Download e-book for kindle: Analysis of inventory systems by H. G. Hadley, T. M. Whitin

By H. G. Hadley, T. M. Whitin

Mathematical versions of stock platforms

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More ozone is obtained by computation at the level of maximum ozone than the observations indicate, and less is obtained for lower levels than has been observed. The above analysis, it will be remembered, applies VERTICAL DIS T RIB UTI 0 N 27 only if the absorption coefficients of oxygen near 2000A are independent of pressure. The results of Heilpern, mentioned in section 10, indicate a strong pressure dependence for the absorption coefficients of oxygen above 2100A. It is just below here, 19502100A, that the values of the absorption coefficients of oxygen are very important in the calculations.

At any rate, it is the writer's belief that the chain of events will prove to be so complicated that statistical methods will be very difficult to apply, and that the importance of the problem justifies considerable labor in the direction of deducing the nature of any physical link as an indication of the ultimate relationship between solar anomalies and tropospheric-weather anomalies. Section 20. The meteorological significance of atmospheric ozone At the present time, the primary importance of ozone to meteorology stems from the fact that ozone content is a quasi-conservative property of an air parcel in the lower stratosphere.

Etc. Thus the rate of change of 113 is relatively larger the farther 11 3 is from equilibrium. 8). Table 4 gives the time Llt for these changes at levels below 40 km for cases I, II, and V. The results in table 4 show that above the level of maximum ozone at 30 km, the amount of ozone is usually apt to be near equilibrium. At, and especially below the level of maximum ozone, however, the VoL. 2 computed times are so large as to indicate that the ozone is practically never in equilibrium with the sun.

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