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7. Drag the blue endpoint of the triangle. Dragging endpoints is the most direct way to change the geometry. Dragging the line directly may also work, but this sometimes produces odd results, particularly in versions earlier than SolidWorks 2007. The sketch leaves a ghost when dragging so that you can see where you started. 8. Click the Smart Dimension tool, and then click the horizontal line and the angled line. This produces an angle dimension. Place the angle dimension inside the triangle, and give it a value of 30 . 9. Click the Sketch Fillet tool, set the radius value to 0.10 inches, and click each of the three endpoints. Where the 1.000-inch dimension connects to the sketch, SolidWorks has created virtual sharps. Figure 4.31 shows the sketch at this point. You may now want to turn off the Sketch Relations display because the screen is getting pretty busy. You can find this setting at View Sketch Relations.

Using 11 samples, the relative standard deviation is 0.3. Approximating the probability density 2 function (pdf) of the estimator to be Gaussian with mean P and variance P /N, the probability that the estimate is more than 20% off is then (8.27) 1 Pr(0.8P < P < 1.2P ) = 2 Q(0.2 N) For N = 11 this probability becomes 0.5. Example 8.4 Consider now the case of wideband measurements, where measurements are done at ten independently fading frequencies. How do the results change Again aiming to estimate the narrowband channel attenuation averaged over small-scale fading, usage of wideband measurements just implies that N = 110 measurements are now available. Modifying Eq. (8.27), we nd that the probability for more than 20% error has decreased to 0.036.

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You know Gmail: It s Google s massively popular web-based email service. In an era where Microsoft and Yahoo! provided lackluster web-based email, Gmail was a revelation: massive storage space, a terrific user interface, and fantastic spam and virus protection. Over time, while the incumbent webmail services languished, Google continued to innovate, adding features like POP download, IMAP access, integrated instant messaging, and much, much more. But the most important Gmail feature for me, at least is the ability to have your own personal Gmail at your own domain. Now, ordinary folks can have arguably one of the best email services available without having to put an @gmail.com at the end of their address. Did I mention that you can get this for free Before Google made this service available, I had laboriously set up an email server myself and provided it to my hosting clients. No longer; when a client hosts his or her site with me and wants to also get email, I push it to Google. The features are better, the overall experience is better, I don t pay a cent, and it s completely trouble-free. For the rest of this section, I m going to take you through the process of setting up a domain with Google Apps. While Apps is a complete service that offers a calendar, office tools, and email, it s only the latter that I ll concern you with here. You can explore the rest on your own. Follow these steps:

We nally turn to the spatial correlation of the shadowing alone (without small-scale fading). The value of the shadowing changes only slowly with the location of the MS. Thus, realizations of the shadowing eld strength (or power) that are measured at a distance x apart are correlated. The most common model is that of an exponential correlation, i.e., Ex {F (x)F (x + x)} = exp( x/x), where the decorrelation distance x is typically on the order of 5 50 m, depending on the environment.

A disaster recovery plan is like a smoke alarm in your house you know that you need it, but you don t really appreciate it until disaster strikes. With the correct documentation and backups, as described in this chapter, you can quickly restore servers to operating condition and keep your business running even after a major server failure. Not only is creating a disaster recovery plan very important, but practicing it and keeping the documentation up to date as the need arises is also vital to the health of your system.

TABLE 18.

Assuming that the current flow is essentially one-dimensional from the source to the drain (this assumption will be inadequate for short-channel devices), the drain current is described by dn J. (x, y) = qlt.t nE + qD. dn dy (3.1)

It is difficult to find the factors of large numbers, but it also may not be easy to factorize algebraic expressions. Consider, for example,

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