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Reno, R. R., 34, 486, 487, 498 Rescorla, R. A., 279 Resnick, M. D., 670 Retzlaff, P., 386 Revenstorf, D., 232, 233 Reynolds, A. J., 332, 333 Reynolds, C. F., 256 Reynolds, K., 487, 498 Rezai, K., 309 Reznikoff, M., 555 Rhodewalt, F., 253 Ribinstein, L. V., 564 Ribisl, K. M., 329 Ricci, A., 307 Rice, G. T., 196, 198, 199, 200, 202 Rice, M. E., 196, 197, 198, 200, 202 Richards, F. J., 451 Richardson, H. S., 340 Richardson, M. W., 432 Richardson, W. S., 263 Richmond, R., 583, 588, 590, 599 Riddoch, M. J., 291 Rihs, F., 300 Rinck, C. M., 359 Rindskopf, D., 667 Rindskopf, D. M., 332 Ringelstein, E. B., 300 Ripley, B. D., 58 Rips, L., 168 Rips, L. J., 561 Rissanen, J., 585, 587, 589 Ritter, C., 573 Ritter, W., 306 Ritterband, L. M., 256, 260 Rizzolatti, G., 302 Robbins, P. C., 196, 197, 198, 199, 201, 202 Roberts, L. J., 232, 233 Roberts, M. C., 305 Roberts, M. M., 96 Roberts, R., 309 Roberts, R. C., 304 Roberts, T. P., 312 Robertson, L. C., 294 Robins, E., 294 Robins, R. W., 369 Robinson, E., 221 Robins-Wahlin, T. B., 308 Robles, T. F., 256 Robson, P., 218 Roby, J., 297 Roche, A., 452 Roderick, M., 561 Rodriguez, M., 251, 252 Roed, J. C., 135 Roese, N. J., 549 Rog, D. J., 236 Rogers, H. J., 438, 441 Rogers, R., 189, 190, 203, 205, 206 Rogosa, D., 452, 471 Rohrbaugh, J. W., 304 Rolls, E. T., 290 Romano, J., 261 Romney, D. M., 410, 412 Ronchetti, E. M., 77, 628 Rooney, B. L., 250 Roper, S. N., 309 Rose, J. S., 626 Rose, S. E., 310

When you edit a bitmap graphic, you modify pixels, rather than lines and curves. Bitmap graphics are resolution-dependent, because the data describing the image is fixed to a grid of a particular size. Editing a bitmap graphic can change the quality of its appearance. In particular, resizing a bitmap graphic can make the edges of the image ragged as pixels are redistributed within the grid. Displaying a bitmap graphic on an output device that has a lower resolution than the image itself also degrades the quality of its appearance.

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groundwater discharge to wells Water wells come in a great range of shapes and sizes For the most part they are approximately vertical excavations from the ground surface down to some position below the water table (or the base of the overlying aquitard where the shallowest aquifer at a given site is con ned) The construction of wells has a very ancient pedigree For instance, there are hand-dug wells still in use today in parts of Iran which were constructed more than 3000 years ago Hand-digging of wells was the principal technique of well construction worldwide until the nineteenth century, when various types of drilling rig nally came into widespread use An interesting collation of early drilling techniques has been presented by Eberle and Persons (1978).

For water vapour in air, Le is about 0.85, showing that water vapour diffuses faster than heat travels in air. The term with Le is therefore non-zero, and its sign depends on whether the temperature of the transported air at the point in question is rising or falling. In any mixing situation in the atmosphere, air packets will exist, which have opposite signs. This will lead to highly local uctuations in the water content of clouds as well as the evident uctuations in the existence of the cloud that are seen at cloud edges. An example of the locality of the aerosol formation produced is seen in the calculations for cooled laminar ow in a tube performed by Barrett and Fissan [79], but calculations for actual turbulent ows in the atmosphere are lacking. The same physics will apply to any volatile material that forms aerosol when the temperature is lowered in the atmosphere. The uctuations that arise will depend on the Lewis number for vapour transport of the material in air. Most organics are expected to have relatively slow

The rst drilling rigs operated by means of percussion, with a blade of some sort being repeatedly dropped into the hole to break up the strata into looser fragments which can then be removed using a long, narrow bucket known as a bailer Alternating periods of cutting and bailing of fragments from the hole eventually results in a deep hole suitable for completion as a well While percussive drilling can be used to drill in consolidated materials, it is very slow in such applications, and is thus largely restricted nowadays to sinking wells in soft sediments Further developments in drilling technology were stimulated by the phenomenal growth of the oil industry in the late nineteenth century.

e g(x) e 2.80212 = = 0.0572 g(x) 1+e 1 + e 2.80212 Thus, the estimated probability that a customer with 100 day minutes will churn is less than 6%. This is less than the overall proportion of churners in the data set, 14.5%, indicating that low day minutes somehow protects against churn. However, for a customer with 300 day minutes, we have e g(x) e 3.92929 + 0.0112717(day mins) = g(x) 1+e 1 + e 3.92929 + 0.0112717(day mins)

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