The Quantum Mechanics of Global Warming - University of Virginia

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Principal greenhouse gas: water vapor Secondary: carbon dioxide, methane, CFC’s, … Absorption lines are pressure-broadened Robert A. Rohde for the Global Warming Art project
Principal greenhouse gas: water vapor Secondary: carbon dioxide, methane, CFC’s, … Absorption lines are pressure-broadened IR photons are on average absorbed and emitted about 2x on way out to space Robert A. Rohde for the Global Warming Art project
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: 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
Page 83 and 84: Coriolis Force ∂q ∂t + J(ψ, q)
Page 87 and 88: Coriolis Force
Page 89 and 90: Stratification
Page 91 and 92: Stratification q = ∇ 2 ψ + f −
Page 93 and 94: Stratification Sets Synoptic Length
Page 96 and 97: 7. The NADW Meridional Cell and Dee
Page 98 and 99:
City Latitude January ( o F) August
Page 100 and 101:
Topography & Angular Momentum Richa
Page 103 and 104:
PV = nRT
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
Page 113 and 114:
Hopf Functional Approach dx dt = x2
Page 116 and 117:
A. Sanchez-Lavega et al. Nature 451
Page 118 and 119:
0 A. Sanchez-Lavega et al. Nature 4
Page 120 and 121:
Direct Numerical Simulation of Jet
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10 -5 -10 10 8 (a) Mean Absolute Vo
Page 124 and 125:
25 days
Page 126 and 127:
Ecosystems & Feedbacks C. D. Keelin
Page 128 and 129:
J. B. Marston, M. Oppenheimer, R. M
Page 130 and 131:
Physics of Feedbacks Input (I) Syst
Page 132 and 133:
Some Feedbacks Already Included in
Page 134 and 135:
Page 136 and 137:
Page 138 and 139:
Page 140 and 141:
IPCC 2001
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?
Page 152:
“Human beings are now carrying ou
Page 156 and 157:
Antarctic Dome C Siegenthaler et al
Page 158:
Lake Mead
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