminosity = Area × Intensity = 4πR 2 sun × σT 4 sun Space incoming energy flux outgoing energy flux (IR) πR 2 E 4πr 2 E (1 − a) 4πR 2 sun σT 4 sun = 4πR 2 E σT 4 E
Energy Balance Luminosity = Area × Intensity = 4πR 2 sun × σT 4 sun Space incoming energy flux outgoing energy flux (IR) πR 2 E 4πr 2 E (1 − a) 4πR 2 sun σT 4 sun = 4πR 2 E σT 4 E
Page 1 and 2: The Quantum Mechanics of Global War
Page 4 and 5: cooler sun continental drift orogen
Page 6 and 7: Outline • Quantum Mechanics #1: b
Page 12 and 13: Crisis in 19th Century Classical Ph
Page 22 and 23: The Solution: Quanta Light is compo
Page 24 and 25: The Solution: Quanta Light is compo
Page 26 and 27: Temperature of the Earth Rsun The e
Page 28 and 29: Temperature of the Earth Rsun The e
Page 30 and 31: Energy Balance Luminosity = Area ×
Page 38 and 39: Planet Earth Mars Venus calculated
Page 40 and 41: Planet Earth Mars Venus calculated
Page 43 and 44: Why We Aren’t Freezing from Clima
Page 45 and 46: H2O hν - + + hν hν = Ef - Ei CO2
Page 47 and 48: Principal greenhouse gas: water vap
Page 49 and 50: Principal greenhouse gas: water vap
Page 51 and 52: Ω = 1372 W/m 2 John Harte, Conside
Page 53 and 54: John Harte, Consider a Spherical Co
Page 55 and 56: Tropopause Z e Z e + !Z e Held & So
Page 57 and 58: Quantum Zero-Point Motion (Harold U
Page 59 and 60: Quantum Zero-Point Motion Classical
Page 61 and 62: Quantum Zero-Point Motion Classical
Page 63 and 64: Eccentricity: 100 and 413 kyr N S
Page 65 and 66: α Draconis (2000 BC) Polaris (now)
Page 67 and 68: Spectral Analysis of Isotope Record
Page 69 and 70: What amplifies orbital forcing to p
Page 71 and 72: Martian Climate May Also Show Orbit
Page 73 and 74: LIDE 7 Ice Age Climate Forcings (W/
Page 75 and 76: Single Layer Models
Page 77 and 78: Single Layer Models Vorticity Dω D
Page 79 and 80: Single Layer Models Vorticity Dω D
Page 81 and 82: Coriolis Force
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Coriolis Force ∂q ∂t + J(ψ, q)
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Coriolis Force
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Stratification
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Stratification q = ∇ 2 ψ + f −
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Stratification Sets Synoptic Length
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7. The NADW Meridional Cell and Dee
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City Latitude January ( o F) August
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Topography & Angular Momentum Richa
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PV = nRT
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PV = nRT Thermodynamics vs. Statist
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Hopf Functional Approach
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Hopf Functional Approach dx dt = x2
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Hopf Functional Approach dx dt = x2
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A. Sanchez-Lavega et al. Nature 451
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0 A. Sanchez-Lavega et al. Nature 4
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Direct Numerical Simulation of Jet
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10 -5 -10 10 8 (a) Mean Absolute Vo
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25 days
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Ecosystems & Feedbacks C. D. Keelin
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J. B. Marston, M. Oppenheimer, R. M
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Physics of Feedbacks Input (I) Syst
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Some Feedbacks Already Included in
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IPCC 2001
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An estimate of the contribution to
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Source: Global Warming Art
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What Can Modern Physics Contribute?
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“Human beings are now carrying ou
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Antarctic Dome C Siegenthaler et al
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Lake Mead
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The Quantum Mechanics of Global Warming - University of Virginia

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