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The origins of NTVEMES go back a long way (Section 1.3.1) and there is much experience on which to build success. The second example illustrates the technological advances in teleinonitoring that have been applied to air travel. Like its competitors, British Airways is concerned to provide the best available healthcare to its passengers [ 1921. Each aircraft carries a comprehensive medical kit and trained personnel but the situation in a Boeing 747 at 30 000 feet on a 17-hOlIr long-haul flight is not exactly equivalent to a fully-equipped emergency room on the ground. Since the 1980s, commercial companies based in hospitals have operated a verbal support service for in-flight emergencies. However, question-andanswer techniques are no substitute for measurements and so BA has worked with Telemedic Systems to develop a laptop computer device to monitor vital signs and relay them to medical personnel on the ground via satellite [193]. Telemedic Systems has worked with similar companies to add new monitors to the basic vital signs unit. For example, patients now have access to a respiratory device that measures air mass flow and analyses their breath since the latter can reveal the

Different solutions for the temperature distribution have been derived by various workers, depending on the assumptions made concerning the relative contributions of the above phenomena. Two models derived by Peacock & Wang (1999) and representing relatively cool and warm subducting lithosphere are shown in Plate 9.3 (between pp. 244 and 245). Although differing in detail, all such models indicate that the downgoing slab maintains its thermal identity to great depths and that, exceptionally, temperature contrasts up to 1000 C may exist between the core of the slab and normal mantle at a depth of 700 km. As noted in Section 9.4, the length of the Benioff zone depends on the depth to which the subducting oceanic lithosphere maintains a relatively cold central core. Molnar et al. (1979) deduced that the downward de ection of isotherms, and hence the length of the seismic zone, is proportional to both the rate of subduction and the square of the thickness of the lithosphere. Lithosphere thickness is proportional to the square root of its age (Turcotte & Schubert, 2002) so that the length

Figure 8.12 shows graphically the two-node Bayesian network. In this diagram the node Sex is in boldface to indicate that it has been instantiated that is to say, evidence has been observed that the student s sex is female. Based on this observation, the probabilities of X are updated accordingly. One problem with the use of joint probabilities in the calculation of conditional probabilities is that the complete speci cation of a joint probability distribution will require a great many numbers. For the two-node case, this was a relatively small number only 2 * 3 = 6 joint probabilities. In general, however, one would need to specify n1 n2 . . . nk probabilities, where ni is the number of

Note that the dollar symbol ($) is typically ASCII character 24 (in U.S. fonts) and can be accessed directly from the keyboard.

you can access all the functions that are defined in the two files, Sample.rb and Math.rb. However, what if both the files contain some functions with common names This will result in code ambiguity. To avoid code ambiguity, you can use modules. This is another advantage of using modules.

22:7

Specifying the Document Type HTML, Head, and Body Tags Styles Markup for Paragraphs Markup for Characters Special Characters Organizational Elements

sacri cial technology is illustrated in Figure 18.27. On the left-hand side of the gure, the overgrown inkjet chamber is still lled with Cu. On the right-hand side the Cu lling has already been etched out with nitric acid. In both cases, direct nucleation is not possible and either seeding with nanopowder [179] or the insertion of a thin interfacial nucleation layer is needed. In both illustrated examples BEN has been used in conjunction with a special, thin, interfacial nucleation layer.

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Be careful with your setting for the Scale parameter, in order to avoid unexpected results. If you have to size a Flash movie out of its aspect ratio, the Flash player needs to know what to do with any extra room it has to fill. Figure 23-5

Dreamweaver initially assigns a temporary filename and an absolute pixel value to your HTML frameset code. Both can be modified later, if you wish.

The next step is to put the constants into the Java class that we created. Here is the code for that class.

Figure 16.8 Electrochemical conversion of nitrobiphenyls. Cyclic voltammogram of a nitrobiphenyl-functionalized UNCD electrode recorded in 100-mM potassium chloride aqueous electrolyte solution. The rst scan (1) shows an irreversible wave, peaking at 1.08V versus Ag/AgCl, corresponding to the reduction of the residual nitro groups (see inset). A surface coverage of about 5 10 10 mol/ cm2 is obtained from the total current under the cathodic peak (grey area)

13:2

The aSize argument indicates the maximum amount of space in bytes to be freed by the Compact() call. This allows manual mode clients to