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The Epistemologies of Non-Forecasting Simulations, Part II: Climate, Chaos, Computing Style, and the Contextual Plasticity of Error

Published online by Cambridge University Press:  01 June 2009

Lambert Williams
Affiliation:
Harvard University and Max-Planck-Institut für Wissenschaftsgeschichte, Berlin
William Thomas
Affiliation:
Center for the History of Physics, American Institute of Physics, College Park, Maryland
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Argument

We continue our analysis of modeling practices that focus more on qualitative understanding of system behavior than the attempt to provide sharp forecasts. The argument here is built around three episodes: the ambitious work of the Princeton Meteorological Project; the seemingly simple models of convection in weather systems by Edward Lorenz at MIT; and then finally analysis of the dripping faucet by Robert Shaw and the Dynamical Systems Collective at UC Santa Cruz. Using the Princeton Meteorological Project as an argumentative foil for the later chaos work of Lorenz and Shaw, we first show how the epistemological interest of modeling came to shift from issuing predictions to probing the very meaning and limits of prediction. The second step of our argument shows that what may be seen in one context of use as a modeling technology that is error ridden, imprecise, or inadequate, may be parsed completely differently in another context. This argument about technology and practice, we argue, feeds through to epistemological conceptions of error. Far from being something that can be defined in the absolute, the notion of error is shown to be contextually plastic.

Information

Type
Research Article
Copyright
Copyright © Cambridge University Press 2009
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Fig. 1. The Royal McBee LGP-30. The approximate dimensions of this “desk” machine, not including the typewriter shelf to the left, are 26 inches deep by 33 inches high by 44 inches long. Immediately above the cooling unit and the digital display unit (marked in the middle of the machine) is the control panel. At top right is the memory drum, and below that lies the power supply: 1,500 watts were needed for operation. Courtesy of the Computer History Museum, Mountain View, California.

Figure 1

Fig. 2. The Lorenz Attractor. This visualization of Lorenz's three-equation model shows how a trajectory through phase space evolves over time in a complex and non-repeating pattern (Lorenz 1963, 137). © 2009 American Meteorological Society (AMS)

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Fig. 3. Depiction of a Systron Donner analog computer. With analog machines, computations are performed using such properties as electrical resistance and voltage. Courtesy of the Computer History Museum, Mountain View, California.

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Fig. 4. The Dripping Faucet System. Drops falling from the faucet at top left break a light beam, which produces pulses in a photocell signal. The pulses in turn operate a timer with a resolution of 4 microseconds that produces the basic data: time intervals between drops (Shaw 1984, 3). © 2009 Aerial Press

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Fig. 5. A time-versus-time map for the period 2 regime of the dripping faucet. Period doubling is the best known “route to chaos”: first comes period doubling (in this case, two drops before the system behavior repeats itself), then quadrupling (four drops before repetition), and so on until the onset of chaos (Shaw 1984, 8). © 2009 Aerial Press

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Fig. 6. Shaw's model of a water drop at low flow rate. A spring bearing a mass (m) is stretched linearly until at a certain distance the mass “falls off” by Δm as a drop detaches (Shaw 1984, 15). © 2009 Aerial Press

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Fig. 7. A time-versus-time map comparing dripping faucet system data with the “naïve” analog model (Shaw 1984, 16). © 2009 Aerial Press

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Fig. 8. The Rössler Attractor. Rössler's original paper makes plain a certain family resemblance between his structure and the Lorenz attractor given as Figure 2 above. In particular, it shares the same tracing of trajectories over finite values but with chaotic oscillation (Shaw 1984, 17). © 2009 Aerial Press

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Fig. 9. Invariant distribution with and without noise added. This gives a map of the values and probabilities that a given event may have (Shaw 1984, 55). © 2009 Aerial Press