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this problem, header compression can be used or multiple voice frames can be packed together before encapsulating them into one RTP packet A trade-o exists between the number of voice frames that can be packed into one packet and the amount of delay due to large packet size, which may cause degradation of voice quality As mentioned in 2, the packet delay jitter bu er at the receiver s end attempts to neutralize the e ects of variation in delay from one packet to the next in the incoming packet voice streams (RTP streams) An arti cial delay is added to each packet s arrival time in order to write asynchronously the incoming packets at the head of the bu er The speech frames are extracted from the tail of the same bu er at a steady rate for proper playback.

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This delay jitter bu er is elastic, and its occupancy level is allowed to grow and shrink to accommodate the delay variations However, the delay jitter bu er should never be allowed to under ow or over ow This may cause breaks or discontinuity in the reproduced voice signal Belated packets may cause the bu er to under ow, and precocious packets may cause it to over ow This can be avoided by setting a threshold in the delay jitter bu er and delaying the playout until the bu er occupancy exceeds this threshold This threshold value must be dynamic enough to re ect the changing network conditions As a result, the additional delay due to this bu er would not adversely a ect the voice quality.

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Depending on the delay budget, type of CODEC, voice sample/packet size, and implementation complexity, the delay jitter bu er s size may vary from two to four voice samples/packets This is equivalent to 40 to 80 msec of delay for a voice sample/packet size of 20 msec, for example, in a G711 or 64 Kbps PCM-coded voice signal For G729 (CS-ACELP, 8 Kbps) coding 15 msec of coding delay is incurred, and if 30 msec of voice sample/packet size is used, the delay jitter bu er size may become 60 msec or higher The situation gets worse when G7231 (ACELP, 53 Kbps) coding is sued, because a coding delay of 375 msec is incurred A larger delay jitter bu er may cause degradation in voice quality unless appropriate hardware-based echo cancellation is deployed.

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Management of Voice Quality During a VoIP Session In circuit switching, once a circuit is allocated for a voice call or connection, the quality of transmission of the voice signal is almost guaranteed for the duration of the conversation This is not the case in packet-switched networks unless an emulated circuit for example, the ATM technology that supports circuit emulation service [8] for real-time applications like real-time voice conversation is allocated for the service As suggested in 2 and mentioned earlier, any one or more of the techniques discussed in the following paragraphs can be used to maintain the desired quality of voice transmission during a VoIP session The size of the VoIP packets can be reduced by using a smaller voice sample and/or by compressing the RTP/UDP/IP headers by using the recommendation suggested in IETF s RFC 2508 This may call for more processing, buf-.

Figure 7.6 Summertime low-elevation sunshine as measured by a Campbell Stokes sunshine recorder at Hazelrigg near Lancaster, UK. The measure shown, E , is calculated with respect to the overall amount of bright sunshine: E = (q/((t/d)/w)) 100, where q is the amount of sunshine recorded between given solar zenith angles near sunrise and sunset, t is the total amount of sunshine recorded for a 20-day range around mid-summer, d is the total number of daylight hours between sunrise and sunset for same range of days, that is the maximum potential hours of sunshine, and w is the amount time of the whole template division occupies. For the results shown all these quantities were measured in hours. This measure removes the interannual variability in total sunshine. The solar elevation ranges, plotted in the gure, are labelled by their equivalent path length through a 1-km-deep planetary boundary layer. The reduction in sunshine due to the eruptions of el Chichon (March April 1982) and Mt Pinatubo (June 1991) is sustained over 2 3 years and is due to an enhancement of the stratospheric aerosol. Such variation in solar irradiance at the surface due to sporadic perturbations of the stratospheric aerosol by volcanic eruptions is likely to signi cantly affect observed trends in surface measurements, such as those shown here and those used in the global dimming literature [71]. (Figure adapted from Horseman et al. [72].)

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