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very simple and the major dif culty is to keep the time of the reference place with a good enough accuracy, that is, with a drift less than a few seconds per day. Pendulums, although of good accuracy on land, were unable to provide this accuracy at sea, mainly because of the motions of the ship and changes in humidity and temperature. John Harrison built four different clocks, leading to numerous innovative concepts. After almost 50 years of remarkable achievements, in August 1765 a panel of six experts gathered at Harrison s house in London and examined the nal H4 watch. John and William (his son) nally received the rst half of the longitude prize. The other half was nally awarded to them by Act of Parliament in June 1773. Certainly more important is the fact that John Harrison was nally recognized as being the man who solved the longitude problem. One of the most famous demonstrations of Harrison s clocks ef ciency was provided by James Cook during the second of his three famous voyages in the Paci c Ocean. This second trip was dedicated to the exploration of Antarctica. In April 1772, he sailed south with two ships: the Resolution and the Adventure. He spent 171 days sailing through the ice of the Antarctic and decided to sail back to the Paci c islands. He returned to London harbor in June 1775, after more than 40,000 nautical miles. During this voyage, he was carrying K1, Kendall s copy of Harrison s H4. The daily rate of loss of K1 never exceeded eight seconds (corresponding to a distance of two nautical miles at the equator) during the entire voyage. This was the proof that longitude could be measured using a watch.

At the edge of the Antarctic vortex there is a broad region which is warmer than the vortex interior and so currently contains few PSCs As increased greenhouse gases cool the stratosphere, there may be more ozone loss in this edge region despite the reduced chlorine from CFCs [91] One can conceive of other climate effects on stratospheric ozone: changes in the Brewer Dobson circulation due to changes in the energy or distribution of the tropospheric waves driving it; changes in stratospheric chemistry due to changes in the hydrological cycle and, hence, in HOx abundances; etc These are active areas of research in the chemistry-climate modelling community [88] but the community is still some way off providing a quantitative understanding, often because of limitations in the treatment of aerosol processes.

Global Mobile Suppliers Association, 10 Global navigation satellite system (GNSS), 459 Global positioning system (GPS), 459 GLONASS system, 459 GMSC (gateway MSC), 13 Google.com, 88 GPRS (general packet radio service), see GSM/ GPRS/EDGE characteristics of, generally, 83, 206 charging for, 415, 422 423, 426 network, 183 GPRS RAN (GERAN), 320, 361 362 GPRS SGSN, 414 415 GPRS tunneling protocol (GTP), 364 GPRS/WCDMA, 32 33 Group key Kg, 383 Group management hierarchy (GMH), digital rights management, 401 G.723.1, 208 G.729, 208 GSM (global system for mobile communication), see GSM/EDGE; GSM/GPRS/EDGE characteristics of, generally, 208 evolution of, 66 phones, 205 standardization, 13 GSM (Group Speciale Mobile), 414 GSM Association, 10 GSM/EDGE, 9 10 GSM/GPRS/EDGE end-user performance, 31 33 GSM principle, 24 26 operator performance, 29 31 radio access network architecture, 26 service creation principle, 26 27 GSM/GPRS, synchronization, 261 GSM MSC, 414 GSM900, 29 Hacks, 384 Handheld Device Markup Language (HDML), 5, 67 Handheld PCs, 205 Handover (HO)/handoff, IP multicast system, 343 345 Handover packet loss, 316 317 Handshake protocol DRM security, 379 380 WAP 1.0, 77 HARQ, 28 Harvest Web cache, 121 123 Headers, HTTP/1.1 end-to-end, 50 51 entity, 51, 54 56

Including detailed microphysics and heterogeneous chemistry, to describe aerosol physics and ozone chemistry, is dif cult within climate models that are already computationally expensive In this chapter, I have tried to give a general sense of the behaviour of the stratospheric aerosol layer, its impact on environmental chemistry and, hence, its impact wider impact on the earth system In the half century since its discovery, the Junge layer has become very well characterised.

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There are, however, some surprisingly fundamental questions remaining: how much new particle formation occurs in the stratosphere, and, if any, where does the formation take place What are the most important mechanisms for freezing of aerosol or PSC particles How will the aerosol and PSC distribution respond to climate change, and will this response be driven by temperature alone, or by changes in circulation and changes in composition (especially of water vapour) And how will changes in aerosol and cloud feedback onto climate In the untangling of these questions, observations, detailed models, parameterisations and conceptual arguments will all play a part and will, in any event, build on the solid observational and theoretical understanding developed since the 1960s..

(See also Section 11.1.) Compatible norms: Let 11 lla and II lib be norms for (m xl) and (n xl) vectors, respectively. The norm 11 11 for (m x n) matrices is compatible with 11 lla and II lib if