R v Brown

Churchill, R. V., Brown, J. W. and Veikey, R. F., Complex Variables and Applications (third edition), McGraw-Hill Book Company, New York (1974). 

Tuazon, E. C., W. P. L. Carter, R. V. Brown, R. Atkinson, A. M. Winer, and J. N. Pitts, Jr., "Atmospheric Reaction Mechanisms of Amine Fuels, Report No. ESL-TR-82-17, U.S. Air Force Engineering and Services Center, Tyndall Air Force Base, FL, March 1982. 

As will be appreciated after the consideration of the provisions of the 1998 Act in Section 12.6, the standards required for obtaining and processing information form the basic building blocks of data protection and these decisions are likely to remain important and influential. On the other hand, the only case under the Data Protection Act 1984 to reach the House of Lords, R v Brown ([1996] 1 All ER 545), although containing some authoritative statements about privacy and data protection is unlikely to remain of direct relevance. The central issue in the case was the meaning of use in the context of unauthorized use which was a criminal offence by virtue of the provisions of Section 5(2) (b), and was also in the third data protection principle (see Table 12.4). In contrast, the criminal offences in the 1998 Act no longer contain this constraction and neither is it a feature of the new data protection principles. 

Fig. 9.3 Methyl cyanide (CH3CN) versus carbon monoxide (CO) mixing ratios measured iiom the R/V Brown and calculated with a chemistry GCM. Avraage values are shown by the straight lines. The measurements (black) were performed between 12 °S, 73 °E and 17 °N, 69 °E. The measurements in blue represent air masses transported from the northwest, as determined by back-trajectory calculations [25]. Because our chemistry GCM is unable to distinguish the air mass history, because it mixes the air masses at 1.8° resolution, the slope of the red line is less steep than of the black line...

Considering that the pollution occurs at low latitudes, one expects strong pho-tocheuucal activity, possibly giving rise to ozone (O3) buildup. Because of its important role in atmospheric chemistry, O3 was measured from all platforms and ground stations, as well as through balloon soundings from KCO and the R/V Brown [29]. In several O3 profiles over KCO (Fig. 10.5a), sharp peaks can be discerned, with a particularly pronounced O3 maximum above the BL. The O3 minimum within the BL, which extended to an altitude of 0.5-1 km, and the maximum directly above are not well reproduced by the model. This is related to a... 

NO, as measured from the Citation aircraft, was generally below the detection limit of 40 pptv. On the R/V Brown, NO was generally below 10 pptv (T.P. Carsey, R.R. Dickerson, M.L. Farmer, unpublished data). 

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