Biometeorological Methods by R. E. Munn PDF

By R. E. Munn

ISBN-10: 012510250X

ISBN-13: 9780125102506

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12) dT/dt = (T7! - T)/\ where dT/dt = the rate of change with time of the indicated temperature, λ = a constant of proportionality (dimension of time). 13) (Τχ - T)/(Ti - TQ) = exp(-*/X) when the instant of immersion into the new environment is taken as t = 0. For time t = λ, the right-hand side of Eq. 8% of its original difference (T1 - T0). 2% of the initial temperature difference. The quantity λ is known as the time constant. , Eq. 12) is a first-order differential equation. 6. Physical Time Lags 35 The dependence of λ on wind speed and on the diameter of a thermometer is illustrated in Fig.

12) dT/dt = (T7! - T)/\ where dT/dt = the rate of change with time of the indicated temperature, λ = a constant of proportionality (dimension of time). 13) (Τχ - T)/(Ti - TQ) = exp(-*/X) when the instant of immersion into the new environment is taken as t = 0. For time t = λ, the right-hand side of Eq. 8% of its original difference (T1 - T0). 2% of the initial temperature difference. The quantity λ is known as the time constant. , Eq. 12) is a first-order differential equation. 6. Physical Time Lags 35 The dependence of λ on wind speed and on the diameter of a thermometer is illustrated in Fig.

To the north of the arctic front in summer, for example, precipitation is uncertain and temperatures are not high enough to support tree growth, suggesting that the climatological position of fronts may be a useful index of the integrated effect of a number of weather variables. If the hypothesis is accepted, two interesting questions arise: (a) Will the position of the tree-line shift if the general circulation changes, and if so, what is the time constant of the response? (b) Will the general circulation change if the tree-line advances or retreats?

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Biometeorological Methods by R. E. Munn


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